TY - JOUR AU - Bi, Yao AU - Chen, Huan AU - Hanski, Eero AU - Kuritani, Takeshi AU - Wu, Hong-Xiang AU - Zhang, Feng-Qi AU - Liu, Jia AU - Gu, Xiao-Yan AU - Xia, Qun-Ke TI - Hydrous mantle plume promoted the generation of continental flood basalts in the Tarim large igneous province JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 14 PY - 2024 IS - 1 SN - 2045-2322 DO - 10.1038/s41598-024-60213-4 UR - https://m2.mtmt.hu/api/publication/34832360 ID - 34832360 AB - Recent research on the water content of large igneous provinces (LIPs) has revealed that water has a significant impact on the formation of LIPs. However, most studies focus on the water content of mafic–ultramafic rocks, while relatively little attention has been paid to the water content of continental flood basalts (CFB), which form the major part of LIPs and are characterized by huge volumes (> 1 × 10 5 km 3 ) and short eruption times. Here, we determined water contents of clinopyroxene crystals from the Akesu diabase, which is co-genetic with flood basalts of the Tarim LIP in China. Based on these measurements, we obtained a water content of higher than 1.23 ± 0.49 wt.% for the parental magma to the Tarim CFB and a minimum water content of 1230 ± 490 ppm for the mantle source, thus indicating the presence of a hydrous mantle plume. Combined with previous studies, our results suggest that water plays a key role in the formation of the Tarim LIP. Additionally, the whole-rock compositions of the Akesu diabase indicate a contribution of pyroxenite in the mantle source. This is consistent with a model, in which water was brought into the Tarim mantle plume by a subducted oceanic plate that entered the deep mantle. LA - English DB - MTMT ER - TY - JOUR AU - Chang-Yu, Zhu AU - Huan, Chen AU - Yan-Tao, Hao AU - Qunke, Xia TI - The effects of partial melting and metasomatism on peridotite water contents: insights from Shuangliao Volcano Group, Northeast China JF - JOURNAL OF PETROLOGY J2 - J PETROL VL - 65 PY - 2024 SP - 1 EP - 20 PG - 20 SN - 0022-3530 UR - https://m2.mtmt.hu/api/publication/34781760 ID - 34781760 LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Lange, Thomas Pieter AU - Patkó, Levente AU - Aradi, László Előd AU - Berkesi, Márta AU - Peter, M. E. Tollan AU - José, Alberto Padrón-Navarta AU - Jörg, Hermann AU - Gergely, Szilveszter AU - Szabó, Csaba AU - Kovács, István János TI - Formation of amphibole lamellae in mantle pyroxene by fluid-mediated metasomatism: A focal plane array FTIR study from the Carpathian-Pannonian region JF - AMERICAN MINERALOGIST J2 - AM MINERAL VL - 109 PY - 2024 IS - 1 SP - 87 EP - 102 PG - 16 SN - 0003-004X DO - 10.2138/am-2022-8662 UR - https://m2.mtmt.hu/api/publication/33785006 ID - 33785006 N1 - MTA FI Lendület Pannon LitH2 Oscope Research Group, Institute of Earth Physics and Space Science, Sopron, 9400, Hungary Institute of Earth Physics and Space Science, Sopron, 9400, Hungary Lithosphere Fluid Research Laboratory, Department of Petrology and Geochemistry, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, 1117, Hungary Doctoral School of Environmental Sciences, Eötvös Loránd University, Budapest, 1117, Hungary Institut für Geologie, Universität Bern, Bern, 3012, Switzerland Géosciences Montpellier, CNRS-Université de Montpellier, Université des Antilles, Montpellier, 34090, France Instituto Andaluz de Ciencias de la Tierra, CSIC, University of Granada, Armilla, 18100, Spain Department of Applied Biotechnology and Food Science, Budapest University of Technology and Economics, Budapest, 1111, Hungary Export Date: 19 January 2024 Correspondence Address: Liptai, N.; MTA FI Lendület Pannon LitH2 Oscope Research Group, Hungary; email: n.liptai.elte@gmail.com Funding details: Ministerio de Ciencia e Innovación, MICINN, RYC2018-024363-I Funding details: Nemzeti Kutatási Fejlesztési és Innovációs Hivatal, NKFI, K141956 Funding text 1: We are thankful to Dóra Kesjár for help with the FTIR analyses. We are grateful for the thorough and constructive comments of David M. Jenkins and an anonymous reviewer, and the editorial handling by Anne Peslier. This study was financially supported by the MTA FI Lendület Pannon LitHOscope Research Group and the NKFIH K141956 Topo-Transylvania grant. JAPN acknowledges financial support from the Spanish MICINN through the Ramón y Cajal fellowship (RYC2018-024363-I). 2 LA - English DB - MTMT ER - TY - JOUR AU - Harangi, Szabolcs AU - Szarvas, I AU - Haranginé Lukács, Réka TI - Wide-ranging and violent volcanic history of a quiet transborder area : volcanic geoheritage of the Novohrad–Nógrád UNESCO Global Geopark JF - GEOCONSERVATION RESEARCH J2 - GEOCONSERVATION RES VL - 6 PY - 2023 IS - 1 SP - 178 EP - 206 PG - 29 SN - 2588-7343 DO - 10.30486/gcr.2023.1982587.1133 UR - https://m2.mtmt.hu/api/publication/34052385 ID - 34052385 N1 - Eötvös Loránd University, Faculty of Geography and Earth Sciences, Department of Petrology and Geochemsitry, Pázmány sétány 1/C, Budapest, H-1117, Hungary MTA-ELTE Volcanology Research Group, Pázmány sétány 1/C, Budapest, H-1117, Hungary Ipolytarnóc Fossils Nature Conservation Area, Bükk National Park, Ipolytarnóc, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network (ELKH), Budapest, Hungary Cited By :1 Export Date: 13 October 2023 Correspondence Address: Harangi, S.; Eötvös Loránd UniversityHungary; email: harangi.szabolcs@ttk.elte.hu AB - The Novohrad–Nógrád UNESCO Global Geopark is the first cross-border geopark located between Slovakia and Hungary, Eastern–Central Europe. “Ancient world without borders” – its motto reflects both the remarkable geodiversity and the strong link between people living on either side of the state border. In this relatively small area, almost all types of eruption products can be found from basaltic through andesitic to rhyolitic, reflecting the wide-ranging volcanism of the Pannonian Basin over the last 20 million years, which were the largest eruptions in Europe at the time. The Ipolytarnóc Site, the gateway of the geopark and possessor of a European- Diploma for Protected Areas, documents when one of these devastating eruption events buried a subtropical-forested area with thick pyroclastic deposits and preserved vertebrate footprints. On the other hand, relatively young eruptions of basaltic magmas occurred in this area that give another specific atmosphere to the geopark. Columnar jointing with concave and convex curvilinear shapes shown both by basalts and andesites is another