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Title: Geologic and structural characters of Liaohe fault depression--Rich in oil and gas rift valley in northeastern China

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:6106874
 [1]
  1. China Univ. of Geosciences, Wuhan (China)

Liaohe fault depression is famous for its first class in per square kilometer oil reserves and yield, and the third level in output in China. It lies in the north part of Bo Sea and Liaoning province with about 12,400 km[sup 2] in onshore area. The basement consisted of metamorphic rocks, covered by upper Jurassic-lower Cretaceous red clastic formation intercalated by a coal system stratum (1,600 m), Eogene dark mudstone and sand-conglomeratic rock formation with 1,200m source bed (about 7,000m), and Neogene-Quaternary motley sand-mudstone formation (more than 1,000m). Fourteen sets of oil-bearing strata exist in the basement and overburdens. Liaohe depression is characterized by a horst and graben system. The features are as follows: (1) bulge and sag alternate within depression; (2) the shape of depression and the undulation of basement are the mirror image of Moho; (3) the magnificent Tanlu strike-slip fault system runs through the middle Liaohe area, the faults are almost normal faults with some strike-slip natures; (4) alkaline volcanics erupted many times from later Mesozoic to Cenozoic; (5) high heat flux, the average value is 2.24 HFU, the geothermal gradient is 4 C/100m in Eogene; (6) seismic activity was frequent, according to statistics, before the Haicheng earthquake which was of 7.3 magnitude in 1975, there were 257 shocks lower than 4.7 magnitude; (7) the extensional rate of rift valley is about 20%; (8) trap is related to compacting anticline, rollover anticline, pinching sandstone, onlap strata, confined fault block, stratigraphic unconformity, diapiric mudstone dome and buried hills.

OSTI ID:
6106874
Report Number(s):
CONF-921058-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 24:7; Conference: 1992 annual meeting of the Geological Society of America (GSA), Cincinnati, OH (United States), 26-29 Oct 1992; ISSN 0016-7592
Country of Publication:
United States
Language:
English