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Thermal history of the periphery of the Junggar Basin, Northwestern China

Organic Geochemistry
By: , and 

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Abstract

Geochemical analysis of rock core samples show that the basin periphery has experienced low thermal stress; present-day heat flows are in the range of 25-35 mW/m2 and have not been significantly higher than the worldwide mean of approx. 63 mW/m2 since the mid-Permian. Present day heat flows were determined from corrected borehole temperatures and rock thermal conductivities. Paleo-heat flows were determined by first-order reaction kinetic modeling of several geochemical paleothermometers (vitrinite reflectance, clay mineral diagenesis and relative proportions of sterane and hopane biological marker diastereomers). ?? 1994.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Thermal history of the periphery of the Junggar Basin, Northwestern China
Series title Organic Geochemistry
Volume 21
Issue 3-4
Year Published 1994
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Organic Geochemistry
First page 393
Last page 405
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