peculiar natural value. Due to the regional uplift and the associated erosion, most of the volcanic edifices were removed and the root zones of the volcanoes were revealed, giving a special character. The volcanic heritage meets specific cultural and historical heritage, which makes this geopark a particular tourist destination. There are four visitor centers and several nature trails with explanation panels showing concise summaries of the volcanological features in three languages (Hungarian, Slovakian and English). Among the rich indoor and outdoor activities, the annual Volcano Day program in Ipolytarnóc with an interactive volcano show attracts many people. This is an evolving geopark, where continuously renewing attractions serve the geoeducation and geotourism purposes in parallel with geoheritage conservation management. LA - English DB - MTMT ER - TY - JOUR AU - Győri, Erzsébet AU - Czanik, Csenge AU - Czecze, Barbara AU - Fodor, Csilla AU - Gribovszki, Katalin Eszter AU - Kalmár, Dániel AU - Kiss, János AU - Kovács, István János AU - Marótiné Kiszely, Márta AU - Liptai, Nóra AU - Süle, Bálint AU - Timkó, Máté AU - Varga, Péter AU - Wéber, Zoltán TI - Hungarian national report on IASPEI (2019-2022) JF - GEOMATIKAI KÖZLEMÉNYEK / PUBLICATIONS IN GEOMATICS J2 - GEOMAT KÖZL VL - 25 PY - 2022 SP - 117 EP - 137 PG - 21 SN - 1419-6492 UR - https://m2.mtmt.hu/api/publication/34045288 ID - 34045288 LA - English DB - MTMT ER - TY - THES AU - Konstantinos, Thomaidis TI - Do mantle xenoliths preserve water signature from the lithospheric mantle and how? An analytical, experimental and numerical approach PY - 2022 SP - 132 UR - https://m2.mtmt.hu/api/publication/33363917 ID - 33363917 LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Gráczer, Zoltán AU - Szanyi, Gyöngyvér AU - Cloetingh, SAPL. AU - Süle, Bálint AU - Aradi, LE. AU - Falus, Gy AU - Bokelmann, G AU - Timkó, Máté AU - Timár, Gábor AU - Szabó, Csaba AU - Kovács, István János TI - Seismic anisotropy in the mantle of a tectonically inverted extensional basin: A shear-wave splitting and mantle xenolith study on the western Carpathian-Pannonian region JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 845 PY - 2022 PG - 16 SN - 0040-1951 DO - 10.1016/j.tecto.2022.229643 UR - https://m2.mtmt.hu/api/publication/33249428 ID - 33249428 N1 - MTA FI Lendület Pannon LitH2Oscope Research Group, Institute of Earth Physics and Space Science, Sopron, Hungary Institute of Earth Physics and Space Science, Sopron, Hungary Tectonics Group, Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands Lithosphere Fluid Research Laboratory, Department of Petrology and Geochemistry, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Supervisory Authority of Regulatory Affairs, Budapest, Hungary Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria Department of Geophysics and Space Science, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Export Date: 21 December 2022 Correspondence Address: Liptai, N.; MTA FI Lendület Pannon LitH2Oscope Research Group, Hungary; email: liptai.nora@epss.hu LA - English DB - MTMT ER - TY - JOUR AU - Nformidah-Ndah, Siggy S. AU - Tollan, Peter M. E. AU - Hermann, Joerg AU - Tchouankoue, Jean Pierre TI - Depletion and refertilisation of the lithospheric mantle below the Kapsiki plateau (Northern Cameroon Volcanic Line) deduced from trace element and H2O systematics in mantle xenoliths JF - JOURNAL OF AFRICAN EARTH SCIENCES J2 - J AFR EARTH SCI VL - 189 PY - 2022 PG - 17 SN - 1464-343X DO - 10.1016/j.jafrearsci.2022.104483 UR - https://m2.mtmt.hu/api/publication/32958157 ID - 32958157 AB - Clinopyroxene bearing spinel harzburgites recovered from Cenozoic alkaline basalts from the Kapsiki plateau were investigated with the aim of understanding depletion and enrichment processes in the subcontinental mantle below a major tectonic line. Concentrations of major and trace elements (including H) were determined in-situ in olivine, orthopyroxene, clinopyroxene and spinel by EPMA, LA-ICP-MS and FTIR. The xenoliths are refractory with high olivine (0.91-0.92) and orthopyroxene (0.92-0.93) Mg# coupled with relatively high modal proportions of clinopyroxene (5-8%) and a remarkably wide range in clinopyroxene Mg# (0.91-0.94), interpreted to reflect high degrees of partial melting followed by modal and chemical metasomatic refertilization. A fractional partial melting model of orthopyroxene trace elements in a depleted mantle indicates 20-30% of melting. Clinopyroxenes show two groups based on their CaO contents (18.7-18.9 and 20.6-22.6 wt %) suggesting a secondary origin and modal metasomatism. The low Ca clinopyroxenes were the latest to be formed, and the wide range of clinopyroxene Mg# shows a lack of equilibrium with the coexisting minerals. The high Ca clinopyroxenes record ancient metasomatic events that are also documented in orthopyroxene. Cryptic metasomatism is shown by strong progressive enrichments in LREEs and MREEs of orthopyroxene and clinopyroxene. Th vs La and Sr vs Nd of clinopyroxene are used to identify different generations of metasomatism. Ti/Eu vs (La/ Yb)(N) and Zr/Hf systematics indicate that the metasomatising agent has both a carbonatite and a silicate component. The structural hydroxyl contents of the different mineral phases are very low (< 1 ppm for olivine, 40-48 ppm for orthopyroxene and 164-277 ppm for clinopyroxene). The very low water contents compared to typical sub-continental peridotites could be attributed to the depleted nature of the xenoliths or reflect lower water activities of carbonatitic melts relative to alkaline melts. Estimated fO(2) values expressed as delta logFMQ, (where FMQ corresponds to the fayalite magnetite-quartz oxygen buffer) range from -0.42 to -0.26 and are consistent with minor OH stretching regions of 3520 cm(-1) in orthopyroxene, related to a ferric iron defect.