@article{MTMT:34450441, title = {Linking mineral deposits to crustal necking: insights from the Western Alps}, url = {https://m2.mtmt.hu/api/publication/34450441}, author = {Dall’Asta, N and Manatschal, G and Hoareau, G}, doi = {10.1007/s00126-023-01226-3}, journal-iso = {MINER DEPOSITA}, journal = {MINERALIUM DEPOSITA}, volume = {In press}, unique-id = {34450441}, issn = {0026-4598}, year = {2023}, eissn = {1432-1866} } @article{MTMT:34131524, title = {Upper Carnian to Rhaetian (Upper Triassic) conodont and carbon-isotope stratigraphy of the Csővár borehole succession, Hungary}, url = {https://m2.mtmt.hu/api/publication/34131524}, author = {Karádi, Viktor and Korte, Christoph}, doi = {10.1016/j.palaeo.2023.111792}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {630}, unique-id = {34131524}, issn = {0031-0182}, year = {2023}, eissn = {1872-616X}, orcid-numbers = {Karádi, Viktor/0000-0002-5923-2944} } @article{MTMT:32795655, title = {Complex deformation history of the Keszthely Hills, Transdanubian Range, Hungary}, url = {https://m2.mtmt.hu/api/publication/32795655}, author = {Héja, Gábor and Fodor, László and Csillag, Gábor and Ortner, H and Kövér, Szilvia}, doi = {10.1556/24.2022.00114}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {65}, unique-id = {32795655}, issn = {1788-2281}, year = {2022}, eissn = {1789-3348}, pages = {77-110}, orcid-numbers = {Kövér, Szilvia/0000-0002-6736-4226} } @article{MTMT:33241347, title = {Depositional and structural controls on a fault-related dolostone formation (Maestrat Basin, E Spain)}, url = {https://m2.mtmt.hu/api/publication/33241347}, author = {Humphrey, Elliot and Gomez-Rivas, Enrique and Diego Martin-Martin, Juan and Neilson, Joyce and Salas, Ramon and Guimera, Joan}, doi = {10.1111/bre.12647}, journal-iso = {BASIN RES}, journal = {BASIN RESEARCH}, volume = {34}, unique-id = {33241347}, issn = {0950-091X}, abstract = {Fault-related dolomitisation is responsible for the development of numerous hydrocarbon reservoirs hosted in diagenetically-altered carbonates and is therefore critical to hydrocarbon exploration, subsurface storage (i.e. CO2), the formation of associated mineralisation (i.e. MVT-deposits) and for understanding the key controls on subsurface fluid flow. Multiple dolomitised outcrop analogues have been characterised in recent years, but uncertainty still remains as to the controls on dolomitisation in terms of dolostone geobody size and geometries, their distribution and how they impact reservoir quality. Late Tithonian shallow-marine carbonates at Serra Esparreguera in the Maestrat Basin (E. Spain) were partially dolomitised on the seismic scale, resulting in a spectrum of geobodies with varying degrees of spatial connectivity. Dolostone predominantly replaces Polpis Fm wackestones and packstones, and bioclastic grainstones of the Bovalar Fm. Dolostone geobodies transition through vertical stratigraphy from being massive and spatially extensive to localised stratabound bodies as textural heterogeneity increases. Irregular dolostone geometries occur in the Polpis Fm, which is texturally homogenous relative to the overlying Bovalar Fm, cross-cutting bedding in areas with high abundance of faults. Faults occur adjacent to dolostone and constrain its lateral extent across the outcrop. Dolomitisation fronts are typically sharp with morphologies affected by small-scale faults and bedding-parallel stylolites. Dolomitisation occurred under burial conditions and dolostones were later overprinted by phases of calcite and saddle dolomite cementation. The spatial distribution of dolostone is strongly influenced by the depositional heterogeneity and faults, while smaller structures (i.e. metre-scale fractures and stylolites) and bedding surfaces controlled the dolomitisation front geometry. Dolostone geobodies at Serra Esparreguera provide new insights into the structural, depositional and diagenetic controls on dolomitisation at a seismic scale, which can be used as a predictive guide to improve the understanding of carbonate reservoirs with complex paragenetic histories.