Diaplectic transformation of minerals: Vorotilov drill core, Puchezh-Katunki impact crater, Russia

Details Diaplectic transformation of minerals: Vorotilov drill core, Puchezh-Katunki impact crater, Russia Diaplectic transformation of minerals: Vorotilov drill core, Puchezh-Katunki impact crater, Russia

Sep 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992lmip.conf...25f&link_type=abstract

In Lunar and Planetary Inst., International Conference on Large Meteorite Impacts and Planetary Evolution p 25 (SEE N93-10112 01

Astronomy and Astrophysics

Astronomy

Breccia, Core Sampling, Impact Damage, Metamorphic Rocks, Meteorite Collisions, Meteorite Craters, Meteoritic Damage, Minerals, Gneiss, Olivine, Peridotite, Precambrian Period, U.S.S.R.

Scientific paper

The Vorotilov core was drilled in the central uplift of the Puchezh-Katunki astrobleme to a depth of 5.1 km. Impactites are revealed in the rocks of the core beginning from a depth of 366 m: suevites (66 m), allogenic breccias (112 m), and autogenic breccias (deeper than 544 m). These rocks are represented by shocked-metamorphic gneisses, schists, amphibolites of Archean age, and magmatic rocks (dolerites, olivines, and peridotites) that lie between them.

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