| Dégi, Júlia, Abart, Rainer, Török, Kálmán, Rhede, Dieter, Petrishcheva, Elena (2009) Evidence for xenolith–host basalt interaction from chemical patterns in Fe–Ti-oxides from mafic granulite xenoliths of the Bakony–Balaton Volcanic field (W-Hungary) Mineralogy and Petrology, 95 (3) 219-234 doi:10.1007/s00710-008-0035-0 | Journal (article/letter/editorial) | granulite xenoliths of the Bakony–Balaton Volcanic field (W-Hungary) Júlia Dégi & Rainer Abart & Kálmán Török...Optics of the Hungarian Academy of Sciences, Konkoly-Thege út 29-33, H-1121 Budapest, Hungary e-mail: julia...Geophysical Institute of Hungary, Kolumbusz u. 17-23, H-1145 Budapest, Hungary D. Rhede GFZ German Research...Basin. In the Bakony–BalatonHighland Volcanic Field of Western-Hungary material from the deep lithosphere...amphibole) from the Bakony– Balaton-Highland Volcanic Field have been subject to a number of studies (e | | Török, Kálmán, Németh, Bianka, Koller, Friedrich, Dégi, Júlia, Badenszki, Eszter, Szabó, Csaba, Mogessie, Aberra (2014) Evolution of the middle crust beneath the western Pannonian Basin: a xenolith study. Mineralogy and Petrology, 108 (1) 33-47 doi:10.1007/s00710-013-0287-1 | Journal (article/letter/editorial) | Geophysical Institute of Hungary, 1145 Budapest, Columbus u. 17-21, Hungary e-mail: torok.kalman@mfgi...University, 1117 Budapest, Pázmány Péter sétány 1/C, Hungary A. Mogessie Institute of Mineralogy and Petrology...Highland Volcanic Field, LHPVF Little Hungarian Plain Volcanic Field, NGVF Nógrád– Gömör Volcanic Field, PMVF...PMVF Persani Mountains Volcanic Field, SBVF Styrian Basin Volcanic Field. Hills and mountains are shown...is based on the Geological map of Hungary 1:200 000 (L-33-XII-Veszprém), modified after Jugovics (1968) | | | Journal (article/letter/editorial) | megacrysts from basaltic tuff (Szentbékkálla, western Hungary) Kálmán Török a,*, Eniko" Bali b, Csaba Szabó...for Geophysics and Environmental Physics of the Hungarian Academy of Sciences, Department of Geophysics...Pázmány Peter sétány 1/C, H-1117 Budapest, Hungary b Lithosphere Fluid Research Laboratory, Department...Pázmány Peter sétány 1/C, H-1117 Budapest, Hungary Received 22 March 2002; accepted 26 September 2002...Szentbékkálla (Bakony – Balaton Highland, western Hungary). The barite droplets contain 3.22 – 14.7 wt.% | | Demény, A., Dallai, L., Frezzotti, M.-L., Vennemann, T.W., Embey-Isztin, A., Dobosi, G., Nagy, G. (2010) Origin of CO2 and carbonate veins in mantle-derived xenoliths in the Pannonian Basin. Lithos, 117 (1) 172-182 doi:10.1016/j.lithos.2010.02.013 | Journal (article/letter/editorial) | Geochemical Research, Hungarian Academy of Sciences, Budaörsi út 45., H-1112, Budapest, Hungary CNR-Ist. Geoscienze...and Petrology, Hungarian Natural History Museum, Budapest, Ludovika tér 2., H-1088, Hungary b a r t i c...in peridotite xenoliths of the Pannonian Basin, Hungary, were investigated by means of petrographic investigation...basaltic rocks of the Balaton Highland, Central Hungary. Based on melting point and homogenization temperature...xenoliths, clinopyroxene, amphibole, spinel and magnetite megacrysts as well as lower crustal granulite | | Demény, A, Vennemann, T.W, Hegner, E, Nagy, G, Milton, J.A, Embey-Isztin, A, Homonnay, Z, Dobosi, G (2004) Trace element and C–O–Sr–Nd isotope evidence for subduction-related carbonate–silicate melts in mantle xenoliths (Pannonian Basin, Hungary) Lithos, 75 (1) 89-113 doi:10.1016/j.lithos.2003.12.016 | Journal (article/letter/editorial) | carbonate–silicate melts in mantle xenoliths (Pannonian Basin, Hungary) A. Demény a,*, T.W. Vennemann b,1, E. Hegner...Geochemical Research, Hungarian Academy of Sciences, Budaörsi út 45, H-1112 Budapest, Hungary b Institute for...and Petrology, Hungarian Natural History Museum, Ludovika tér 2, H-1088 Budapest, Hungary f Department...University, Pázmány P. s. 2, H-1117 Budapest, Hungary Received 11 December 2002; received in revised...from Szentbékálla (Balaton Highland, Central Hungary). Strong resorption of amphibole suggests multiple | | | Journal (article/letter/editorial) | AND PETROLOGY, HUNGARIAN NATURAL HISTORY MUSEUM, LUDOVIKA TÉR 2,1083 BUDAPEST, HUNGARY RECEIVED OCTOBER...xenoliths from Pliocene alkali basalts of western Hungary represent the lower crust of the Pannonian Basin...xenoliths have higher 143Nd/144Nd and fall within the field of local lithospheric upper mantle. The material...evidence of the nature of the lower crust beneath volcanic regions (e.g. Griffin & O’Reilly, 1987; Rudnick... Bondoróhegy—Bo) in the Balaton Highlands of Hungary, north-west of Lake Balaton (Fig. 1). The host | | | Report (volume) | Prepared for the Society of Economic Geologists Field Conference — 4-13 September 1999 Series Editor:...Epithermal Mineralization of the Tokaj Mtns., Northeast Hungary: Shallow Levels of Low-Sulfidation Type Systems...Mineralization of the Matra Mountains, Northeast Hungary iGaiter, F Moinar,,.J. Poldessy, 1 zZelenka, J...cee ssee eae