}, keywords = {carbonate; structural diagenesis; Dolostone; Maestrat Basin; fault-related dolomitisation}, year = {2022}, eissn = {1365-2117}, pages = {961-990}, orcid-numbers = {Gomez-Rivas, Enrique/0000-0002-1317-6289; Neilson, Joyce/0000-0001-6213-2373; Guimera, Joan/0000-0002-0323-4633} } @article{MTMT:33241348, title = {The Diagenetic Alteration of the Carbonate Rocks from the Permian Qixia Formation as Response to Two Periods of Hydrothermal Fluids Charging in the Central Uplift of Sichuan Basin, SW China}, url = {https://m2.mtmt.hu/api/publication/33241348}, author = {Chen, Pei and Fu, Meiyan and Deng, Hucheng and Xu, Wang and Wu, Dong and He, Puwei and Guo, Hengwei}, doi = {10.3390/min11111212}, journal-iso = {MINERALS-BASEL}, journal = {MINERALS}, volume = {11}, unique-id = {33241348}, abstract = {The hydrothermal fluid-carbonate rock reaction is frequently regarded to occur in deep-burial diagenesis, and the hydrothermal dissolution is usually distributed and takes place along the faults. Previous studies have suggested that there was hydrothermal fluid activity locally in the Permian Qixia Formation in Sichuan Basin, likely related to the Emeishan basalt eruption. However, the effect of hydrothermal fluids on the carbonate rocks of the Qixia Formation in the central uplift of Sichuan Basin is still unclear. Based on the characteristics and geochemical parameters of the diagenetic minerals, this study aims to reveal the diagenetic alteration related to the hydrothermal fluid-rock reaction in the Qixia Formation and reestablish the diagenetic evolution by using the timing of diagenetic mineral precipitation. The methods include petrographic observation; trace and rare earth element (REE) analysis; C, O and Sr isotope measurement; fluid inclusion temperature measurement and cathodoluminescence analysis. According to the petrographic characteristics, the dolostones are mainly of crystalline structure, namely fine-medium crystalline dolostone, meso-coarse crystalline dolostone, and coarse crystalline dolostone, with the cathodoluminescence color becoming brighter in that order. The limestones from the Qixia Formation are of the bioclastic limestone type, with no cathodoluminescence color. Compared with dolostones, limestones have higher Sr content, lower Mn content, and heavier oxygen isotopes. With the crystalline size of dolostone becoming coarser, the oxygen isotopes of dolostones tend to become lighter. The meso-coarse crystalline dolostone has the highest Mn content and negative carbon isotope. Both limestones and dolostones have an obvious positive Eu anomaly in the Qixia Formation. However, the REE patterns of fine-medium crystalline dolostones are very different from those of meso-coarse crystalline dolostones. It is credible that there were two periods of hydrothermal fluid charging, with different chemical compositions. The first period of hydrothermal fluids could laterally migrate along the sequence boundary. Fine-medium crystalline dolostones were almost completely distributed below the sequence boundary and were dolomitized during the shallow burial period. As products of the hydrothermal fluid-dolostone reaction, the saddle-shaped dolomites in the meso-coarse crystalline dolostones were the evidence of the second period of hydrothermal fluids. As a result, the dolomitization model was established according to the timing of diagenetic mineral precipitation, which can improve that the geological understanding of the effect of hydrothermal fluid activities on the carbonate rocks in the Qixia Formation.}, keywords = {Elements; isotope; Permian; SICHUAN BASIN; Hydrothermal dolomitization; dolostones}, year = {2021}, eissn = {2075-163X} } @article{MTMT:31509680, title = {Thermal convection dolomitization induced by the Emeishan Large Igneous Province}, url = {https://m2.mtmt.hu/api/publication/31509680}, author = {Dong, Y and Chen, H and Wang, J and Hou, M and Xu, S and Zhu, P and Zhang, C and Cui, Y}, doi = {10.1016/j.marpetgeo.2020.104308}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {116}, unique-id = {31509680}, issn = {0264-8172}, abstract = {The mechanism of dolomitization has long been debated due to complex sedimentary and diagenetic conditions. Large-scale dolomite bodies were recently discovered in the Permian Cisuralian Qixia Formation (284-273 Ma) in the northwestern Sichuan Basin, providing an opportunity to understand the dolomitization associated with the Emeishan Large Igneous