& nbsp;The combination of textural investigations, major, and trace element and H2O data suggests that a refractory subcontinental mantle was affected by several episodes of intraplate metasomatism dominated by silicatecarbonatite melts above the North-Eastern end of the Cameroon Volcanic Line. LA - English DB - MTMT ER - TY - JOUR AU - Azevedo-Vannson, Samantha AU - France, Lydéric AU - Ingrin, Jannick AU - Chazot, Gilles TI - Mantle metasomatic influence on water contents in continental lithosphere: New constraints from garnet pyroxenite xenoliths (France & Cameroon volcanic provinces) JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 575 PY - 2021 SN - 0009-2541 DO - 10.1016/j.chemgeo.2021.120257 UR - https://m2.mtmt.hu/api/publication/32020415 ID - 32020415 N1 - Cited By :3 Export Date: 10 March 2023 Correspondence Address: Azevedo-Vannson, S.; Université de Lorraine, France; email: samantha.azevedo-vannson@mnhn.fr LA - English DB - MTMT ER - TY - JOUR AU - Gose, Jürgen AU - Schmädicke, Esther TI - H 2 O in omphacite of quartz and coesite eclogite from Erzgebirge and Fichtelgebirge, Germany JF - JOURNAL OF METAMORPHIC GEOLOGY J2 - J METAMORPH GEOL VL - 1 PY - 2021 SP - 1 EP - 22 PG - 22 SN - 0263-4929 DO - 10.1111/jmg.12642 UR - https://m2.mtmt.hu/api/publication/32593001 ID - 32593001 N1 - Cited By :1 Export Date: 10 March 2023 Correspondence Address: Schmädicke, E.; Geozentrum Nordbayern, Germany; email: esther.schmaedicke@fau.de LA - English DB - MTMT ER - TY - JOUR AU - Kovács, István János AU - Liptai, Nóra AU - Koptev, A AU - Cloetingh, SAPL. AU - Lange, Thomas Pieter AU - Mațenco, L AU - Szakács, A AU - Radulian, M AU - Berkesi, Márta AU - Patkó, Levente AU - Molnár, Gábor AU - Novák, Attila AU - Wesztergom, Viktor AU - Szabó, Csaba AU - Fancsik, Tamás TI - The ‘pargasosphere’ hypothesis: Looking at global plate tectonics from a new perspective JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 204 PY - 2021 PG - 20 SN - 0921-8181 DO - 10.1016/j.gloplacha.2021.103547 UR - https://m2.mtmt.hu/api/publication/32080418 ID - 32080418 N1 - MTA EK Lendület Pannon LitH2Oscope Research Group, Centre for Energy Research, Budapest, Hungary Institute of Earth Physics and Space Science (ELKH EPSS), Sopron, Hungary Centre for Energy Research, Institute for Energy Security and Environmental Safety, Budapest, Hungary University of Tübingen, Department of Geosciences, Tübingen, Germany Tectonics Group, Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands Lithosphere Fluid Research Lab (LRG), Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Department of Environmental Research Centre, Institute for Nuclear Research (ATOMKI), Debrecen, Hungary Institute of Geodynamics, Romanian Academy, Bucharest, Romania National Institute of Earth Physics, Bucharest, Romania Academy of Romanian Scientists, Bucharest, Romania Geological, Geophysical and Space Research Group of the Hungarian Academy of Sciences at Eötvös Loránd University, Budapest, Hungary Óbuda University, Alba Regia Technical Faculty, Institute of Geoinformatics, Székesfehérvár, Hungary Mining and Geological Survey of Hungary, Budapest, Hungary Cited By :22 Export Date: 9 April 2024 CODEN: GPCHE Correspondence Address: Kovács, I.J.; MTA EK Lendület Pannon LitH2Oscope Research Group, Hungary; email: kovacs.istvan.janos@csfk.mta.hu LA - English DB - MTMT ER - TY - CONF AU - Kővágó, Ákos AU - KOVACS, Marinel AU - KESJÁR, Dóra AU - Szabó, Csaba AU - KOVÁCS, István János TI - Új FTIR mérési eredmények az Avas–Gutin mészalkáli vulkáni kőzeteiből: poszterupciós hatások nyomai a fenokristályok szerkezeti hidroxil-tartalmában : New FTIR data from the Oaş–Gutâi Mts. and post eruption effects on the water content of phenocrysts T2 - XXII. Bányászati, Kohászati és Földtani Konferencia PB - Erdélyi Magyar Műszaki Tudományos Társaság (EMT) C1 - Kolozsvár PY - 2021 SP - 83 EP - 84 PG - 2 UR - https://m2.mtmt.hu/api/publication/32038750 ID - 32038750 LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Berkesi, Márta AU - Patkó, Levente AU - Bodnár, RJ AU - O’Reilly, SY AU - Griffin, WL AU - Szabó, Csaba TI - Characterization of the metasomatizing agent in the upper mantle beneath the northern Pannonian Basin based on Raman imaging, FIB-SEM and LA-ICP-MS analyses of silicate melt inclusions in spinel peridotite JF - AMERICAN MINERALOGIST J2 - AM MINERAL VL - 106 PY - 2021 IS - 5 SP - 685 EP - 700 PG - 16 SN - 0003-004X DO - 10.2138/am-2021-7292 UR - https://m2.mtmt.hu/api/publication/31956559 ID - 31956559 N1 - Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös University, 1/C Pázmány Péter sétány, Budapest, H-1117, Hungary Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and Gemoc, Department of Earth and Planetary Sciences, Macquarie University, Herring Road, North Ryde, NSW 2019, Australia Institute for Nuclear Research, Isotope Climatology and Environmental Research Centre, 18/C Bem tér, Debrecen, Hungary Fluids Research Laboratory, Department of Geosciences, Virginia Tech, 926 West Campus Drive, Blacksburg, VA, United States Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, 6-8 Csatkai Endre u, Sopron, 9400, Hungary Cited By :2 Export Date: 1 July 2022 Correspondence Address: Liptai, N.; Lithosphere Fluid Research Lab, 1/C Pázmány Péter sétány, Hungary; email: n.liptai.elte@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Lange, Thomas Pieter AU - Patkó, Levente AU - Pintér, Zsanett AU - Berkesi, Márta AU - Aradi, László Előd AU - Szabó, Csaba AU - Kovács, István János TI - Effect of water on the rheology of the lithospheric mantle in young extensional basin systems as shown by xenoliths from the Carpathian-Pannonian region JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 196 PY - 2021 PG - 12 SN - 0921-8181 DO - 10.1016/j.gloplacha.2020.103364 UR - https://m2.mtmt.hu/api/publication/31655281 ID - 31655281 N1 - MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, Hungary School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia Export Date: 27 November 2020 CODEN: GPCHE Correspondence Address: Liptai, N.; MTA CSFK Lendület Pannon LitH2Oscope Research Group, Mining and Geological Survey of HungaryHungary; email: liptai.nora@csfk.mta.hu Funding Agency and Grant Number: Lendulet Research Grant; ELTE Institutional Excellence Program by the Hungarian Ministry of Human Capacities [1783-3/2018/FEKUTSRAT]; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [NN128629]; [GINOP2.3.2-15-2016-00009] Funding text: The authors owe thanks to Judith Mihaly and Csaba Nemeth for their help with FTIR analyses. We are grateful for the detailed and constructive reviews of Wolfram Geissler and Ioan Seghedi, as well as for the editorial handling by Liviu Matenco. This study was financially supported by a Lendulet Research Grant to the MTA CSFK Lendulet Pannon LitH2Oscope Research Group, the ELTE Institutional Excellence Program (1783-3/2018/FEKUTSRAT) by the Hungarian Ministry of Human Capacities to L. Patko, L. E. Aradi, M. Berkesi and Cs. Szabo, the GINOP2.3.2-15-2016-00009 research program to L. Patko, and the Hungarian Scientific Research Fund (grant nr. NN128629, Topo-Transylvania) to I. Kovacs. The manuscript is dedicated to the memory of Prof. Frank Horvath, who was a pioneer in building cooperations between geophysical and geochemical research. MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, Hungary School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia Cited By :1 Export Date: 16 February 2021 CODEN: GPCHE Correspondence Address: Liptai, N.; MTA CSFK Lendület Pannon LitH2Oscope Research Group, Hungary; email: liptai.nora@csfk.mta.hu Funding details: GINOP-2.3.2-15-2016-00009 Funding details: Hungarian Scientific Research Fund, OTKA Funding text 1: The authors owe thanks to Judith Mihály and Csaba Németh for their help with FTIR analyses. We are grateful for the detailed and constructive reviews of Wolfram Geissler and Ioan Seghedi, as well as for the editorial handling by Liviu Matenco. This study was financially supported by a Lendület Research Grant to the MTA CSFK Lendület Pannon LitH 2 Oscope Research Group, the ELTE Institutional Excellence Program (1783-3/2018/FEKUTSRAT) by the Hungarian Ministry of Human Capacities to L. Patkó, L. E. Aradi, M. Berkesi and Cs. Szabó, the GINOP-2.3.2-15-2016-00009 research program to L. Patkó, and the Hungarian Scientific Research Fund (grant nr. NN128629, Topo-Transylvania) to I. Kovács. The manuscript is dedicated to the memory of Prof. Frank Horváth, who was a pioneer in building cooperations between geophysical and geochemical research. MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, Hungary School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia Export Date: 28 May 2021 CODEN: GPCHE Correspondence Address: Liptai, N.; MTA CSFK Lendület Pannon LitH2Oscope Research Group, Hungary; email: liptai.nora@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Patkó, Levente AU - Novák, Attila AU - Klébesz, Rita AU - Liptai, Nóra AU - Lange, Thomas Pieter AU - Molnár, Gábor AU - Csontos, László AU - Wesztergom, Viktor AU - Kovács, István János AU - Szabó, Csaba TI - Effect of metasomatism on the electrical resistivity of the lithospheric mantle – An integrated research using magnetotelluric sounding and xenoliths beneath the Nógrád-Gömör Volcanic Field JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 197 PY - 2021 PG - 17 SN - 0921-8181 DO - 10.1016/j.gloplacha.2020.103389 UR - https://m2.mtmt.hu/api/publication/31789122 ID - 31789122 N1 - Lithosphere Fluid Research Lab (LRG), Eötvös Loránd University, Budapest, Hungary Lendület Pannon LitH2Oscope Research Group, Research Centre for Astronomy and Earth Sciences (CSFK), Sopron, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research (ATOMKI), Debrecen, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences (CSFK), Sopron, Hungary Geological, Geophysical and Space Research Group of the Hungarian Academy of Sciences, Eötvös Loránd University, Budapest, Hungary Exploration & Production Division, MOL Group, Budapest, Hungary Export Date: 4 January 2021 CODEN: GPCHE Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab (LRG), Eötvös Loránd UniversityHungary; email: cszabo@elte.hu Lithosphere Fluid Research Lab (LRG), Eötvös Loránd University, Budapest, Hungary Lendület Pannon LitH2Oscope Research Group, Research Centre for Astronomy and Earth Sciences (CSFK), Sopron, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research (ATOMKI), Debrecen, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences (CSFK), Sopron, Hungary Geological, Geophysical and Space Research Group of the Hungarian Academy of Sciences, Eötvös Loránd University, Budapest, Hungary Exploration & Production Division, MOL Group, Budapest, Hungary Export Date: 16 February 2021 CODEN: GPCHE Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab (LRG), Hungary; email: cszabo@elte.hu Funding details: GINOP-2.3.2-15-2016-00009 Funding details: European Social Fund, ESF, LP-2018/5 Funding details: Magyar Tudományos Akadémia, MTA, BO/00795/11/10 Funding details: Nemzeti Kutatási Fejlesztési és Innovációs Hivatal, NKFIH, K128122, 1783-3/2018/FEKUTSRAT Funding text 1: The authors acknowledge Csaba Molnár for his help with MT measurements in the field and László Szarka for his contribution in MT methodology. This research was supported by the TAMOP-4.2.2.C–11/1/KONV-2012-0015 (Earth-system) project sponsored by the European Social Fund . The project was further financed by a Lendület Research Grant to the MTA CSFK Lendület Pannon LitH 2 Oscope Research Group (LP-2018/5) and the NKFIH K128122 grant to the Topo-Transylvania community. This work was completed with the support of the ELTE Institutional Excellence Program (1783-3/2018/FEKUTSRAT) managed by the Hungarian Ministry of Human Capacities to L. Patkó and Cs. Szabó. L. Patkó and T. P. Lange were also supported by the GINOP-2.3.2-15-2016-00009 research program. A. Novak was sponsored by the János Bolyai Scholarship of the Hungarian Academy of Sciences ( BO/00795/11/10 ). This is the 104th publication of the Lithosphere Fluid Research Lab (LRG) collaboration with the GGI. Lithosphere Fluid Research Lab (LRG), Eötvös Loránd University, Budapest, Hungary Lendület Pannon LitH2Oscope Research Group, Research Centre for Astronomy and Earth Sciences (CSFK), Sopron, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research (ATOMKI), Debrecen, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences (CSFK), Sopron, Hungary Geological, Geophysical and Space Research Group of the Hungarian Academy of Sciences, Eötvös Loránd University, Budapest, Hungary Exploration & Production Division, MOL Group, Budapest, Hungary Export Date: 28 May 2021 CODEN: GPCHE Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab (LRG), Hungary; email: cszabo@elte.hu LA - English DB - MTMT ER - TY - THES AU - Siggy, Signe Nformidah-Ndah TI - Evolution of the subcontinental lithospheric mantle below a major tectono-volcanic structure: constraints from mantle xenoliths along the Cameroon Volcanic Line PY - 2021 SP - 272 UR - https://m2.mtmt.hu/api/publication/34841914 ID - 34841914 LA - English DB - MTMT ER - TY - JOUR AU - Wang, Yong-Feng AU - Qin, Jun-Ying AU - Soustelle, Vincent AU - Zhang, Jun-Feng AU - Xu, Hai-Jin TI - Pyroxene does not always preserve its source hydrogen concentration: Clues from some peridotite xenoliths JF - GEOCHIMICA ET COSMOCHIMICA ACTA J2 - GEOCHIM COSMOCHIM AC VL - 292 PY - 2021 SP - 382 EP - 408 PG - 27 SN - 0016-7037 DO - 10.1016/j.gca.2020.10.003 UR - https://m2.mtmt.hu/api/publication/31664831 