Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (3): 693-704.doi: 10.13278/j.cnki.jjuese.20170176

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Porosity Origin and Controlling Factors of Ultra-Deep, Low Porosity and Ultra-Low Permeability Sandstone Reservoirs: A Case Study of Bashijiqike Formation in Keshen Area of Kuqa Depression, Tarim Basin

Sun Haitao1, Zhong Dakang1, Li Yong2, Mao Yakun1, Yang Xianzhang1,2   

  1. 1. College of Geosciences, China University of Petroleum, Beijing 102249, China;
    2. PetroChina Tarim Oilfield Company, Korla 841000, Xinjiang, China
  • Received:2017-09-24 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41302108) and National Science and Technology Major Project (2016ZX05002-004-011)

Abstract: As a result of a complex diagenetic evolution, a reservoir with low porosity and ultra-low permeability exists in the ultra-deep sandstones of Bashijiqike Formation of Cretaceous in the Keshen area of Kuqa depression, Tarim basin. This paper presents an overview of the types and origin of the sandstone porosity and the controlling factors. Based on the identification of many cast and fluorometric slices by using the field emission scanning electron microscope and confocal microscope, eight types of pores and two kinds of fissures in this sandstone reservoir are recognized according to their shape, scale and origin. The pores are dominated by the secondary pores, which is the result of the following complex geological process:1) The sandstone was buried shallow for a long time in the early stage, so no porosity-decreasing effect occurred during the weak compaction; 2) The Early Cementation saved some primary intergranular pores; 3) The porosity was further decreased by the effect of the tectonic compression in the late burial process;4) The secondary pores were mainly formed by the later dissolution, but which didn't evidently change the porosity of the sandstone reservoir.

Key words: Kuqa depression, Cretaceous, sandstones reservoir, diagenesis, controlling factors

CLC Number: 

  • P618.13
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