Authors:
Szabolcs Nagy Eötvös Loránd University, Budapest, Hungary
H-1117, Budapest, Pázmány Péter sétány 1/c., Hungary

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Sándor Józsa Eötvös Loránd University, Budapest, Hungary
H-1117, Budapest, Pázmány Péter sétány 1/c., Hungary

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Arnold Gucsik Max Planck Institute for Chemistry Department of Biogeochemistry, Mainz, Germany
Hahn-Meitner Weg 1, D-55128, Mainz, Germany

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Szaniszló Bérczi Eötvös Loránd University, Budapest, Hungary
H-1117, Budapest, Pázmány Péter sétány 1/c., Hungary

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Kiyotaka Ninagawa Department of Applied Physics, Okayama University of Science, Okayama, Japan

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Hirotsugu Nishido Research Institute of Natural Sciences, Okayama University of Science, Okayama, Japan
1-1 Ridai-cho, Okayama, 700-0005, Japan

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Miklós Veres Research Institute for Solid State Physics and Optics, Hungarian Academy of Sciences, Budapest, Hungary
H-1525, Budapest, PO Box 49, Hungary

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Ákos Kereszturi Konkoly Thege Miklós Astronomical Institute, Research Centre for Astronomy and Earth Sciences Hungarian Academy of Sciences, Budapest, Hungary
H-1121, Budapest, Konkoly-Thege Miklós u. 14, Hungary

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Henrik Hargitai Konkoly Thege Miklós Astronomical Institute, Research Centre for Astronomy and Earth Sciences Hungarian Academy of Sciences, Budapest, Hungary
H-1117, Budapest, Pázmány Péter sétány 1/c., Hungary

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Abstract

We studied optical microscopic and micro-Raman spectroscopic signatures of shocked olivine from the ALH 77005 Martian meteorite sample. The purpose of this study is to document pressure and temperature-related effects in olivine over the entire sample, which can aid in understanding structural changes due to shock metamorphism and the post-shock thermal annealing processes of lherzolitic Martian meteorites. According to the optical microscope observations, three areas may be discernible in olivine of the ALH 77005 in the vicinity of the melt pocket. The first area is the thermally undisturbed part of a grain, which contains a high density of shock-induced planar microdeformations such as Planar Deformation Features (PDFs) and Planar Fractures (PFs). Compared to the first area, the second area shows less shock-induced microstructures, while the third area is a strongly recrystallized region, but not formed from a melt.

A common Raman spectral feature of these olivines is a regular doublet peak centered at 823 and 852 cm−1; additionally, two new peaks at 535 and 755 cm−1 appear in the weakly annealed transition zones.

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Senior editors

Editor(s)-in-Chief: Attila DEMÉNY

Deputy Editor(s)-in-Chief: Béla RAUCSIK

Co-ordinating Editor(s): Gábor SCHMIEDL

Editorial Board

  • Zsolt BENKÓ (Geochemistry, Ar dating; Institute for Nuclear Research, Debrecen)
  • Szabolcs HARANGI (Petrology, geochemistry, volcanology; Eötvös Loránd University, Budapest)
  • Anette GÖTZ (Sedimentology; Landesamt für Bergbau, Energie und Geologie, Hannover)
  • János HAAS (Regional Geology and Sedimentology; Eötvös Loránd University, Budapest)
  • István Gábor HATVANI (Geomathematics; Institute for Geological and Geochemical Research, Budapest)
  • Henry M. LIEBERMAN (Language Editor; Salt Lake City)
  • János KOVÁCS (Quaternary geology; University of Pécs)
  • Szilvia KÖVÉR (Sedimentology; Eötvös Loránd University, Budapest)
  • Tivadar M. TÓTH (Mineralogy; Petrology    University of Szeged)
  • Stephen J. MOJZSIS (Petrology, geochemistry and planetology; University of Colorado Boulder)
  • Norbert NÉMETH (Structural geology; University of Miskolc)
  • Attila ŐSI (Paleontology; Eötvös Loránd University, Budapest)
  • József PÁLFY (Fossils and Stratigraphic Records; Eötvös Loránd University, Budapest)
  • György POGÁCSÁS (Petroleum Geology; Eötvös Loránd University, Budapest)
  • Krisztina SEBE (Tectonics, sedimentology, geomorphology University of Pécs)
  • Ioan SEGHEDY (Petrology and geochemistry; Institute of Geodynamics, Bucharest)
  • Lóránd SILYE (Paleontology; Babeș-Bolyai University, Cluj-Napoca)
  • Ákos TÖRÖK (Applied and Environmental Earth Sciences; Budapest University of Technology and Economics, Budapest)
  • Norbert ZAJZON (Petrology and geochemistry; University of Miskolc)
  • Ferenc MOLNÁR (ore geology, geochemistry, geochronology, archaeometry; Geological Survey of Finland, Espoo)

Advisory Board

Due to the changes in editorial functions, the Advisory Board has been terminated. The participation of former Advisory Board members is highly appreciated and gratefully thanked.

CENTRAL EUROPEAN GEOLOGY
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Hungarian Academy of Sciences
Address: Budaörsi út 45. H-1112 Budapest, Hungary
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E-mail: demeny@geochem.hu

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Central European Geology
Language English
Size Vol 1-63: B5
Vol 64- : A4
Year of
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2007 (1952)
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1
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2
Founder Magyar Tudományos Akadémia  
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