Interpretation of gravity data in the Timber Mountain area of the Nevada Test Site
Technical Report
·
OSTI ID:5858879
The Timber Mountain area occurs within a volcanic province where Cenozoic volcanic rocks of unknown thickness are deposited. Analysis of gravity data indicates about 12,000 feet of these rocks are beneath Timber Mountain and in the moat. Gravity lows of small amplitude define the moat area, whereas gravity highs define the mountain, which is composed of extrusive rhyolitic and intrusive silicic complexes. Bouguer anomaly maps (densities of 2.67 and 2.20 g/cm/sup 3/) and residual maps (first-order and second-order surfaces) are presented. By correlating all four maps a better understanding of the subsurface structure is obtained. Three geologic cross sections are presented that define, in general, this structure. 9 figures, 3 tables.
- Research Organization:
- Geological Survey, Denver, CO (USA)
- DOE Contract Number:
- EY-76-A-08-0474
- OSTI ID:
- 5858879
- Report Number(s):
- USGS-474-308
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
58 GEOSCIENCES
580100* -- Geology & Hydrology-- (-1989)
DATA
DATA FORMS
DENSITY
EXPERIMENTAL DATA
GEOLOGIC STRUCTURES
GEOLOGY
GEOPHYSICAL SURVEYS
GRAPHS
GRAVITY SURVEYS
IGNEOUS ROCKS
INFORMATION
LEVELS
NEVADA TEST SITE
NUMERICAL DATA
PHYSICAL PROPERTIES
ROCKS
STRATIGRAPHY
TOPOGRAPHY
UNDERGROUND
VOLCANIC ROCKS
WELLS
580100* -- Geology & Hydrology-- (-1989)
DATA
DATA FORMS
DENSITY
EXPERIMENTAL DATA
GEOLOGIC STRUCTURES
GEOLOGY
GEOPHYSICAL SURVEYS
GRAPHS
GRAVITY SURVEYS
IGNEOUS ROCKS
INFORMATION
LEVELS
NEVADA TEST SITE
NUMERICAL DATA
PHYSICAL PROPERTIES
ROCKS
STRATIGRAPHY
TOPOGRAPHY
UNDERGROUND
VOLCANIC ROCKS
WELLS