Organic Carbon versus Major Elements Relationship in Rocks of the Bazhenov Formation, Western Siberia View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2001-05

AUTHORS

V. G. Eder, V. O. Krasavchikov, Yu. N. Zanin, A. G. Zamirailova

ABSTRACT

A close relation of the organic carbon (Corg) content with major has been established for rocks of the Upper Jurassic–Lower Cretaceous Bazhenov Formation. Applying the method of multiple linear regression, it has been demonstrated that the Corgcontent in rocks of the Bazhenov Formation is stringently controlled by its bulk chemical composition. This inference is consistent with the existing ideas regarding a close interrelation between the following main components of rocks: organic carbon and authigenic quartz formed on remains of Radiolaria; pyrite formed in a highly reducing medium of Corg-rich sediments; and terrigenous clayey material diluting the authigenic siliceous–carbonaceous–pyritic matrix. These components chiefly determine the spectrum of major elements in the Bazhenov Formation. The establishment of the close relation between the Corgcontent and the group of major elements refutes the suggestion of some authors that siliceous material was supplied to nonlithified sediments of the Bazhenov sea by hydrothermal solutions, because this mechanism would have inevitably upset geochemical relations between elements in the studied rocks. More... »

PAGES

236-242

Identifiers

URI

http://scigraph.springernature.com/pub.10.1023/a:1010477308529

DOI

http://dx.doi.org/10.1023/a:1010477308529

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1044721532


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