Development and Application of a Paleomagnetic/Geochemical Method for Constraining the Timing of Burial Diagenetic and Fluid

Elmore, Richard D. ; Engel, Michael H.

University of Oklahoma, Norman, OK

关键词: Mineralogy;    Sediments;    Reservoir Fluids;    Clays;    58 Geosciences;   

DOI  :  10.2172/837764
RP-ID  :  DOE/ER/14643-1
RP-ID  :  FG03-96ER14643
RP-ID  :  837764

美国|英语

来源: UNT Digital Library

【 摘 要 】

Studies of diagenesis caused by fluid migration or other events are commonly hindered by a lack of temporal control. Our results to date demonstrate that a paleomagnetic/geochemical approach can be used to date fluid migration as well as burial diagenetic events. Our principal working hypothesis is that burial diagenetic processes (e.g., maturation of organic-rich sediments and clay diagenesis) and the migration of fluids can trigger the authigenesis of magnetic mineral phases. The ages of these events can be constrained by comparing chemical remanent magnetizations (CRMs) to independently established Apparent Polar Wander Paths. While geochemical (e.g. stable isotope and organic analyses) and petrographic studies provide important clues for establishing these relationships, the ultimate test of this hypothesis requires the application of independent dating methods to verify the paleomagnetic ages. Towards this end, we have used K-Ar dating of illitization as an alternative method for constraining the ages of magnetic mineral phases in our field areas.