LITHOLOGIC RESERVOIRS ›› 2015, Vol. 27 ›› Issue (5): 6-12.doi: 10.3969/j.issn.1673-8926.2015.05.002

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Carbonate facies and sedimentary evolution of Upper Devonian Tuqiaozi Formation in Ganxi section of Longmen Mountain

Li Fengjie， Qu Xuelin， Du Lingchun， Jing Xigui， Cheng Xiaoyu   

  1.  Institute of Sedimentary Geology ， Chengdu University of Technology ， Chengdu 610059 ， China
  • Online:2015-09-26 Published:2015-09-26

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Abstract:

Based on the data of cross sections, the Upper Devonian Tuqiaozi Formation in Ganxi section of the Longmen Mountain is considered to be carbonate ramp deposits. With the sea level of a brief fall in the middle sedimentary stage of Tuqiaozi Formation, the carbonate ramp transformed to carbonate platform, of which the most direct identification mark is the emergence of breccia and slump deposit in the front of reef. There are two types of subfacies including shallow ramp and deep water ramp in carbonate ramp and two types of subfacies including platform edge reef and beach and foreslope in carbonate platform. Two whole carbonate sedimentary cycles developed in Tuqiaozi Formation. There are different sedimentary features between the two sedimentary cycles with the changes of sea level rise and fall. The carbonate ramp of Tuqiaozi Formation in Ganxi section is characterized by rhythmite formed by micrite-marl.

Key words: conglomerate reservoirs, alluvial fan reservoir, reservoir architecture, seismic attributes, Karamay Oilfield

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