ID - 31664831 N1 - Funding Agency and Grant Number: National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41590623, 41372224, 41872230] Funding text: We thank Luan-Xi Bai, Jin-Lin Li, and Qian Ma for help with sample collection and thin-section preparation. Hua-Ping Ren and Peng-Xiao Li are appreciated for assistance with FTIR measurements and data processing. We are also grateful to Zhao-Chu Hu and Tao Luo for help with LA-ICP-MS analyses, and to Ji-Hao Zhu for help with EMPA analyses. We are indebted to Huai Cheng and Yu Yuan for help with LA-ICP-MS data processing. Constructive and insightful comments by Jollands M. C., an anonymous reviewer, and the editor, Catalano J. G., help to improve our manuscript significantly and are greatly appreciated. This work was supported by the National Natural Science Foundation of China [grant numbers 41590623, 41372224, 41872230]. School of Earth Sciences and State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China Global Tectonic Center, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China Export Date: 16 February 2021 Correspondence Address: Wang, Y.-F.; School of Earth Sciences and State Key Laboratory of Geological Processes and Mineral Resources, China; email: yfwang@cug.edu.cn Funding details: National Natural Science Foundation of China, NSFC, 41590623, 41372224, 41872230 Funding text 1: We thank Luan-Xi Bai, Jin-Lin Li, and Qian Ma for help with sample collection and thin-section preparation. Hua-Ping Ren and Peng-Xiao Li are appreciated for assistance with FTIR measurements and data processing. We are also grateful to Zhao-Chu Hu and Tao Luo for help with LA-ICP-MS analyses, and to Ji-Hao Zhu for help with EMPA analyses. We are indebted to Huai Cheng and Yu Yuan for help with LA-ICP-MS data processing. Constructive and insightful comments by Jollands M. C., an anonymous reviewer, and the editor, Catalano J. G., help to improve our manuscript significantly and are greatly appreciated. This work was supported by the National Natural Science Foundation of China [grant numbers 41590623 , 41372224 , 41872230 ]. LA - English DB - MTMT ER - TY - JOUR AU - Yang, Yan AU - Ingrin, Jannick AU - Liu, Wendi AU - Huang, Weihua AU - Gu, Xiaoyan AU - Xia, Qunke TI - Behavior and origin of hydrogen defects in natural orthopyroxene during high-temperature processes JF - AMERICAN MINERALOGIST J2 - AM MINERAL VL - 106 PY - 2021 IS - 11 SP - 1768 EP - 1779 PG - 12 SN - 0003-004X DO - 10.2138/am-2021-7741 UR - https://m2.mtmt.hu/api/publication/32489446 ID - 32489446 N1 - Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province, School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China CNRS, INRAE, ENSCL, UMR 8207, UMET, Unité Matériaux et Transformations, University of Lille, Lille, F 59000, France Export Date: 10 March 2023 Correspondence Address: Yang, Y.; Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province, China; email: yanyang2005@zju.edu.cn LA - English DB - MTMT ER - TY - JOUR AU - Ashley, Aaron Wolfgang AU - Bizimis, Michael AU - Peslier, Anne H AU - Jackson, Matthew AU - Konter, Jasper G TI - Metasomatism and Hydration of the Oceanic Lithosphere: a Case Study of Peridotite Xenoliths from Samoa JF - JOURNAL OF PETROLOGY J2 - J PETROL VL - 61 PY - 2020 IS - 2 SP - 1 EP - 29 PG - 29 SN - 0022-3530 DO - 10.1093/petrology/egaa028 UR - https://m2.mtmt.hu/api/publication/31651327 ID - 31651327 N1 - Funding Agency and Grant Number: National Sciences FoundationNational Science Foundation (NSF) [1624310, 1624315]; Geological Society of America student grant [12121-18] Funding text: This work was supported by the National Sciences Foundation (OCE #1624310 to A.H.P. and OCE #1624315 to M.B.) and a Geological Society of America student grant (12121-18 to A.W.A.). Export Date: 16 February 2021 Correspondence Address: Ashley, A.W.; Department of Earth, United States; email: awashley93@gmail.com Funding details: OCE #1624310, 1624315, 12121-18 Funding text 1: Our sincere thanks go to Rajdeep Dasgupta and Kyusei Tsuno for access to, and their help with, Raman spectroscopy, and to Ioannis Baziotis for help interpreting the results. Paul B?guelin is thanked for his helpful comments on the paper. Many thanks go to the Editor, Marjorie Wilson, and Associate Editor, Adam Kent, for handling our paper, and to reviewers Qun-Ke Xia, Peter Tollan and an anonymous reviewer for their helpful and detailed comments that resulted in a much-improved paper. This work was supported by the National Sciences Foundation (OCE #1624310 to A.H.P. and OCE #1624315 to M.B.) and a Geological Society of America student grant (12121-18 to A.W.A.). LA - English DB - MTMT ER - TY - JOUR AU - Balan, Etienne AU - Paulatto, Lorenzo AU - Liu, Jia AU - Ingrin, Jannick TI - Low-temperature infrared spectrum and atomic-scale structure of hydrous defects in diopside JF - EUROPEAN JOURNAL OF MINERALOGY J2 - EUR J MINERAL VL - 32 PY - 2020 IS - 5 SP - 505 EP - 520 PG - 16 SN - 0935-1221 DO - 10.5194/ejm-32-505-2020 UR - https://m2.mtmt.hu/api/publication/31651386 ID - 31651386 N1 - Funding Agency and Grant Number: TelluS Program of CNRS-INSU Funding text: Calculations have been performed using the computing resources of IMPMC (Sorbonne Universite-CNRS-MNHN) and the HPC resources of IDRIS under the allocation 2020-A0080910820 attributed to GENCI (Grand Equipement National de Calcul Intensif). This work was supported by the TelluS Program of CNRS-INSU. Sorbonne Université, CNRS, MNHN, Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), 4 place Jussieu, Paris Cedex 05, 75252, France Univ. Lille, CNRS, INRAE, ENSCL, UMR 8207, UMET - Unité Matériaux et Transformations, Lille, 59000, France School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China Cited By :1 Export Date: 16 February 2021 Correspondence Address: Balan, E.; Sorbonne Université, 4 place Jussieu, France; email: etienne.balan@sorbonne-universite.fr Funding text 1: computing resources of IMPMC (Sorbonne Université-CNRS-MNHN) and the HPC resources of IDRIS under the allocation 2020-A0080910820 attributed to GENCI (Grand Equipement National de Calcul Intensif). This work was supported by the TelluS Program of CNRS-INSU. LA - English DB - MTMT ER - TY - JOUR AU - Doucet, LS AU - Xu, YJ AU - Klaessens, D AU - Hui, HJ AU - Ionov, DA AU - Mattielli, N TI - Decoupled water and iron enrichments in the cratonic mantle: A study on peridotite xenoliths from Tok, SE Siberian Craton JF - AMERICAN MINERALOGIST J2 - AM MINERAL VL - 105 PY - 2020 IS - 6 SP - 803 EP - 819 PG - 17 SN - 0003-004X DO - 10.2138/am-2020-7316 UR - https://m2.mtmt.hu/api/publication/31374720 ID - 31374720 N1 - Funding Agency and Grant Number: Belgium F.R.S.