Authors:
Ildikó Gyollai Institute of Physics, Dept. Material Physics, Eötvös University, Faculty of Science, Budapest, Hungary
H-1117, Budapest, Pázmány P. s. 1/a, Hungary

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Arnold Gucsik Dept. of Geochemistry, Max Planck Institute for Chemistry, Mainz, Germany
Joh.-J. Becherweg 27, D-55128, Mainz, Germany

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Szabolcs Nagy Institute of Physics, Dept. Material Physics, Eötvös University, Faculty of Science, Budapest, Hungary
H-1117, Budapest, Pázmány P. s. 1/a, Hungary

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Szaniszló Bérczi Institute of Physics, Dept. Material Physics, Eötvös University, Faculty of Science, Budapest, Hungary
H-1117, Budapest, Pázmány P. s. 1/a, Hungary

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Abstract

We investigated three types of shocked feldspar in the Asuka-881757,531-2 sample with midinfrared spectroscopy (reflectance mode). Under the petrographic microscope three types of site were characterized by (1) undulatory extinction, (2) undulatory extinction with isotropic patches and decreased interference color, and (3) isotropic, lath-shaped feldspars, which is indicative of maskelynite. The IR emissivity maximum (Christiansen feature=CF) changes with the chemical composition of feldspar. One of the Christiansen composition features exhibits a wave length peak of 1234 cm−1 for anorthite; another feature appears at 1245 cm−1 for maskelynite (Palomba et al. 2006).

With the help of IR spectroscopy we observed three vibrational types in our spectra: (1) peaks of depolimerization of SiO4 tetrahedra (500–650 cm−1, 950–1150 cm−1), (2) peaks of stretching and bending vibrational modes of SiO6 octahedra (750–850 cm−1), and (3) Si-O stretching vibration of SiO4 units (Johnson and Hörz 2003; Johnson et al. 2003, 2007). All these vibration types were observed at the less shocked sites. In the spectrum of highly shocked maskelynite only a broader band close to 1000 cm−1 was observed, which is the main vibrational band of maskelynite (Palomba et al. 2006). The calculated FWHM showed the disordering rate of shocked feldspars. On the basis of the measurements it could be concluded that the estimated shock pressure range gradually increases from 17–35 GPa for different degrees of undulatory sites, to 35–45 GPa for maskelynite sites.

  • Fernandes, V.A., A. Morris, R. Burgess 2005: New Ar-Ar Age determinations for the lunar mare basalts Asuka 881757 and Yamato 793169 (abstract). — In Lunar and Planetary Science 36, abstract no. 1002, 36th Lunar and Planetary Science Conference, Houston.

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  • C. Koeberl G. Kurat F. Brandstätter 1993 Gabbroic lunar mare meteorites Asuka-881757 (Asuka-31) and Yamato 793169: Geochemical and mineralogical study, Proc. NIPR Symp. Antarct. Meteorites Nat. Inst. Polar Res. Tokyo 14 34.

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  • J.R. Johnson M.I. Staid M.D. Kraft 2007 Thermal infrared spectroscopy and modeling of experimentally shocked basalts American Mineralogist 92/ 7 1148 1157.

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  • J.R. Johnson F. Hörz M.I. Staid 2003 Thermal infrared spectroscopy and modeling of experimentally shocked plagioclase feldspars American Mineralogist 88 1575 1582.

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  • J.R. Johnson F. Hörz 2003 Visible/near-infrared spectra of experimentally shocked plagioclase feldspars Journal of Geophysical Research 108 5120.

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  • Johnson, J.R. 2007: Thermal Infrared Emissivity Spectra of Experimentally Shocked Andesine. — Seventh International Conference on Mars 3258.pdf.

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  • E. Palomba A. Rotundi L. Colangeli 2006 Infrared micro-spectroscopy of the Martian meteorite Zagami: Extraction of individual mineral phase spectra — Icarus 182 68 79.

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  • D. Stöffler 1972 Deformation and transformation of rock-forming mineral by natural and experimental shock processes: I. Behavior of minerals under shock compression Forschr. Miner. 49 50 113.

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  • D. Stöffler 1974 Deformation and transformation of rock-forming minerals by natural and experimental shock processes: II. Physical properties of shocked minerals Fortschr. Miner. 51 256 289.

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  • D. Stöffler K. Keil S. Edward 1991 Shock metamorphism of ordinary chondrites Geochimica et Cosmochimica Acta 55/ 12 3845 3867.

  • K. Yanai H. Kojima 1991 Varieties of lunar meteorites recovered from Antarctica Proc. NIPR Symp. Antarct. Meteorites 4 70 90.

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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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2023  
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Central European Geology
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Central European Geology
Language English
Size Vol 1-63: B5
Vol 64- : A4
Year of
Foundation
2007 (1952)
Volumes
per Year
1
Issues
per Year
2
Founder Magyar Tudományos Akadémia  
Founder's
Address
H-1051 Budapest, Hungary, Széchenyi István tér 9.
Publisher Akadémiai Kiadó
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ISSN 1788-2281 (Print)
ISSN 1789-3348 (Online)

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