Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (2): 518-532.doi: 10.13278/j.cnki.jjuese.201502115

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Characteristics of the Sequence Stratigraphy and Sequence Stratigraphy Framework, the Middle to Upper Cambrian in Western Xuefeng Mountains Area

Zhao Can1, Li Xubing1, Huan Jinlai2, Chen Xiaohong1, Liu An1, Wei Kai1, Zhang Hua3   

  1. 1. Wuhan Institute of Geology and Mineral Resources, Wuhan 430223, China;
    2. Zhanjiang branch, CNOOC (China) Co., Ltd., Zhanjiang 524057, Guangdong, China;
    3. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
  • Received:2013-05-06 Published:2015-03-26

Abstract:

We present the sequence stratigraphy characteristics of the Middle-Upper Cambrian in the area of western Xuefeng Mountain through comprehensive analyses of sedimentology, rock mineralogy, carbon isotope geochemistry. Based on the results, the Middle-Upper Cambrian can be divided into one second-order sequence, and five third-order sequences. Within the time range of second-order sequence, the shallow waterfacies experienced sedimentary evolution from a confined platform tidal flat, to an open platform, then to aconfined platform tidal flat again; while the slope transition zone experienced sedimentary evolution from a marginal platform, to a frontier slow slope,and then to a marginal platform again. The deep water facies in the south-east of the research area is formed from deep shelf, basin, toshallow shelf. The grain dolomite, stromatolite reefs deposited during the third-order sequence of sea rise transgression and the dissolved porosity and karst breccia dolomite formed during the high sea level bear the significant potential for oil and gas exploration, and are worthy of further study.

Key words: meter-scale cyclic sequence, sequence stratigraphy characteristis, sequence stratigraphy framework, Middle to Upper Cambrian, western Xuefeng Mountains area

CLC Number: 

  • P618.13

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