TY - CHAP AU - Ozsvárt, Péter AU - Vető, István AU - Nagymarosy, András ED - Bosnakoff, Mariann ED - Főzy, István TI - A paleogén-medence fejlődése a korai oligocénben mikropaleontológiai és geokémiai adatok tükrében T2 - 22. Magyar Őslénytani Vándorgyűlés, Döbrönte. Program, előadáskivonatok, kirándulásvezető PB - Magyarhoni Földtani Társulat CY - Budapest SN - 9789638221759 PY - 2019 SP - 28 EP - 28 PG - 1 UR - https://m2.mtmt.hu/api/publication/31971213 ID - 31971213 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Albert, Gáspár TI - A kõpatak völgye JF - TERMÉSZET VILÁGA J2 - TERMÉSZET VILÁGA VL - 144 PY - 2013 IS - 2 SP - 85 EP - 86 PG - 2 SN - 0040-3717 UR - https://m2.mtmt.hu/api/publication/2209355 ID - 2209355 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Kerékgyártó, Tamás TI - Ipari célú hévíz kútpár tervezése Úri (Pest megyei település) térségében JF - HIDROLÓGIAI TÁJÉKOZTATÓ J2 - HIDROLÓGIAI TÁJÉKOZTATÓ VL - 50 PY - 2011 IS - 1 SP - 40 EP - 41 PG - 2 SN - 0439-0954 UR - https://m2.mtmt.hu/api/publication/3110525 ID - 3110525 N1 - # Kötet üres: Kötet ismeretlen LA - Hungarian DB - MTMT ER - TY - JOUR AU - Sebe, Krisztina AU - Csillag, Gábor AU - Thamóné Bozsó, Edit TI - Platóhelyzetű eolikus üledékek és formák az Agár-tető bazaltfennsíkján (Déli-Bakony). Mountain-top aeolian deposits and ventifacts on the basalt plateau of Agár-tető (Southern Bakony, Hungary) TS - Mountain-top aeolian deposits and ventifacts on the basalt plateau of Agár-tető (Southern Bakony, Hungary) JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 141 PY - 2011 IS - 4 SP - 393 EP - 399 PG - 7 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/2076240 ID - 2076240 AB - Mountain-top or cliff-top aeolian deposits are a special type of aeolian sediment, which are transported upwards along steep or even vertical slopes by the wind. Most of the published occurrences are of Holocene age. In Europe, they have been reported from a few sites along the western margin of the continent. Here we describe aeolian deposits covering the extensive basalt plateau of Agár-teto in the Transdanubian Range (Southern Bakony). The deposits have a thickness of around 0.5 m on horizontal surfaces, while in wind shadow they can be several metres thick. They are mainly medium-sorted, with grain sizes ranging from clay to fine gravel but the dominant type is fine sand. The majority of the grains are quartz and probably originated from the north - i.e. from Lake Pannon sediments underlying the basalt. The sediment material itself must have been transported onto the plateau by strong winds during the Pleistocene glacials. Trapping was most probably caused by the coarse surface roughness (i.e. a surface strewn with basalt blocks), by vegetation cover and, in the case of thick accumulations, by the topographical position. Strong aeolian activity is indicated by wind-fluted basalt blocks as well. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Czira, Tamás AU - Tipold, F. TI - A magyar szakpolitikai területi értékelési rendszer intézményesülése, főbb eredményei, kihívásai. JF - FALU VÁROS RÉGIÓ J2 - FALU VÁROS RÉGIÓ PY - 2010 IS - 1 SP - 4 EP - 9 PG - 6 SN - 1218-2613 UR - https://m2.mtmt.hu/api/publication/32211767 ID - 32211767 LA - Hungarian DB - MTMT ER - TY - BOOK AU - Fancsik, Tamás ED - Balla, Zoltán ED - Piros, Olga TI - A Magyar Állami Földtani Intézet Évi Jelentése (2009) ET - 0 PB - Magyar Állami Földtani Intézet (MÁFI) CY - Budapest PY - 2010 SP - 378 UR - https://m2.mtmt.hu/api/publication/3037596 ID - 3037596 LA - English DB - MTMT ER - TY - JOUR AU - Albert, Gáspár TI - Volumetric modelling of cavities and pores in the Pál-völgy Cave, Budapest. A budapesti Pál-völgyi-barlang üreg- és pórustérfogatának modellezése TS - A budapesti Pál-völgyi-barlang üreg- és pórustérfogatának modellezése JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 140 PY - 2010 IS - 3 SP - 263 EP - 280 PG - 18 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1768076 ID - 1768076 N1 - Megjegyzés-24492344 Hiányzó Besorolás: 'A budapesti pál-völgyi-barlang üreg- és pórustérfogatának modellezése',24 Admin megjegyzés-24492344 tblsubtype: (name,DocTypeID) ('A budapesti pál-völgyi-barlang üreg- és pórustérfogatának modellezése',24) #Besorolás Cited By :3 Export Date: 26 November 2019 Correspondence Address: Gáspár, A.; Magyar Állami Földtani Intézet, 1143 Budapest, Stefánia út 14, Hungary AB - The aim of this study was the determination of the respective volumes of the cavities in the Pál-völgy Cave (Budapest) and the confirmation of the post-diagenetic origin of the porosity in the incorporating carbonate rock body. This was done by measuring the size and frequency of the fractures and solution marks in the vicinity of the cave. For this a volumetric and a porosity model of the cave and its environs was constructed. This new method for volumetric cave modelling also solved the problem of processing cave maps from archives and data acquired by quick measurement.This involved producing volumetric data with highly accurate mathematical approaches. Furthermore, the value of this new, mostly theoretical, approach for volumetric cave modelling was reinforced by the porosity model, which was based on field measurements. Through the modelling, an estimation of the probable, but still not explored size of the Pál-völgy Cave was also calculated. LA - English DB - MTMT ER - TY - JOUR AU - Kovács-Pálffy, P AU - Földessy, János AU - Kónya, Péter AU - Bertalan, Éva TI - Bentonite deposits of Hungary – a review of their mineralogy and geology. JF - ACTA MINERALOGICA PETROGRAPHICA - ABSTRACT SERIES J2 - ACTA MINERAL PETROGR ABSTRACT SER VL - 6 PY - 2010 SP - 308 EP - 308 PG - 1 SN - 1589-4835 UR - https://m2.mtmt.hu/api/publication/1378829 ID - 1378829 N1 - Abstract Series, MECC2010, Budapest, Hungary 25-29/08/2010 LA - English DB - MTMT ER - TY - CONF AU - HORVáTH, É. AU - JORDÁN, Gy. AU - Fügedi, Ubul AU - BARTHA, A. AU - BALLÓK, M. AU - KUTI, L. AU - HELTAI, GY. AU - KALMÁR, J. AU - WALDMANN, I. AU - NAPRADEAN, I. AU - DAMIAN, G. TI - Nehézfém-szennyezések vizsgálata felhagyott bányaterületeken. Erdélyi esettanulmány. T2 - VIII. Földtudományi Ankét, Nagykanizsa, C1 - Nagykanizsa PY - 2009 SP - 2 EP - 2 PG - 1 UR - https://m2.mtmt.hu/api/publication/31305409 ID - 31305409 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Albert, Gáspár TI - Az észlelési földtani térképek digitális feldolgozásának /archiválásának menete JF - MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE J2 - M ÁLL FÖLDT INT JELENT VL - 2007 PY - 2009 SP - 45 EP - 53 PG - 9 SN - 0368-9751 UR - https://m2.mtmt.hu/api/publication/1878516 ID - 1878516 AB - During geological surveying the most important objects, besides the hammer and loupe, are the maps and notes. The basic geological data are recorded cartographically on a map with reference key and literally in a booklet. These data are the most genuine information, which can be accessed later, that’s why the preservation of the original notes should be an important aim for an institution, which performs regular scientific observations. In the Geological Institute of Hungary, where geological mapping is one of the primary functions for nearly 140 years, the data of manuscripts are hardly or inaccessible because of the difficulty of cataloging and organizing of them. The needs of recent times make it necessary, the technological frames make it possible to use geological information in the scale of observation, which means the use of authentic data. To achieve this, a method has been worked out, which aimed to transform the information of draw-up maps and field note manuscripts into a unified form, which can be compared with other databases, to insert them into a geographical information system, to create a uniform layout for the digitalized maps, and to operate a functional data storage system. In the study performed, the frames and main connections of this method on demonstrated cases have been revealed. LA - Hungarian DB - MTMT ER -