-FNRS "mandat Charge de Recherche"Fonds de la Recherche Scientifique - FNRS [1.B.102.14F]; CAS (Chinese Academy of Sciences)Chinese Academy of Sciences [2017VCA0009]; Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41590623, 41573055] Funding text: Financial support was provided to L.S.D. by the Belgium F.R.S.-FNRS "mandat Charge de Recherche" (no. 1.B.102.14F). D.A.I. acknowledges the Visiting Scientist fellowships within the CAS (Chinese Academy of Sciences) President's International Fellowship Initiative (PIFI) in 2017-19 (Grant No. 2017VCA0009). H.H. acknowledges support from the Natural Science Foundation of China (41590623 and 41573055). Export Date: 16 February 2021 LA - English DB - MTMT ER - TY - JOUR AU - Gartner, AJJB AU - McKenzie, D TI - Estimates of the temperature and melting conditions of the Carpathian‐Pannonian upper mantle from volcanism and seismology JF - GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS J2 - GEOCHEM GEOPHY GEOSY VL - 21 PY - 2020 IS - 10 PG - 21 SN - 1525-2027 DO - 10.1029/2020GC009334 UR - https://m2.mtmt.hu/api/publication/31618594 ID - 31618594 N1 - Funding Agency and Grant Number: European Research Council (ERC) under the European UnionEuropean Research Council (ERC) [759563] Funding text: We thank Bill White, Godfrey Fitton, and an anonymous reviewer for their constructive reviews, and Janne Blichert-Toft for editorial handling. We also thank two anonymous reviewers whose perceptive comments helped to improve an earlier version of this paper. A. J. J. B. G. would like to thank Ioan Seghedi for his help and suggestions. During the writing of this paper, A. J. J. B. G. received funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement 759563). A. J. J. B. G. conceived the project and wrote the paper. D. M. carried out the modeling. Export Date: 16 February 2021 Correspondence Address: Bracco Gartner, A.J.J.; Faculty of Science, Netherlands; email: a.j.j.braccogartner@vu.nl Funding details: 759563 Funding details: European Research Council, ERC Funding text 1: We thank Bill White, Godfrey Fitton, and an anonymous reviewer for their constructive reviews, and Janne Blichert‐Toft for editorial handling. We also thank two anonymous reviewers whose perceptive comments helped to improve an earlier version of this paper. A. J. J. B. G. would like to thank Ioan Seghedi for his help and suggestions. During the writing of this paper, A. J. J. B. G. received funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement 759563). A. J. J. B. G. conceived the project and wrote the paper. D. M. carried out the modeling. AB - What drives the formation of basaltic melts beneath intraplate volcanoes not associated with extensive thermal anomalies or lithospheric extension? Detailed constraints on the melting conditions and source region are imperative to resolve this question. Here we model the geochemistry of alkali basalts and mantle nodules brought up by young (12–0.1 Ma) intraplate volcanoes distributed across the Carpathian-Pannonian region and combine the results with geophysical observations. Rare earth element inversion and forward calculation of elemental concentrations show that the basalts require the mantle to have undergone less than 1% melting in the garnet-spinel transition zone, at depths of about 63–72 km. The calculated melt distributions correspond to a mantle potential temperature of ∼1257°C, equivalent to a real temperature of 1290°C at 65 km beneath the Pannonian Basin. The composition, modal mineralogy, and clinopyroxene geochemistry of some of the entrained mantle nodules closely resemble the basalt source, though the latter equilibrated at greater depths. The gravity anomalies and topography of the Basin reveal no large-scale features that can account for the post-extensional volcanism. Instead, the lithospheric thickness and geotherm show that melting occurs because the base of the lithosphere, at ∼50-km depth, is close to or at the solidus temperature over a large part of the Basin. Hence, only a small amount of upwelling is required to produce minor volumes (up to a few cubic kilometers) of melt. We conclude that the Pannonian volcanism originates from upwelling in the asthenosphere just below thinned lithosphere, which is likely to be driven by thermal buoyancy. LA - English DB - MTMT ER - TY - JOUR AU - Kovács, István János AU - Patkó, Levente AU - Liptai, Nóra AU - Lange, Thomas Pieter AU - Taracsák, Z. AU - Cloetingh, S.A.P.L. AU - Török, Kálmán AU - Király, Edit AU - Karátson, Dávid AU - Biró, Tamás AU - Kiss, János AU - Pálos, Zsófia AU - Aradi, László Előd AU - Falus, György AU - Hidas, K. AU - Berkesi, Márta AU - Koptev, A. AU - Novák, Attila AU - Wesztergom, Viktor AU - Fancsik, Tamás AU - Szabó, Csaba TI - The role of water and compression in the genesis of alkaline basalts: Inferences from the Carpathian-Pannonian region JF - LITHOS J2 - LITHOS VL - 354-355 PY - 2020 PG - 16 SN - 0024-4937 DO - 10.1016/j.lithos.2019.105323 UR - https://m2.mtmt.hu/api/publication/31006469 ID - 31006469 N1 - MTA CSFK Lendület Pannon LitH2Oscope Research Group, Sopron, Hungary CSFK Geodetic and Geophysical Institute, Sopron, Hungary Eötvös University, Department of Petrology and Geochemistry, Lithosphere Fluid Research Lab, Budapest, Hungary Institute for Nuclear Research, Isotope Climatology and Environmental Research Centre, Debrecen, Hungary University of Manchester, Department of Earth and Environmental Sciences, Manchester, United Kingdom Utrecht University, Tectonics Research Group, Utrecht, Netherlands Mining and Geological Survey of Hungary, Budapest, Hungary Eötvös University, Department of Physical Geography, Budapest, Hungary Instituto Andaluz de Ciencias de la Tierra, CSIC-UGR, Granada, Spain University of Tübingen, Department of Geosciences, Tübingen, Germany Export Date: 28 May 2021 Correspondence Address: Kovács, I.; MTA CSFK Lendület Pannon LitH2Oscope Research GroupHungary; email: kovacs.istvan.janos@csfk.mta.hu LA - English DB - MTMT ER - TY - THES AU - Patkó, Levente TI - Integrated study on the interaction between upper mantle and mafic melt evidenced by wehrlite xenoliths from the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin, Central Europe) PY - 2020 DO - 10.15476/ELTE.2020.022 UR - https://m2.mtmt.hu/api/publication/31789195 ID - 31789195 LA - English DB - MTMT ER - TY - JOUR AU - Patkó, Levente AU - Liptai, Nóra AU - Aradi, László Előd AU - Klébesz, Rita AU - Sendula, Eszter AU - Bodnar, Robert J. AU - Kovács, István János AU - Hidas, Károly AU - Cesare, Bernardo AU - Novák, Attila AU - Trásy, Balázs AU - Szabó, Csaba TI - Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths JF - GEOSCIENCE FRONTIERS J2 - GEOSCI FRONT VL - 11 PY - 2020 IS - 3 SP - 943 EP - 964 PG - 22 SN - 1674-9871 DO - 10.1016/j.gsf.2019.09.012 UR - https://m2.mtmt.hu/api/publication/31044367 ID - 31044367 N1 - Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary CCFS-GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, Australia Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Sopron, Hungary Fluids Research Laboratory, Department of Geosciences, Virginia Tech, Blacksburg, VA, United States MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Sopron, Hungary Instituto Andaluz de Ciencias de La Tierra, CSIC & UGR, Armilla, Granada, Spain Department of Geosciences, University of Padua, Padua, Italy Department of Geology, Eötvös Loránd University, Budapest, Hungary Export Date: 28 May 2021 Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab, Hungary; email: cszabo@elte.hu LA - English DB - MTMT ER - TY - THES AU - Aradi, László Előd TI - Geochemical and tectonic evolution of the subcontinental lithospheric mantle under the Styrian Basin based on ultramafic xenoliths PY - 2019 SP - 157 UR - https://m2.mtmt.hu/api/publication/31029627 ID - 31029627 LA - English DB - MTMT ER - TY - CONF AU - Ingrin, J. AU - Azevedo-Vannson, S. AU - France, L. TI - Identification of two distinct OH infrared signatures in pyroxenes from pyroxenite xenoliths T2 - Geophysical Research Abstracts PY - 2019 SP - 1 PG - 1 UR - https://m2.mtmt.hu/api/publication/30723909 ID - 30723909 LA - English DB - MTMT ER - TY - JOUR AU - Lange, Thomas Pieter AU - Szabó, Csaba AU - Liptai, Nóra AU - Patkó, Levente AU - Gelencsér, Orsolya AU - Aradi, László Előd AU - Kovács, István János TI - A földköpeny reológiai kutatása: mennyiségi Fourier transzformációs infravörös spektrometria alkalmazása egy Persány hegységi xenolit példáján JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 149 PY - 2019 IS - 3 SP - 233 EP - 254 PG - 22 SN - 0015-542X DO - 10.23928/foldt.kozl.2019.149.3.233 UR - https://m2.mtmt.hu/api/publication/30850025 ID - 30850025 N1 - Eötvös Loránd Tudományegyetem, Földrajz-és Földtudományi Intézet, Litoszféra Fluidum Kutató Laboratórium (LRG), Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary MTA CSFK Lendület Pannon LitH2 Oscope Lendület Kutatócsoport, Hungary MTA CSFK Geofizika és Geodéziai Intézet, Csatkai Endre u. 6–8, Sopron, H–9400, Hungary MTA Atommagkutató Intézet, Izotóp Klimatológiai és Környezetkutató Központ (IKER), Bem tér 18/c, Debrecen, H–4026, Hungary Cited By :3 Export Date: 16 February 2021 Correspondence Address: Lange, T.P.; Eötvös Loránd Tudományegyetem, Pázmány Péter sétány 1/c, Hungary; email: lange.thomas@hotmail.com Funding details: Magyar Tudományos Akadémia, MTA Funding text 1: A szerz?k k?sz?nik az LRG tagok k?zrem?k?d?s?t, k?-l?n?sen P?LOS Zs?fia ?nzetlen seg?ts?g?t. Az FT?IR m?r?-sek kivitelez?s?ben ny?jtott seg?ts?g?rt k?sz?net illeti KESJ?R D?r?t (MTA CSFK FGI). LANGE Thomas Pieter k?sz?ni az Emberi Er?forr?sok Miniszt?riuma ?NKP-18-3 k?dsz?m? ?j Nemzeti Kiv?l?-s?g Programj?nak t?mogat?s?t, amely hozz?j?rult a dol-gozat elk?sz?t?s?hez. ARADI L?szl? k?sz?ni az ELTE Fels?oktat?si Int?zm?-nyi Kiv?l?s?gi Program (1783-3/2018/FEKUTSRAT) nev? p?ly?zat t?mogat?s?t, amely az Emberi Er?forr?sok Miniszt?riuma t?mogat?s?val val?sult meg. A k?zirat elk?-sz?lt?t t?mogatta az MTA CSFK Lend?let Pannon LitH2 Oscope Kutat?csoport. A cikk az LRG 97. publik?ci?ja, amely a MTA CSFK GGI ?s a Lend?let Pannon LitH2 Oscope Kutat?csoportj?val egy?ttm?k?d?sben k?sz?lt. A szerz?k k?sz?nik BAL?ZS Attil?nak ?s az Anonim b?r?l?knak a k?zirat olvas?sa sor?n tett jav?t?saikat ?s hasz-nos javaslataikat/tan?csaikat. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Hidas, K. AU - Tommasi, A. AU - Patkó, Levente AU - Kovács, István János AU - Griffin, W.L. AU - O'Reilly, S.Y. AU - Pearson, N.J. AU - Szabó, Csaba TI - Lateral and vertical heterogeneity in the lithospheric mantle at the northern margin of the Pannonian Basin reconstructed from peridotite xenolith microstructures JF - JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH J2 - J GEOPHYS RES SOLID EARTH VL - 124 PY - 2019 IS - 7 SP - 6315 EP - 6336 PG - 22 SN - 2169-9313 DO - 10.1029/2018JB016582 UR - https://m2.mtmt.hu/api/publication/30706849 ID - 30706849 N1 - Funding Agency and Grant Number: Marie Curie International Reintegration Grant [NAMS-230937]; Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences; Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences); Macquarie University international PhD scholarship; ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS); Ministry of Economy, Industry and Competitiveness (MINECO, Spain); State Research Agency (AEI, Spain) [FPDI-2013-16253, CGL2016-81085-R]; DEST Systemic Infrastructure Grants; ARC LIEF; NCRIS/AuScope; Macquarie University; Hungarian Scientific Research Fund (OTKA) [PD101683] Funding text: The authors would like to thank the people who contributed to this work. We owe thanks to Fabrice Barou and David Adams for their help with EBSDSEM analyses at Geosciences Montpellier and at CCFS Macquarie University, respectively. Laszlo Aradi is acknowledged for his help with field work, petrography and MTEX application. We are grateful for the constructive criticism of Sandra Piazolo and Jacques Precigout and two anonymous reviewers, as well as for the editorial handling of Stephen Parman. Our research received financial support from a Marie Curie International Reintegration Grant (grant NAMS-230937), a postdoctoral grant (grant PD101683) of the Hungarian Scientific Research Fund (OTKA), and a Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences to I. J. K., as well as from the Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences). N. L. received support from Macquarie University international PhD scholarship and project and travel funding from ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS). K. H. acknowledges funding from Ministry of Economy, Industry and Competitiveness (MINECO, Spain) and the State Research Agency (AEI, Spain; grants FPDI-2013-16253 and CGL2016-81085-R). Instruments