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U.S. Department of Energy
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Faulting and jointing in and near surface mines of southwestern Indiana

Technical Report ·
OSTI ID:6092515
Three major areas of faulting have been delimited by past studies in southern Indiana: the Mt. Carmel Fault in south-central Indiana, the Wabash Valley Fault System in Posey and Gibson counties, and faulting in Perry and Spencer counties. This project completed the mapping and characterization of the remaining known large faults in southern Indiana, including the Georgetown Fault in Floyd County and the newly named Crandall Fault in Harrison County. The Georgetown and Crandall Faults are normal faults that have a maximum vertical displacement of about 65 feet. They are post-Valmeyeran and pre-Pleistocene in age and are probably the result of hinge-line deformation between the subsiding Illinois Basin and the Cincinnati Arch. In contrast, abundant small-scale faults and joints are related to regional compressive lithospheric stress or to sedimentologic processes that operated penecontemporaneously with deposition of the rocks in which they are found. Structures related to regional stress include small-scale thrust faults with displacements of a few inches to a few feet and joints that are widespread in mines and outcrops in rocks of Mississippian and Pennsylvanian age. The jointing and most of the small-scale thrust faulting indicate that southern Indiana is affected by the Midcontinent Stress Province in the northern part of the study area and by another stress field in the southern part. An east-west boundary can be defined between the two stress fields. 22 references, 18 figures.
Research Organization:
Indiana Geological Survey, Bloomington (USA)
OSTI ID:
6092515
Report Number(s):
NUREG/CR-4117; ON: TI85900565
Country of Publication:
United States
Language:
English

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