Geologic context of geodetic data across a basin and range normal fault, Crescent Valley, Nevada
Geodetic strain and late Quaternary faulting in the Basin and Range province is distributed over a region much wider than historic seismicity, which is localized near the margins of the province. In the relatively aseismic interior, both the magnitude and direction of geodetic strain may be inconsis...
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Main Authors: | , , , |
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格式: | Article |
語言: | English |
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2012
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在線閱讀: | https://hdl.handle.net/10356/95646 http://hdl.handle.net/10220/8428 |
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