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The Los Angeles Basin is a sedimentary basin located in Southern California, in a region known as the Peninsular Ranges. The basin is also connected to an anomalous group of east-west trending chains of mountains collectively known as the Transverse Ranges. The present basin is a coastal lowland area, whose floor is marked by elongate low ...
The city of Los Angeles handles all building permits and air permitting issues for the oil field. Geology Beverly Hills Oil Field Structure Map. The field is a faulted anticlinal structure with oil trapped by a combination of structural and stratigraphic mechanisms. Bounding the field on the south is the Brentwood-Las Cienegas Fault, and the ...
The Wilmington Oil Field is a prolific petroleum field in Los Angeles County in southern California in the United States. Discovered in 1932, it is the third largest oil field in the United States in terms of cumulative oil production. [1] The field runs roughly southeast to northwest through the Los Angeles Basin, stretching from the middle of ...
Geology. Los Angeles City Oil Field Geologic map and cross section. Oil in the Los Angeles City field is relatively close to the surface. Every productive deposit has been in a single geologic unit, the shallow Miocene -age Puente Formation.
Puente Hills Fault. Map showing the location of the Puente Hills Fault. The Puente Hills Fault (also known as the Puente Hills Thrust Fault System) is an active geological fault that is located in the Los Angeles Basin in California. The thrust fault was discovered in 1999 and runs about 40 km (25 mi) in three discrete sections from the Puente ...
Vasquez Formation. / 34.48000°N 118.31667°W / 34.48000; -118.31667. The Vasquez Formation ( Tvz) is a geologic formation cropping out at the eponymous Vasquez Rocks in southern California. The formation dates to the Late Oligocene to Early Miocene ( Arikareean in the NALMA classification ).
English: This map indicates the location of the Los Angeles Basin in relation to the Transverse and Peninsular Ranges.
Geology. Salt Lake Oil Field Structure Map. The field is near the northern edge of the Los Angeles Basin, about two miles (3 km) south of the Hollywood Hills, the nearest portion of the Santa Monica Mountains. The Santa Monica Fault, not known to be active, demarcates the boundary between the basin and the mountains.
The Hollywood fault is an active fault of approximately 9 miles (14 km) in length located along the northern edge of the Los Angeles basin. [1] It is part of a system of seismically active folds and faults that constitute the complex transition zone between the Transverse and Peninsular Ranges.
Geology Map showing relation of the Dos Cuadras Field to the Rincon anticlinal trend. The Dos Cuadras field is a faulted anticlinal structure which plunges at both ends, thereby forming an ideal trap for hydrocarbon accumulation.