A study of sequence stratigraphy of the Early Cretaceous coal-bearing series in the southeastern Songliao Basin, NE China

被引:4
作者
Shao, Kai [1 ,2 ,3 ,4 ]
Shao, Longyi [2 ,3 ]
Ma, Dongmin [1 ]
Wang, Dongdong [2 ,3 ,5 ]
Wang, Shuai [2 ,3 ]
Gao, Di [2 ,3 ,6 ]
机构
[1] Xian Univ Sci & Technol, Coll Resources & Environm, Xian 710054, Shaanxi, Peoples R China
[2] China Univ Min & Technol Beijing, State Key Lab Coal Resources & Safe Min, Beijing 10008, Peoples R China
[3] China Univ Min & Technol Beijing, Coll Geosci & Surveying Engn, Beijing 10008, Peoples R China
[4] Shannxi Coalbed Methane Dev Co Ltd, Xian 710119, Shaanxi, Peoples R China
[5] Shandong Univ Sci & Technol, Coll Geol Sci & Engn, Qingdao 266590, Shandong, Peoples R China
[6] Henan Polytech Univ, Coll Resources & Environm, Jiaozuo 454000, Henan, Peoples R China
基金
中国国家自然科学基金;
关键词
Songliao Basin; Sequence stratigraphy; Depositional system; Coal accumulation; ERLIAN BASIN; ARCHITECTURE; PALEOGEOGRAPHY; FILLS; UNITS;
D O I
10.1007/s40789-020-00339-8
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The Early Cretaceous is an important coal accumulation period in China. Abundant coal resources were formed in the southeastern margin of Songliao Basin. Sequence stratigraphy and coal accumulation of the Early Cretaceous in the southeastern margin of Songliao Basin have been studied on the basis of extensive outcrop and borehole data. Based on regional unconformity, basal erosional surfaces of incised valley fills, and abrupt depositional facies-reversal surface, six sequence boundaries have been identified, which subdivide the Early Cretaceous coal-bearing series into 5 third-order sequences. Sequence I corresponds to Huoshiling Formation, sequences II and III correspond to member I and member II of Shahezi Formation. Sequences IV and V correspond to member I and member II of Yingcheng Formation. Sequence I developed at the initial subsiding stage, sequence II and III developed during the stable subsiding stage, while sequence IV and V developed during the basin shrinkage stage. The major coal seams were developed in the sequence II and III, which ensured the relative balance between the increase rate of the accommodation space and the rate of peat accumulation for a longer period, thus forming a thick coal seam.
引用
收藏
页码:263 / 272
页数:10
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