Westfälische Wilhelms-Universität
Münster
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Institut für Planetologie Wilhelm-Klemmstrasse 10 48149 Münster Geschäftsführender Direktor: Prof. Dr. Tilman Spohn |
Tel. (0251) 83-33496
Fax: (0251) 83-36301 e-mail: ifp@uni-muenster.de www: http://ifp.uni-muenster.de/ |
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Forschungsschwerpunkte 2001 - 2002 Fachbereich 14 - Geowissenschaften
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Geochemische Untersuchungen an Impaktlithologien des Popigai-Kraters, Russlnd
It has
been demonstrated convincingly that geochemical and isotopic characteristics of impact melt
lithologies (melt
rocks, melt particles in melt breccias and suevites) can be used to constrain their precursor
materials, and to
relate ejected impact melt glass in proximal and distant ejecta to the respective source crater.
An unambiguous
correlation of ejected impact melt products (tektites, micro-tektites, impact melt glass,
micro-crystites) with the
parent crater, however, was only possible in a few cases despite the high sensitivity of isotopic
techniques. This
may be due to the fact that only parts of the terrestrial crater population are known but also due
to the lack of
systematic isotope studies on impact craters: Melt products of one cratering event may display
more
heterogeneous isotope characteristics than hitherto assumed. The 35.7 ±
0.2 Ma old
Popigai crater, Siberia, with a diameter of about 100 km is one of the best preserved
terrestrial impact
structures. The heterogeneous target at the Popigai impact site comprises Archean to
Proterozoic metamorphic
rocks of the crystalline basement, Proterozoic red beds, and Cambrian to Cretaceous clastic
sediments and
sedimentary rocks, amongst them carbonate rocks. Moreover, Proterozoic and Permo-Triassic
dolerite dykes
are found in the target. Based on major element, Sr, and Nd isotope data for these target rocks
as well as for
various types of impactites, we show that the melt layer reflects the precursor lithologies in th
erespective
crater sectors. Moreover, we provide the first solid evidence for the clear relation of
microtektites and
microkrystites in the Upper Eocene ejecta layer to the Popigai event.
Drittmittelgeber: Beteiligte Wissenschaftler: Veröffentlichungen: |
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