Seismic constraints on fault angles in Railroad Valley, NV
Conference
·
· Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5021109
- Geological Survey, Denver, CO (United States)
The USGS has obtained 7 seismic reflection lines in eastern Railroad Valley to delineate fault geometries near the Grant Canyon (GC), Kate Springs (KS), and Eagle Springs (ES) oil fields. A NW-trending 120-channel profile over KS reveals a 2-km-wide bench of Paleozoic carbonates (PzC) at about 1.4 sec depth ([approximately]1.4 km of Miocene valley fill) offset by a large, NW-dipping, high-angle normal fault (> 40[degree]) on the east and by two smaller, high-angle normal faults on the west. This profile is consistent with previously published profiles over ES (2 km N of KS), which have been interpreted as indicating a large high-angle fault E of ES. Interpretations of this eastern high-angle fault are based on shallow reflections and diffractions ([approximately]0.1--0.2 sec) and the absence of fault-plane reflections (too steep for reflection returns). An alternative interpretation attributes the shallow reflections to highly cemented conglomerates or megabreccias in the valley fill rather than the top of a Paleozoic block. Recently proposed exploration holes E of KS and ES may resolve this ambiguity. Two NW-trending 120-channel profiles 2--4 km N of GC (11 km S of KS) reveal a quasiplanar reflecting at surface between 1 and 2 sec (1--2 km) depth dipping [approximately]20[degree]NW. The surface is also seen dipping [approximately]10[degree]N on N-trending lines (with minor undulations of [approximately]0.1 sec). A WNW-trending 1,024-channel seismic profile directly over the GC field delineates this low-angle surface E of the field and shows that the PzC reservoirs at GC are 0.2 sec above the westward projection of the reflecting surface. The authors interpret the low-angle surface to be a normal fault that partially decapitates the pluton and underlies the GC field, as proposed by Karen Lund and others.
- OSTI ID:
- 5021109
- Report Number(s):
- CONF-9305259--
- Conference Information:
- Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 25:5
- Country of Publication:
- United States
- Language:
- English
Similar Records
Regional seismic reflection profile from Railroad Valley to Lake Valley, east-central Nevada, reveals a variety of structural styles beneath Neogene basins
Marine crustal reflection profiling offshore Santa Maria Basin westward to base of continental slope
Reinterpretation of Mormon Peak detachment in Mormon Mountains, southern Nevada
Conference
·
Sat Jun 01 00:00:00 EDT 1991
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
·
OSTI ID:5875393
Marine crustal reflection profiling offshore Santa Maria Basin westward to base of continental slope
Conference
·
Mon Feb 29 23:00:00 EST 1988
· AAPG Bull.; (United States)
·
OSTI ID:6633961
Reinterpretation of Mormon Peak detachment in Mormon Mountains, southern Nevada
Conference
·
Sun Jan 31 23:00:00 EST 1988
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:5954268
Related Subjects
02 PETROLEUM
020200 -- Petroleum-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000* -- Geosciences
DEVELOPED COUNTRIES
GEOLOGIC DEPOSITS
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GEOMETRY
GEOPHYSICAL SURVEYS
MATHEMATICS
MINERAL RESOURCES
NEVADA
NORTH AMERICA
ORIENTATION
PETROLEUM DEPOSITS
RESERVOIR ROCK
RESOURCES
SEISMIC SURVEYS
SURVEYS
USA
020200 -- Petroleum-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000* -- Geosciences
DEVELOPED COUNTRIES
GEOLOGIC DEPOSITS
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GEOMETRY
GEOPHYSICAL SURVEYS
MATHEMATICS
MINERAL RESOURCES
NEVADA
NORTH AMERICA
ORIENTATION
PETROLEUM DEPOSITS
RESERVOIR ROCK
RESOURCES
SEISMIC SURVEYS
SURVEYS
USA