Province (ELIP). Traditionally, the dolomites in the Sichuan Basin have been interpreted as hydrothermal dolomitization because of the hydrothermal impacts from the ELIP. Here, we report new petrographic and geochemical data on the Permian dolomites, which we grouped into two categories (matrix dolomites or Md1-Md3 and cement dolomites or Cd), that support thermal convection dolomitization. The petrographic and geochemical features (delta C-1(3), delta O-18, REE, Mn/Sr ratios, Sr-87/Sr-86 ratios) suggest that Md1 were formed in penecontemporaneous seawater, whereas Md2, Md3, and Cd were formed in fluids resembling Permian seawater during shallow burial stage, of which both dolomitizing fluids are non-hydrothermal. High formation temperature inferred from fluid inclusion is consistent with the low delta O-18 values of the Md2, Md3 and Cd, suggesting that the ELIP event may have provided the heat for the dolomitization in the Qixia carbonate platform. The formation of the widespread dolomite bodies was facilitated by the rapid convection exchange between warm pore seawater in the Qixia strata of the platform margin and cold water from outside the slope. Therefore, we demonstrate that the dolomites in the northwestern Sichuan Basin are mainly due to thermal convection dolomitization in the shallow burial stage. This study provides important implications for the mechanism of dolomite formation linked to abnormal geothermal activity.}, keywords = {THERMAL CONVECTION; Permian; dolomitization; ELIP; geochemical analysis}, year = {2020}, eissn = {1873-4073}, orcid-numbers = {Wang, J/0000-0002-1832-958X} } @mastersthesis{MTMT:33806665, title = {CARACTÉRISATION DE LA DOLOMITISATION D’UNE PLATE-FORME CARBONATÉE EN CONTEXTE DE MARGE SALIFÈRE HYPER-ÉTENDUE ET INVERSÉE : EXEMPLE DE LA PLATE-FORME CARBONATÉE JURASSIQUE OUEST-PYRÉNÉENNE}, url = {https://m2.mtmt.hu/api/publication/33806665}, author = {Geoffrey, Motte}, unique-id = {33806665}, year = {2020} } @article{MTMT:31372620, title = {A rejtelmes dolomit}, url = {https://m2.mtmt.hu/api/publication/31372620}, author = {Haas, János and Hips, Kinga}, doi = {10.23928/foldt.kozl.2020.150.2.233}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {150}, unique-id = {31372620}, issn = {0015-542X}, year = {2020}, eissn = {2559-902X}, pages = {233-266}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X} } @article{MTMT:31471257, title = {Fault-controlled dolostone geometries in a transgressive-regressive sequence stratigraphic framework}, url = {https://m2.mtmt.hu/api/publication/31471257}, author = {Yao, Shuqing and Gomez-Rivas, Enrique and Martin-Martin, Juan Diego and Gomez-Gras, David and Trave, Anna and Griera, Albert and Howell, John A.}, doi = {10.1111/sed.12739}, journal-iso = {SEDIMENTOLOGY}, journal = {SEDIMENTOLOGY}, volume = {67}, unique-id = {31471257}, issn = {0037-0746}, abstract = {This study investigates the geometries of fault-controlled dolostone geobodies and their structural and sequence stratigraphic controls, which provide new insights for the prediction and production of fault-controlled dolomitized hydrocarbon reservoirs. A very thick succession (>1600 m) of Aptian-Albian shallow-marine carbonates of the Benassal Formation that crop out in the Benicassim area (Maestrat Basin, eastern Spain) is partly replaced by dolomite, resulting in dolostone geometries ranging from massive patches to stratabound bodies. Detailed mapping, systematic logging and correlation were carried out to characterize the structural, sedimentary and sequence stratigraphic framework of the area and to constrain the principal controls on the full-range of dolostone geometries. The results show that carbonate sediments accumulated in a half graben stacked in three transgressive-regressive sequences. Large-scale massive dolostone patches (with up to kilometre extension) formed near large-scale faults indicating that they acted as entry points for warm dolomitizing fluids into the basin. These dolostone patches laterally pass to large stratabound bodies that extend for long distances (at least 7 km) away from feeding faults, forming a continuum. The presence of a regional unconformity and a clastic fine-grain low-permeability unit (Escucha Formation) on top of the Benassal Formation likely