used at Macquarie University are funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners, and Macquarie University. The data used in this paper are listed in the references, tables, and supporting information. The raw EBSD data are available from the corresponding author upon request. This is the 92nd publication of the Lithosphere Fluid Research Lab (LRG), contribution 1361 from the ARC Centre of Excellence for Core to Crust Fluid Systems (www.ccfs.mq.edu.au) and 1320 from the GEMOC Key Centre (www.gemoc.mq.edu.au). Funding Agency and Grant Number: Marie Curie International Reintegration GrantEuropean Union (EU) [NAMS-230937]; Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences; Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences); Macquarie University international PhD scholarship; ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS)Australian Research Council; Ministry of Economy, Industry and Competitiveness (MINECO, Spain); State Research Agency (AEI, Spain) [FPDI-2013-16253, CGL2016-81085-R]; DEST Systemic Infrastructure GrantsAustralian GovernmentDepartment of Industry, Innovation and Science; ARC LIEFAustralian Research Council; NCRIS/AuScopeAustralian GovernmentDepartment of Industry, Innovation and Science; Macquarie University; Hungarian Scientific Research Fund (OTKA)Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [PD101683] Funding text: The authors would like to thank the people who contributed to this work. We owe thanks to Fabrice Barou and David Adams for their help with EBSDSEM analyses at Geosciences Montpellier and at CCFS Macquarie University, respectively. Laszlo Aradi is acknowledged for his help with field work, petrography and MTEX application. We are grateful for the constructive criticism of Sandra Piazolo and Jacques Precigout and two anonymous reviewers, as well as for the editorial handling of Stephen Parman. Our research received financial support from a Marie Curie International Reintegration Grant (grant NAMS-230937), a postdoctoral grant (grant PD101683) of the Hungarian Scientific Research Fund (OTKA), and a Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences to I. J. K., as well as from the Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences). N. L. received support from Macquarie University international PhD scholarship and project and travel funding from ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS). K. H. acknowledges funding from Ministry of Economy, Industry and Competitiveness (MINECO, Spain) and the State Research Agency (AEI, Spain; grants FPDI-2013-16253 and CGL2016-81085-R). Instruments used at Macquarie University are funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners, and Macquarie University. The data used in this paper are listed in the references, tables, and supporting information. The raw EBSD data are available from the corresponding author upon request. This is the 92nd publication of the Lithosphere Fluid Research Lab (LRG), contribution 1361 from the ARC Centre of Excellence for Core to Crust Fluid Systems (www.ccfs.mq.edu.au) and 1320 from the GEMOC Key Centre (www.gemoc.mq.edu.au). Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös University, Budapest, Hungary Australian Research Council Centre of Excellence for Core to Crust Fluid Systems and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, North Ryde, NSW, Australia Now at MTA CSFK Lendület Pannon LitH2Oscope Research Group, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Instituto Andaluz de Ciencias de la Tierra, CSIC and UGR, Armilla, Spain Departamento de Geodinámica, Universidad de Granada, Granada, Spain Géosciences Montpellier, Université de Montpellier and CNRS, CC 60, Montpellier, cedex 5, France Geodetic and Geophysical Institute, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary MTA CSFK Lendület Pannon LitH2Oscope Research Group, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Cited By :7 Export Date: 16 February 2021 Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab, Hungary; email: cszabo@elte.hu Funding details: 1320 Funding details: Australian Education International, Australian Government, AEI, CGL2016-81085-R, FPDI-2013-16253 Funding details: Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council, CCFS, ARC Funding details: Macquarie University Funding details: Ministerio de Economía y Competitividad, MINECO Funding details: Hungarian Scientific Research Fund, OTKA Funding details: Magyar Tudományos Akadémia, MTA Funding details: Ministerio de Economía, Industria y Competitividad, Gobierno de España, MINECO Funding details: Geochemical Evolution and Metallogeny of Continents, GEMOC Funding text 1: The authors would like to thank the people who contributed to this work. We owe thanks to Fabrice Barou and David Adams for their help with EBSD-SEM analyses at Geosciences Montpellier and at CCFS Macquarie University, respectively. L?szl? Aradi is acknowledged for his help with field work, petrography and MTEX application. We are grateful for the constructive criticism of Sandra Piazolo and Jacques Pr?cigout and two anonymous reviewers, as well as for the editorial handling of Stephen Parman. Our research received financial support from a Marie Curie International Reintegration Grant (grant NAMS-230937), a postdoctoral grant (grant PD101683) of the Hungarian Scientific Research Fund (OTKA), and a Bolyai J?nos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences to I. J. K., as well as from the Lend?let Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences). N. L. received support from Macquarie University international PhD scholarship and project and travel funding from ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS). K. H. acknowledges funding from Ministry of Economy, Industry and Competitiveness (MINECO, Spain) and the State Research Agency (AEI, Spain; grants FPDI-2013-16253 and CGL2016-81085-R). Instruments used at Macquarie University are funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners, and Macquarie University. The data used in this paper are listed in the references, tables, and supporting information. The raw EBSD data are available from the corresponding author upon request. This is the 92nd publication of the Lithosphere Fluid Research Lab (LRG), contribution 1361 from the ARC Centre of Excellence for Core to Crust Fluid Systems (www.ccfs.mq.edu.au) and 1320 from the GEMOC Key Centre (www.gemoc.mq.edu.au). LA - English DB - MTMT ER -