The nature of O18/O16 and C13/C12 secular trends in sedimentary carbonate rocks-Reference-Cited by-同舟云学术

The nature of O18/O16 and C13/C12 secular trends in sedimentary carbonate rocks

Published:1976-11 Issue:11 Volume:40 Page:1387-1395
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Veizer Ján,Hoefs Jochen

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference69 articles.

1. Messung und Deutung relativer Haufigskeitvariationen von O18 von C13 in Karbonatgesteinen und Mineralien;Baertschi;Schweiz. Mineral. Petrog. Mitt.,1957

2. Die Isotopenzusammensetzung von Dolomiten und Kalken aus dem süddeutschen Malm;Bausch;Contrib. Mineral. Petrol.,1972

3. Carbon isotopic evidence for the origin of a banded iron formation in Western Australia;Becker;Geochim. Cosmochim. Acta,1972

4. Dolomitization of the mid-Pacific atolls;Berner;Science,1965

5. Relationship between Ca/Mg ratio and geologic age;Chilingar;Amer. Assoc. Petrol. Geol. Bull.,1956

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