Carbon and oxygen isotopic survey of diagenetic carbonate deposits in the Agardhfjellet Formation (Upper Jurassic), Spitsbergen: preliminary results

ABSTRACT: Diagenetic carbonate deposits (concretions, cementation bodies and cement− stone bands) commonly occur in organic carbon−rich sequence of the Agardhfjellet Forma− tion (Upper Jurassic) in Spitsbergen. They are dominated by dolomite/ankerite and siderite. These deposits originated as a resu...

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Bibliographic Details
Main Authors: Krzysztof P. Krajewski, Instytut Nauk Geologicznych Pan
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.8109
http://www.polish.polar.pan.pl/ppr25/ppr25-027.pdf