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Paleomagnetic studies of salt domes

Conference ·
OSTI ID:6504181
For the past several years, the authors have been pursuing a detailed paleomagnetic and petrographic study of the anhydrite cap rock of the Winnfield salt dome in Louisiana. This is the first such study ever undertaken and offers new insight into the timing of basinal and halokinetic processes. At Winnfield, periodic introduction of metalliferous fluids along the salt or anhydrite interface resulted in the formation of stratiform sulfide laminae, which contain the magnetic mineral pyrrhotite. Dense stratigraphic sampling of a 40-m section of the anhydrite yielded a magnetic reversal sequence that corresponds to sea-floor maganetic anomalies M22 to M20 (Kimmeridgian) and the authors were thus able to determine directly the age and rate of anhydrite accumulation. They recently sampled an additional 20 m of section at Winnfield and initiated a similar study of the Damon Mound, a salt dome in the Houston diapir province.
OSTI ID:
6504181
Report Number(s):
CONF-880301-
Country of Publication:
United States
Language:
English