constrained the dolomitization fluids to an up to 580 m thick interval below the base of the Escucha Formation. Thus, only limestones within this interval, corresponding to the two uppermost transgressive-regressive sequences, were dolomitized. There is a clear relationship between the stratigraphic framework and the preferred replaced beds. Dolomitization preferentially affected sediments deposited in inner to middle ramp settings with predominant wackestone to packstone textures. Such facies are laterally most abundant in the east of the study area (i.e. basinward) and vertically in layers around the maximum flooding zone of the top sequence, which is preferentially affected by dolomitization.}, keywords = {diagenesis; Aptian-Albian; fault-controlled dolomitization; Maestrat Basin; outcrop analogue; stratigraphic sequence}, year = {2020}, eissn = {1365-3091}, pages = {3290-3316}, orcid-numbers = {Gomez-Rivas, Enrique/0000-0002-1317-6289; Gomez-Gras, David/0000-0002-8539-5739; Trave, Anna/0000-0002-2735-3733} } @mastersthesis{MTMT:30545269, title = {Upper triassic conodonts from the Csővár area and the Buda Hills, Hungary and their geologial applications}, url = {https://m2.mtmt.hu/api/publication/30545269}, author = {Karádi, Viktor}, doi = {10.15476/ELTE.2018.098}, publisher = {Eötvös Loránd University}, unique-id = {30545269}, year = {2019}, orcid-numbers = {Karádi, Viktor/0000-0002-5923-2944} } @article{MTMT:31081129, title = {RELATIONSHIP BETWEEN ORIGIN AND DISTRIBUTION OF DOLOMITES IN LOWER PALEOZOIC, JIZHONG DEPRESSION, NORTH CHINA}, url = {https://m2.mtmt.hu/api/publication/31081129}, author = {Yan, W and Jin, Z and Yao, M and Zhao, W}, journal-iso = {FRESEN ENVIRON BULL}, journal = {FRESENIUS ENVIRONMENTAL BULLETIN}, volume = {28}, unique-id = {31081129}, issn = {1018-4619}, abstract = {The origin and distribution of the Lower Paleozoic dolomites in the Jizhong Depression, North China, are related and affect the distribution of the reservoir. The Lower Paleozoic dolomites can be divided into four types: Type-A is gypsiferous mud silt -sized crystalline dolomites; Type-B is non-gypsiferous mud-silt-sized crystalline dolomites; Type C is silt-fine-sized crystalline dolomites; Type-D is medium-coarse-sized crystalline dolomites. Type-A dolomites contains gypsum, with stratiform stromatolites, bird's eye structures and brecciated structures. The ordering of dolomites averages 0.56. delta C-13 averages -0.155 parts per thousand (PDB) and delta O-18 averages -5.669 parts per thousand (PDB). Type-B dolomites are gypsum-free and not associated with gypsum bed. delta C-13 averages -2.114 parts per thousand (PDB). The rest of the characteristic are similar to type A. Type-C dolomites are subhedral and euhedral. Metasomatic relict structure are common. The ordering of dolomites averages 0.75. delta C-13 averages -0.693 parts per thousand (PDB) and delta O-18 averages -6.079 parts per thousand (PDB). Cathodoluminescence is orange and represents zonal structure. Type-D dolomites are subhedral or anhedral. Mosaic structure, recrystallization and residual porphyritic features are common. The ordering of dolomites averages 0.86. delta C-13 averages -1.433 parts per thousand (PDB) and delta O-18 averages -0.149 parts per thousand (PDB). The homogenization temperature of inclusions ranges between 90-330 degrees C. Cathodoluminescence is dark brown. Type-A dolomites and Type-B dolomites are thin, with a small horizontal distribution, but the number of dolomite layer is more. Type-C dolomites have large thickness and large horizontal distribution. It is generally distributed under Type-A and Type-B dolomites. Type-D dolomites have a massive distribution with a large vertical thickness. The range of horizontal distribution is relatively small. These characteristics can be used to analyze the original rock of dolomite, dolomitization temperature, strati graphic burial history, the occurrence time of dolomitization, and the source of magnesium ions. It is indicated that Type-A and Type-B dolomites are formed in tidal flat environment. Type-A dolomites are formed as a result of evaporative pumping. The origin of T-B dolomites are similar to that of dolomite in Andros Island, Bahamas. Type-C dolomites are formed as a result of seepage reflex dolomitization, and have a sandwich structure. Type-D dolomites are formed as a result of burial hydrothermal dolomitization, closely related to the deep faults of the Himalayan Movement and Cenozoic magmatic rocks. These dolomitizations result in different patterns of dolomite distribution. Type-A, Type-B and Type-D dolomites underwent dissolution during the formation process, and could form good reservoirs for oil and gas.