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Central European Geology
Authors:
Ildikó Gyollai
,
Ákos Kereszturi
, and
Elias Chatzitheodoridis

new phases occur in order to highlight the conditions of alterations occurring in the microscopic scale. Based on earlier publications, many impact melt zones indicative of high temperature are present in Zagami ( Malavergne et al. 2001

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LL5 (Impact melt zone) 26 42 14 Chelyabinsk LL5 (after shock loading) 20 85 30

Open access
Central European Geology
Authors:
Arnold Gucsik
,
Tasuku Okumura
,
Hirotsugu Nishido
,
Ildikó Gyollai
,
Kiyotaka Ninagawa
,
Natalie Deseta
, and
Péter Rózsa

. – Physical Reviews , B27 , pp. 3780 – 3795 . Osinski , G.R. 2004 : Impact melt rocks from the Ries impact structure, Germany: an origin as impact melt flows

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Central European Geology
Authors:
Ildikó Gyollai
,
Ildikó Gyollai
,
Szaniszló Bérczi
,
Krisztián Fintor
,
Szabolcs Nagy
, and
Arnold Gucsik

. Mittlefehldt , D.W. , M.M. Lindstrom 2001 : Petrology and geochemistry of Patuxent Range 91501, a clast-poor impact melt from the L-chondrite parent body and Lewis Cliff 88663, an L7 chondrite . – Meteoritics and Planetary Science 36 , pp. 439

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Central European Geology
Authors:
Ildikó Gyollai
,
Ákos Kereszturi
,
Zsolt Kereszty
,
Máté Szabó
, and
Elias Chatzitheodoridis

( Stöffler et al. 1991 ). Wittmann et al. ( 2010 ) studied LaPaz Ice Field clastic impact melts of meteorites, of which the metal-sulfide texture indicated impact temperatures between 950 and 1,500 °C and proposing the age of impact event years on the H

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