Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (2): 569-578.doi: 10.13278/j.cnki.jjuese.20190317

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Genetic Mechanism of High Content Tuffaceous Clastic Rock Reservoir in Hailar-Tamucage Basin

Meng Qi'an, Li Junhui, Li Yue, Zou Yue   

  1. Exploration and Development Research Institute, Daqing Oilfield Company Limited, Daqing 163712, Heilongjiang, China
  • Received:2019-12-27 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Science and Technology Major Project(2016E-0202)

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Abstract: High content of tuffaceous clastic rock reservoirs are widely developed in Tongbomiao Formation and Nantun Formation in the central oil-rich depression of Hailar-Tamucage basin,but the genetic mechanism is unclear. Based on the comprehensive analyses of core, logging, well logging and thin section data, combined with the volcanic events in Hailar-Tamucage basin and its surrounding areas, it is considered that the high tuffaceous clastic rocks developed in the middle oil-rich depression include mainly tuffaceous sandstone, tuffaceous mudstone, and tuffs. In different periods, the development characteristics of high content tuffaceous clastic rock reservoirs are different in different depressions. As a whole, the tuffaceous content in the reservoirs from Tongbomiao Formation to Nantun Formation is getting lower and lower. The high tuffaceous clastic reservoir is mainly developed in the sedimentary period of Tongbomiao Formation and the lower part of Nantun Formation. The volcanic material in the high content tuffaceous clastic rock reservoir is not derived from the basic volcanic activity in the fault depression period, but from the large-scale acidic volcanic eruption event in Daxing'anling area. There are two types of genetic mechanism of the high content tuffaceous clastic reservoir in Hailar-Tamucage basin:one is the direct air drop type of volcanic ash in the same sedimentary period, and the other is the water carrying type that the volcanic ash first dropped on the land and then deposited after being transported in the same sedimentary period. The pyroclastic material in the high tuffaceous clastic rock reservoir is easy to be dissolved by organic acid to form the secondary pores, which provided effective reservoir spaces for the deep oil and gas accumulation, and the volcanic eruption promoted the formation of high-quality source rocks, which is of great significance for oil and gas exploration.

Key words: Hailar-Tamucage basin, central oil-rich depression, Tongbomiao Formation, Nantun Formation, high tuffaceous clastic reservoir, genetic mechanism

CLC Number: 

  • P618.13
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