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Title: Geophysical log documentation of fluid migration from compacting shales: A mineralization model from the devonian strata of the Pine Point Area, Canada

Journal Article · · Econ. Geol.; (United States)

The compaction history of a shale sequence can be evaluated through the interpretation of sonic logs that measure porosity as a function of transit time. Downward dewatering of a shale sequence is indicated by the presence of an undercompacted zone which overlies a normally compacted shale zone and permeable strata. Evaluation of sonic logs for the Middle Devonian shale sequences of the Mackenzie Basin indicates that a substantial volume of water could have been generated by late-stage shale compaction. This derivation of metal-rich formation water is compatible with mineralization features of the reefal carbonate-hosted PbZn sulfide deposits of the Pine Point district. Furthermore, the pattern of shale compaction trends within the basin suggests that expelled fluids migrated within linear conduits, a feature that could have regional exploration significance.

Research Organization:
Department of Geological Sciences, The University of Texas at Austin, Austin, Texas
OSTI ID:
6710009
Journal Information:
Econ. Geol.; (United States), Vol. 78:7
Country of Publication:
United States
Language:
English

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