Quantifying the heterogeneity of the tectonic stress field using borehole data
Author:
Affiliation:
1. Earth and Environmental Science; Temple University; Philadelphia Pennsylvania USA
2. GMEG Science Center; U.S. Geological Survey; Menlo Park California USA
3. Now at Department of Geophysics; Stanford University; Stanford California USA
Funder
Temple University
U.S. Geological Survey's (USGS) Energy Program's Geothermal Resource Investigation Project
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JB014370/fullpdf
Reference86 articles.
1. Inversion technique to determine the in-situ stress field from fracturing data;Aadnoy;J. Pet. Sci. Eng.,1990a
2. In-situ stress directions from borehole fracture traces;Aadnoy;J. Pet. Sci. Eng.,1990b
3. Geophys. Monogr. Ser.;Ampuero,2006
4. A stochastic fault model: 1. Static case;Andrews;J. Geophys. Res.,1980
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