Lithologic Reservoirs ›› 2016, Vol. 28 ›› Issue (5): 99-106.doi: 10.3969/j.issn.1673-8926.2016.05.012

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Restoration of formation compaction and inversion of deposition rate in Dianqianbei exploration area

Zhang Tingshan1,2, Zhang Zhicheng1,2, Wu Kunyu 1,2   

  1. (1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China; 2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China; 3. Research Institute of Exploration and Development, PetroChina Qinghai Oilfield Company, Dunhuang 736202, Gansu, China)
  • Online:2016-09-29 Published:2016-09-29

Abstract:

The Dianqianbei exploration area is a potential shale gas development zone, located in the southern margin of the Sichuan Basin. In order to identify the restoration of formation compaction and inversion of deposition rate, this paper established the Upper Ordovician to Quaternary model of layered acoustic and porosity with depth by using optimization models combined with the traditional methods, then carried out layered back ripping based on the principle of rock skeleton unchanged, acquired the original formation sedimentary thickness and segmented deposition rate, and discussed the relationship between the deposition rate and the abundance of organic matter of shale formation. The results show that the deposition rate is lower and tow?wave like in Dianqianbei area. It increased rapidly to its peak and dropped in early period, then climbed up slowly and downed to valley in later period. The deposition rates of Silurian Longmaxi Formation and Loureping Formation are 77.97 m/Ma and 113.47 m/Ma respectively. The shelf environment with slow deposition rate is beneficial to enhance the organic matter abundance of shale. The results are references for researching stratigraphic burial evolution and shale gas exploration and development.

Key words: carbonate platform, sedimentary facies, sedimentary evolution, Ordovician, Dongpu area, Bohai Bay Basin

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