The Central Slovakia Neogene Volcanic Field: A Review MUR ONC oS LONG SOMA VYAAO) SURE...ee 181 Metallogeny of the Central Slovakia Volcanic Field PONE Mecencn a Cenc aiste save BST en elects | | | Journal (article/letter/editorial) | com/locate/lithos Origin of basaltic magmas of Perşani volcanic field, Romania: A combined whole rock and mineral...Research Group, Pázmány sétány 1/C, H-1117 Budapest, Hungary Department of Petrology and Geochemistry, Eötvös...University, Pázmány sétány 1/C, H-1117 Budapest, Hungary Institute of Geodynamics, Romanian Academy, 19-21...Monogenetic volcanic field Magmagenesis Carpathian–Pannonian region a b s t r a c t The Perşani volcanic field...monogenetic volcanic field in the Carpathian–Pannonian region, eastern-central Europe. Volcanic activity | | Patkó, Levente, Liptai, Nóra, Kovács, István János, Aradi, László Előd, Xia, Qun-Ke, Ingrin, Jannick, Mihály, Judith, O'Reilly, Suzanne Y., Griffin, William L., Wesztergom, Viktor, Szabó, Csaba (2019) Extremely low structural hydroxyl contents in upper mantle xenoliths from the Nógrád-Gömör Volcanic Field (northern Pannonian Basin): Geodynamic implications and the role of post-eruptive re-equilibration. Chemical Geology, 507. 23-41 doi:10.1016/j.chemgeo.2018.12.017 | Journal (article/letter/editorial) | upper mantle xenoliths from the Nógrád-Gömör Volcanic Field (northern Pannonian Basin): Geodynamic implications...upper mantle xenoliths from the Nógrád-Gömör Volcanic Field (northern Pannonian Basin): Geodynamic implications...upper mantle xenoliths from the Nógrád-Gömör Volcanic Field (northern Pannonian Basin): geodynamic implications...and Earth Sciences, Eötvös University, Budapest, Hungary b CCFS-GEMOC, Department of Earth and Planetary...Astronomy and Earth Sciences, Hungarian Academy of Sciences Sopron, Hungary d School of Earth Sciences, | | Patkó, Levente, Liptai, Nóra, Aradi, László Előd, Klébesz, Rita, Sendula, Eszter, Bodnar, Robert J., Kovács, István János, Hidas, Károly, Cesare, Bernardo, Novák, Attila, Trásy, Balázs, Szabó, Csaba (2020) Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths. Geoscience Frontiers, 11 (3) 943-964 doi:10.1016/j.gsf.2019.09.012 | Journal (article/letter/editorial) | in the upper mantle beneath the NógrádGömör Volcanic Field (Northern Pannonian Basin): evidence from xenoliths...in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): evidence from xenoliths...in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): evidence from xenoliths...and Earth Sciences, Eötvös University, Budapest, Hungary b Isotope Climatology and Environmental Research...Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary c CCFS-GEMOC, Department of | | | Journal (article/letter/editorial) | magma bodies, between intrusions and overlying volcanic centres as well as magma-sediments interactions...in transfer and emplacement mechanisms between volcanic and plutonic systems (magma transfer via dykes...(Rocchi et al. 2002; Petford et al. 2000). In volcanic complexes, sequentially emplaced magma batches...of plagioclase, sizes of both are 2 mm. Titan–magnetite (0.2 mm) develops around pyroxene grains. The... 0.3–3 mm. The rock contains a lot of titano–magnetite that concentrates with crystals of pyroxene. Comparative | | | Report (issue) | element spidergram refers to the lavas of the Veneto Volcanic Province (see Beccaluva et al., Chapter 7). Background:...tholeiite magma generation in the Paleogene Veneto volcanic province, southern Alps ....131 L. Beccaluva,...processes in the magma genesis of the Phlegrean Volcanic District, Southern lal ssn sic oe es eos 2 oe 2 es...The geochemical peculiarity of “Plio-Quaternary” volcanic rocks of Sardinia in the circum-Mediterranean:...history of the region remains a matter of debate. Volcanic activity is widespread, with the production of | | | Report (issue) | currents Frans deRooij and Stuart Dalziel 219 Field-based approaches Formation of large-scale shear...reconstruction of the Bakony–Balaton Highland Volcanic Field, Hungary Kàroly Németh 279 Synsedimentary deformation...the turbidites community, and as a pioneer in the field of autosuspension. The grouping of papers within...individual flow processes; and new insights from field research. Research on particulate gravity currents...systems (Komar, 1977; Stacey & Bowen, 1988a,b). Little consideration has been given to the process of | | | Book | Contamination: Constraints From Experimental and Field Evidences Antonio Castro, Carmen Rodríguez, Juan...The petrological and geochemical signatures of volcanic and plutonic rocks reflect the diversity of the...of modern studies modeling the architecture of volcanic plumbing systems. Specifically, minerals, melts...including storage, recharge, and ascent through volcanic conduits. These different petrologic themes provide...It was clear since then that the complexity of volcanic processes and the compositional variability of |
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