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K Transfer during Burial Diagenesis in the Mahakam Delta Basin (Kalimantan, Indonesia)

Published online by Cambridge University Press:  28 February 2024

Sylvie Furlan ,
Norbert Clauer ,
Sam Chaudhuri  and
Frédéric Sommer
Sylvie Furlan
Affiliation:
Centre de Géochimie de la Surface, 1 rue Blessig, 67084 Strasbourg Cedex (France) Department of Geology, Kansas State University, Manhattan, Kansas 66506 (USA)
Norbert Clauer
Affiliation:
Centre de Géochimie de la Surface, 1 rue Blessig, 67084 Strasbourg Cedex (France)
Sam Chaudhuri
Affiliation:
Department of Geology, Kansas State University, Manhattan, Kansas 66506 (USA)
Frédéric Sommer
Affiliation:
Compagnie TOTAL-SA, CST de Beauplan, Route de Versailles, 78470 St Remy-lès-Cheveuse, France
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Abstract

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Progressively buried sandstones and shales of the Mahakam Delta Basin in Indonesia were studied. Mineralogical, morphological and K-Ar isotopic data were obtained for clay, mica and feldspar minerals. The data indicate that K necessary for the illitization of illite/smectite mixed-layer minerals was supplied mainly from K-feldspar alteration within the sandstones and from mica within the shales. Most of the K-feldspar alteration for both the shale and sandstone samples were observed outside the main zone of illitization, which is restricted to the upper 2000 m of sediment. The feldspar grains were altered below this depth for both lithologies. Therefore, illitization requires an open sedimentary system. This is in contrast to the illitization model for deeply buried shales of the Gulf Coast. That system is commonly assumed to be a closed K system.

Keywords

DiagenesisIllitizationK transfer
Type
Research Article
Information
Clays and Clay Minerals , Volume 44 , Issue 2 , April 1996 , pp. 157 - 169
Copyright
Copyright © 1996, The Clay Minerals Society

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