Sedimentary Environment and Coal Accumulation of the Carboniferous and Permian in the Southern North China Basin
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Sedimentary Environment and Coal Accumulation of the Carboniferous and Permian in the Southern North China Basin
Studia Marina SinicaVol. 17, Issue 50, (2010)
作者机构:
山东科技大学地质科学与工程学院
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DIAO Yujie, WEI Jiuchuan, CAO Hong. Sedimentary Environment and Coal Accumulation of the Carboniferous and Permian in the Southern North China Basin. [J]. Studia Marina Sinica 17(50).(2010)
DOI:
DIAO Yujie, WEI Jiuchuan, CAO Hong. Sedimentary Environment and Coal Accumulation of the Carboniferous and Permian in the Southern North China Basin. [J]. Studia Marina Sinica 17(50).(2010)DOI:
Sedimentary Environment and Coal Accumulation of the Carboniferous and Permian in the Southern North China Basin
摘要
Abstract
Four major sedimentary systems of the Carboniferous and Permian in the Southern North China (SNC) Basin were identified in sedimentological and depositional features,such as trace fossil,silt body shape,vertical sequence and logging curve. In addition,the sedimentary facied and typical sequences of sedimentary systems were analyzed in principles of sedimentology and coalfield geology,Furthermore,geological patterns of the coal accumulation,paleogeography and tectonic setting in each geological stage were reconstructed. Corresponding to sedimentary system and facies,there was no coal accumulation in the late carboniferous,while Shihezi Formation of the Middle Permian is the best coal accumulation period. And the delta front and sea-water swamp (the gulf) facies were the best environment for coal accumulation,which are meaningful for coalfield prediction and exploration in the Southern North China (SNC) Basin.