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- W21080287 abstract "The trap at Eagle Springs Field is a combination stratigraphic truncation-subcrop-fault trap. Production occurs from matrix and fracture porosity in reservoirs in the Sheep Pass Formation (Cretaceous and Eocene) and the Garrett Ranch volcanic group (Oligocene). Probably the most unique feature about the field is that the production occurs from the highest position on the lowermost fault block at the basin margin. On the adjacent higher fault blocks the reservoir beds were removed by erosion during the basin and range orogenic event. The position of the truncated edge of the lower Tertiary reservoir units is controlled by the fault pattern at the margin of the valley-basin Graben. Detailed geomorphic studies indicated that this fault pattern may be identified at the surface. Regional geomorphic mapping of fault patterns was conducted to localize areas with possible subcrop truncation patterns similar to Eagle Springs Field. 20 references." @default.
- W21080287 created "2016-06-24" @default.
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- W21080287 date "1979-01-01" @default.
- W21080287 modified "2023-09-24" @default.
- W21080287 title "Geological Techniques Utilized in Trap Spring Field Discovery, Railroad Valley, Nye County, Nevada" @default.
- W21080287 hasPublicationYear "1979" @default.
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