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Data for "Serpentinite-rich Gouge in a Creeping Segment of the Bartlett Springs Fault, Northern California: Comparison with SAFOD and Implications for Seismic Hazard"

Dates

Publication Date
Start Date
2011
End Date
2018

Citation

Moore, D.E., McLaughlin, R.J., and Lienkaemper, J.J., 2021, Data for "Serpentinite-rich Gouge in a Creeping Segment of the Bartlett Springs Fault, Northern California: Comparison with SAFOD and Implications for Seismic Hazard": U.S. Geological Survey data release, https://doi.org/10.5066/P9OUFFKS.

Summary

This report presents the mineral chemistry dataset that was used in a published study of serpentinite-rich gouge from an actively creeping trace of the Bartlett Springs Fault in northern California. The fault gouge consists of porphyroclasts of antigorite serpentinite, talc, chlorite, and tremolite-actinolite in a sheared matrix of the same materials. The compositions of spinels in the serpentinite clasts (Table S1) indicate a forearc-peridotite origin for the serpentinite, consistent with a source in the Coast Range ophiolite. The other major minerals in both the porphyroclasts and matrix were analyzed (Table S2) for comparison with serpentinite-bearing gouge from the creeping section of the San Andreas Fault. Table S3 presents serpentine [...]

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Table S1 BSF spinels v2.csv
“Table S1”
3.51 KB text/csv
Table S2 BSF mineral compositions v2.csv
“Table S2”
5.5 KB text/csv
Table S3 CRO serpentines v2.csv
“Table S3”
3.4 KB text/csv

Purpose

Compositions of the minerals that comprise serpentinite-rich fault gouge within the Bartlett Springs Fault near Lake Pillsbury, California were obtained to determine the depth at which the gouge formed. Serpentine-mineral compositions from outcrops of Coast Range ophiolite in the same area were obtained for comparison to compositions of serpentine in the fault gouge.

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DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9OUFFKS

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