Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (3): 659-673.doi: 10.13278/j.cnki.jjuese.201703102

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Shallow-Water Delta Deposits in a Rifting Lacustrine Basin During Early Stage:A Case Study of the First Member of Dainan Formation at Yong'an Area, Gaoyou Sag

Zhu Zhaoqun1, Lin Chengyan1, Zhang Xianguo1, Li Zhipeng2, Xie Jingjing3, Wei Sudong4, Cheng Ping5   

  1. 1. School of Geosiences, China University of Petroleum, Qingdao 266580, Shandong, China;
    2. Research Institute of Exploration and Development, Shengli Oilfield, SINOPEC, Dongying 257061, Shandong, China;
    3. Shanghai Branch Company, CNOOC Ltd, Shanghai 200030, China;
    4. China Oilfield Service Limited, Langfang 065200, Hebei, China;
    5. No.1 Oil Production Factory, Jiangsu Oilfield Company,SINOPEC, Jiangdu 225265, Jiangsu, China
  • Received:2016-08-10 Online:2017-05-26 Published:2017-05-26
  • Supported by:
    Supported by National Science and Technology Major Project (2011ZX05009-003)

Abstract: Shallow-water delta, as a focus of sedimentology and hydrocarbon exploration, has gotten more attentions in depression lacustrine basin than in rift lacustrine basin. Based on the systematic study of regional geological background in combination with the analysis of cores, well logging, seismic, and test data, it is inferred that when the first member of Dainan Formation was deposited in early rifting stage, the geological conditions with gentle terrain, wide and shallow water, frequently fluctuant lake level, warm and humid climate, and adequate sediment supply were favorable for the formation of shallow-water delta. The shallow-water delta deposits are near to the sediment source and dominated by traction current. Plenty of sedimentary structures caused by strong hydrodynamics have been commonly found in cores. It developed sedimentary sequences of progradation and aggradation vertically and it is characterized by paralleling, sub-paralleling and imbricated seismic reflections. The shallow-water delta front is composed of the main type of sedimentary subfacies, which is widely distributed and can be divided into inner front and outer front. The major sand bodies come from the subaqueous distributary channels in delta front. Different types of sand bodies and sedimentary styles exist and evolve regularly towards the center of lake, which is deeply affected by the change of the ratio of accommodation to sediment supply (Abbr. A/S). Based on above, the sedimentary model of shallow-water delta in rifting lacustrine basin during the early stage was built up, which could contribute to enriching the understanding of shallow water delta in sedimentary perspective and broadening the hydrocarbon exploration domain to certain extent for the study area and even the whole slope belt of Gaoyou sag.

Key words: shallow-water delta, rifting lacustrine basin, depositional model, Gaoyou sag, the first member of Dainan Formation

CLC Number: 

  • TE122.2
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