}, keywords = {dolomite; North China Platform; Jizhong Depression; Lower Paleozoic; Seepage reflux dolomitization; Hydrothermal dolomitization}, year = {2019}, eissn = {1610-2304}, pages = {3946-3962} } @article{MTMT:3399845, title = {Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary)}, url = {https://m2.mtmt.hu/api/publication/3399845}, author = {Garaguly, István and Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Schubert, Félix and Czuppon, György and Frei, R}, doi = {10.1016/j.marpetgeo.2018.07.024}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {98}, unique-id = {3399845}, issn = {0264-8172}, year = {2018}, eissn = {1873-4073}, pages = {270-290}, orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Schubert, Félix/0000-0001-8647-5354; Czuppon, György/0000-0002-7231-6042} } @article{MTMT:3352489, title = {Dolomittest a tatai Kálvária-domb alsó-jura mészkövében}, url = {https://m2.mtmt.hu/api/publication/3352489}, author = {Győri, Orsolya and Mindszenty, Andrea and Haas, János and Czuppon, György}, doi = {10.23928/foldt.kozl.2018.148.1.27}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {148}, unique-id = {3352489}, issn = {0015-542X}, year = {2018}, eissn = {2559-902X}, pages = {27-34}, orcid-numbers = {Győri, Orsolya/0000-0002-3646-9113; Mindszenty, Andrea/0000-0001-8927-3053; Haas, János/0000-0003-0929-8889; Czuppon, György/0000-0002-7231-6042} } @article{MTMT:3420027, title = {Evidences for pre-orogenic passive-margin extension in a Cretaceous fold-and-thrust belt on the basis of combined seismic and field data (western Transdanubian Range, Hungary)}, url = {https://m2.mtmt.hu/api/publication/3420027}, author = {Héja, Gábor and Kövér, Szilvia and Csillag, Gábor and Németh, A and Fodor, László}, doi = {10.1007/s00531-018-1637-3}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {107}, unique-id = {3420027}, issn = {1437-3254}, abstract = {Combined sedimentological and structural analysis was carried out in the field and on 2D seismic reflection profiles to recognize pre-orogenic structures in a Cretaceous fold-and-thrust belt. Detailed field observations were made in the Keszthely Hills, Western Hungary, while 2D seismic interpretation was carried out in the neighbouring Zala Basin. As a result, a fault-controlled intraplatform basin system was identified by a detailed analysis of bounding faults, and related outcrop-scale structures. The Norian–Rhaetian (227–201.3 Ma) synsedimentary faulting was associated with talus breccia formation, small-scale faulting, and dyke formation, in addition to slumping and other soft-sediment deformations. Based on the distribution of talus breccia, WNW–ESE-trending map-scale normal faults were identified in the Keszthely Hills, which is in agreement with the directly observed outcrop-scale synsedimentary faults. On seismic sections, similar WNW- or NW-trending Late Triassic normal faults were identified based on thickness variations of the syn-rift sediments and the presence of wedge-shaped bodies of talus breccia. Normal faulting occurred already in the Norian, and extensional tectonics was active through the Early and Middle Jurassic. The Late Triassic grabens of the western Transdanubian Range could be correlated with those in western part of the Southern Alps, and the Bajuvaric nappe system of the Northern Calcareous Alps. These grabens were situated on the proximal Adriatic margin, and they represent the first sign of the Alpine Tethys rifting. The locus of extension was laterally migrated westward, towards the distal Adriatic margin during Early and Middle Jurassic. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature.