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Imaging the southern trace of the Bl...
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University of Nevada, Las Vegas.
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Imaging the southern trace of the Black Hills fault, Clark County, Nevada.
紀錄類型:
書目-語言資料,印刷品 : Monograph/item
正題名/作者:
Imaging the southern trace of the Black Hills fault, Clark County, Nevada./
作者:
Zaragoza, Shelley A.
面頁冊數:
102 p.
附註:
Adviser: Catherine M. Snelson.
Contained By:
Masters Abstracts International47-01.
標題:
Geology. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1456381
ISBN:
9780549693185
Imaging the southern trace of the Black Hills fault, Clark County, Nevada.
Zaragoza, Shelley A.
Imaging the southern trace of the Black Hills fault, Clark County, Nevada.
- 102 p.
Adviser: Catherine M. Snelson.
Thesis (M.S.)--University of Nevada, Las Vegas, 2008.
The Black Hills fault (BHF) is a SE-dipping normal fault forming the northwestern structural boundary of the Eldorado basin, ∼20 km southeast of Las Vegas, Nevada (Langenheim and Schmidt, 1996). The fault offsets Holocene strata and is thus considered to be active (Fossett, 2005). Therefore, the BHF poses a significant seismic hazard to the greater Las Vegas area.
ISBN: 9780549693185Subjects--Topical Terms:
516570
Geology.
Imaging the southern trace of the Black Hills fault, Clark County, Nevada.
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Imaging the southern trace of the Black Hills fault, Clark County, Nevada.
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102 p.
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Adviser: Catherine M. Snelson.
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Source: Masters Abstracts International, Volume: 47-01, page: 0291.
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The Black Hills fault (BHF) is a SE-dipping normal fault forming the northwestern structural boundary of the Eldorado basin, ∼20 km southeast of Las Vegas, Nevada (Langenheim and Schmidt, 1996). The fault offsets Holocene strata and is thus considered to be active (Fossett, 2005). Therefore, the BHF poses a significant seismic hazard to the greater Las Vegas area.
520
$a
Fossett (2005) estimated that the BHF is capable of producing a M W 6.4 to 6.8 earthquake. However, this suggests a subsurface rupture length greater than the scarp length (Fossett, 2005). To test this hypothesis, remote sensing, geologic mapping, and high-resolution seismic reflection survey were utilized. The result is an interpretive geologic cross-section showing several SE-dipping normal faults on strike with the BHF. This implies that the BHF may be >6 km in length. In addition, several models are proposed to explain the anomalous orientation of the BHF relative to other normal faults in the area.
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