Impact Origin of the Chesapeake Bay Structure and the Source of the North American Tektites

Author:

Koeberl Christian1,Poag C. Wylie2,Reimold Wolf Uwe3,Brandt Dion3

Affiliation:

1. C. Koeberl, Institute of Geochemistry, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria.

2. C. W. Poag, U.S. Geological Survey, Woods Hole, MA 02543, USA.

3. W. U. Reimold and D. Brandt, Department of Geology, University of the Witwatersrand, Johannesburg 2050, South Africa.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference48 articles.

1. MICROSCOPIC LAMELLAR DEFORMATION FEATURES IN QUARTZ - DISCRIMINATIVE CHARACTERISTICS OF SHOCK-GENERATED VARIETIES;ALEXOPOULOS S. J.;GEOLOGY,1988

2. BOHOR F. B., LUNAR PLANET SCI 19, 114 (1988).

3. CHAO ECT, TEKTITES: 51 (1963).

4. BORON CONTENT AND ISOTOPIC COMPOSITION OF TEKTITES AND IMPACT GLASSES - CONSTRAINTS ON SOURCE REGIONS;CHAUSSIDON M;GEOCHIMICA ET COSMOCHIMICA ACTA,1995

5. COSTAIN K. J., EOS 61, 1 (1980).

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