}, keywords = {SYSTEM; SOUTHERN ALPS; Pannonian Basin; tectonic evolution; Back-arc basins; Pre-orogenic extension; Synsedimentary deformation; Norian tectonics; Alpine Tethys rifting; NORTHERN CALCAREOUS ALPS; STRUCTURAL INHERITANCE; ADRIATIC FORELAND; NORMAL FAULTS}, year = {2018}, eissn = {1437-3262}, pages = {2955-2973}, orcid-numbers = {Kövér, Szilvia/0000-0002-6736-4226} } @article{MTMT:3351776, title = {Middle Norian conodonts from the Buda Hills, Hungary: an exceptional record from the western Tethys}, url = {https://m2.mtmt.hu/api/publication/3351776}, author = {Karádi, Viktor}, doi = {10.1007/s41513-017-0009-3}, journal-iso = {J IBER GEOL}, journal = {JOURNAL OF IBERIAN GEOLOGY}, volume = {44}, unique-id = {3351776}, issn = {1698-6180}, abstract = {Purpose: Recent biostratigraphic investigations of pelagic dolomites in the Buda Hills area, Hungary provided unique Middle Norian conodont assemblages. Due to the poorly represented Tethyan record of similar faunas and the present state of our knowledge of Alaunian conodonts, finer age assignment could not have been carried out. The purpose of this study is to discuss the natural cause (sedimentary, tectonic and paleoecological) and artificial biases (lumping taxonomy and inadequate figuration) that led to a scarce representation of the Alaunian conodont record. Further aims are to present here several taxonomic, systematic, and biostratigraphic notes on the Middle Norian conodonts based on the rich material recovered. Methods: Rock samples were processed using standard dissolution technique of dilute acetic acid. Scanning micro-photographs were taken of the conodont specimens from three views. Results: Remarks are added to the problematic species Epigondolella abneptis and Mockina postera, and some aspects for improvement of the Middle Norian conodont biostratigraphy are suggested. Detailed systematic descriptions of 3 genera and 15 species are given. The observed faunas include 5 previously unknown forms, namely Epigondolella aff. vialovi, Mockina aff. matthewi, M. aff. postera, M. aff. spiculata and Mockina sp. A. The Tethyan occurrence of Epigondolella transitia, a transitional Lower/Middle Norian conodont species previously known only from North America, is documented. Conclusions: The assemblage lets an insight into the main characteristics of the Lacian/Alaunian faunal turnover and into the evolutionary trends that resulted in the origination of the last representatives of conodonts of the Sevatian and the Rhaetian. The new conodont record of the Buda Hills highlights the fact that Alaunian conodonts are less known among Upper Triassic faunas. This work suggests the route of the future studies for a more precise and global applicability of conodonts in the Middle Norian biostratigraphy. © 2017, Springer International Publishing Switzerland.}, keywords = {ORIGIN; Hungary; Austria; biostratigraphy; BOUNDARY; Buda hills; Conodonts; magnetostratigraphy; Spiculata; Epigondolella; RHAETIAN STAGE; LAGONEGRO BASIN; GSSP CANDIDATE; SOUTHERN APENNINES; POLARITY TIME-SCALE; SECTION SOUTHWESTERN TURKEY; State-of-the-art; Alaunian}, year = {2018}, eissn = {1886-7995}, pages = {155-174}, orcid-numbers = {Karádi, Viktor/0000-0002-5923-2944} } @article{MTMT:3202162, title = {Középső-triász dolomitok képződésének története és töréses deformációja a Szegedi-medence területén}, url = {https://m2.mtmt.hu/api/publication/3202162}, author = {Garaguly, István and Raucsik, Béla and Raucsikné Varga, Andrea Beáta and Schubert, Félix}, doi = {10.23928/foldt.kozl.2017.147.1.39}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {147}, unique-id = {3202162}, issn = {0015-542X}, year = {2017}, eissn = {2559-902X}, pages = {39-60}, orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Schubert, Félix/0000-0001-8647-5354} } @article{MTMT:3091740, title = {Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis}, url = {https://m2.mtmt.hu/api/publication/3091740}, author = {Haas, János and Hips, Kinga and Budai, Tamás and Győri, Orsolya and Lukoczki, Georgina and Kele, Sándor and Demény, Attila and Poros, Zsófia}, doi = {10.1007/s00531-016-1347-7}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {106}, unique-id = {3091740}, issn = {1437-3254}, year = {2017}, eissn = {1437-3262}, pages = {991-1021}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Győri, Orsolya/0000-0002-3646-9113; Lukoczki, Georgina/0000-0002-0661-0198; Kele, Sándor/0000-0002-8607-7636; Demény, Attila/0000-0003-0522-9018} }