Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Thomas Pieter Lange"'
Autor:
Peter Tollan, José Alberto Padrón-Navarta, Jörg Hermann, István Kovács, Márta Berkesi, Thomas Pieter Lange, Levente Patkó, Csaba Szabó, László Előd Aradi, Nóra Liptai
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Orsolya Gelencsér, András Papucs, Csaba Szabó, Ákos Kővágó, Ábel Szabó, Csilla Király, György Falus, Attila Demény, Dóra Cseresznyés, Sándor Gyila, Alexandru Szakács, Ágnes Gál, István Kovács, György Czuppon, Thomas Pieter Lange, László Palcsu
Publikováno v:
Goldschmidt2021 abstracts.
Nominally anhydrous minerals in the lithospheric mantle, such as olivine and pyroxenes can host a small amount (tens to hundreds of ppm) of structurally bound hydroxyl (‘water’). Numerous studies pointed out that water has a strong effect on the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e90f279eafbfce2d79dd99b9bee48f5
https://doi.org/10.5194/egusphere-egu2020-19001
https://doi.org/10.5194/egusphere-egu2020-19001
Autor:
Thomas Pieter Lange, Zsófia Pálos, Ábel Szabó, Levente Patkó, László Előd Aradi, Csaba Szabó, Márta Berkesi, Nóra Liptai, István Kovács
Amphibole is one of the most abundant ’water’-bearing minerals in the Earth’s upper mantle. Amphiboles occur as interstitial grains, lamellae within pyroxenes or as daughter minerals within fluid inclusions. Most commonly amphibole formation is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2172616b43842998ab372068b230f9d
https://doi.org/10.5194/egusphere-egu2020-1192
https://doi.org/10.5194/egusphere-egu2020-1192
Autor:
István Kovács, Márta Berkesi, Mihály Pósfai, Péter Pekker, Nóra Liptai, Thomas Pieter Lange, Csaba Szabó, Zsófia Pálos
Transmission electron microscopy (TEM) is a powerful, yet scarcely used technique when it comes to investigating mantle minerals and fluid inclusions. It is capable to collect structural information of the studied mineral, its precise chemical compos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8846137c1c3c7815c983edc457d5c377
https://doi.org/10.5194/egusphere-egu2020-19844
https://doi.org/10.5194/egusphere-egu2020-19844
Autor:
Nóra Liptai, Levente Patkó, Thomas Pieter Lange, László Előd Aradi, Marta Berkesi, Csaba Szabó, István János Kovács
Publikováno v:
Goldschmidt Abstracts.
Autor:
Attila Novák, Tamás Fancsik, Viktor Wesztergom, Nóra Liptai, Thomas Pieter Lange, Levente Patkó, Csaba Szabó, Alexandru Szakács, István Kovács, Alexander Koptev, Mircea Radulian, Sierd Cloetingh, Liviu Mațenco, Márta Berkesi, Gábor Molnár
Publikováno v:
Global and Planetary Change, 204, 1. Elsevier
Apart from the lithosphere-asthenosphere boundary (LAB), mid-lithospheric discontinuities (MLDs) in thick and old continental lithospheres appear to play an important role in global plate tectonics. Initiation of intra-continental subduction, delamin
Autor:
Levente Patkó, Attila Novák, István Kovács, László Csontos, Viktor Wesztergom, Thomas Pieter Lange, Nóra Liptai, Csaba Szabó, Rita Klébesz, Gábor Molnár
Publikováno v:
Global and Planetary Change. 197:103389
Long period magnetotelluric (MT) data were collected at 14 locations along a ~50 km long NNW-SSE profile in the Nograd-Gomor Volcanic Field (NGVF), which is one of the five mantle xenolith bearing Neogene alkali basalt locations in the Carpathian-Pan
Autor:
László Előd Aradi, Nóra Liptai, István Kovács, Zsanett Pintér, Thomas Pieter Lange, Márta Berkesi, Levente Patkó, Csaba Szabó
Publikováno v:
Global and Planetary Change. 196:103364
Incorporation of hydrogen as structural hydroxyl (commonly referred to as water) in nominally anhydrous mantle minerals is known for the ‘hydrolytic weakening’ effect, which decreases the strength and electrical resistivity of the rock. Recent mo
Autor:
Csaba Szabó, Thomas Pieter Lange, István Kovács, Levente Patkó, László Előd Aradi, Nóra Liptai, Orsolya Gelencsér
Publikováno v:
Földtani Közlöny. 149:233
A felsőköpenyből származó xenolitok kőzettani és geokémiai vizsgálatával közvetlen ismeretekhez juthatunk a litoszféra fizikai és kémiai állapotáról. Ezen információk birtokában kiszámíthatók a xenolitok által jellemzett köpe