Mineralogy, crystallinity and stable isotopic composition of illitic clays within the Polish Zechstein basin: implications for the genesis of Kupferschiefer mineralization-Reference-Cited by-同舟云学术

Mineralogy, crystallinity and stable isotopic composition of illitic clays within the Polish Zechstein basin: implications for the genesis of Kupferschiefer mineralization

Published:2000-02 Issue:1-4 Volume:163 Page:189-205
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Bechtel A.,Shieh Y.-N.,Elliott W.C.,Oszczepalski S.,Hoernes S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference57 articles.

1. Stable isotopic variations of clay minerals: a key to the understanding of Kupferschiefer-type mineralization, Germany;Bechtel;Geochim. Cosmochim. Acta,1993

2. The origin of the Kupferschiefer-type mineralization in the Richelsdorf hills, Germany, as deduced from stable isotope and organic geochemical studies;Bechtel;Chem. Geol.,1991

3. Reconstruction of the thermal history of the Kupferschiefer within the Zechstein basin of Central Europe: a stable isotope and organic geochemical approach;Bechtel;Ore Geol. Rev,1995

4. Indirect age determination of Kupfrschiefer-type mineralization in the Polish Zechstein basin by K/Ar dating of illite: preliminary results;Bechtel;Econ. Geol.,1996

5. Conversion of hydrogenic materials to hydrogen for isotopic analysis;Bigeleisen;Anal. Chem.,1952

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