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Article Navigation >  Acta Sedimentologica Sinica  > 1998  >  16(1): 126-131

Li Yumei, Zhao Chenglin. Study on Diagenesis in the Slope of the Saline Lake Basin:An Example From the Tertiary of the Aer jin Slope in Caidam Basin[J]. Acta Sedimentologica Sinica, 1998, 16(1): 126-131.
Citation: Li Yumei, Zhao Chenglin. Study on Diagenesis in the Slope of the Saline Lake Basin:An Example From the Tertiary of the Aer jin Slope in Caidam Basin[J]. Acta Sedimentologica Sinica, 1998, 16(1): 126-131.
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Study on Diagenesis in the Slope of the Saline Lake Basin:An Example From the Tertiary of the Aer jin Slope in Caidam Basin

  • Geoscience Department Uaiversity of Petroleum Beijing 102200

  • Received Date: 1997-03-06
  • Rev Recd Date: 1997-12-30
  • Publish Date: 1998-03-10
  • The Tertiary in the Aerjin Slope in Caidam Basin is characterized by strong carbonate recrystallization，weak compaction, weak quartz overgrowth and enrichment of the early-stage carbonate. The carbonate ce-ment,influenced by the salinity to some degree,is mainly inorganic with few relation to biogas. In muds clayassemblage is illite-illite/montmorillonite-chlorite. With the increase of depth the relative content of illite fluc-tuates and that of chlorite decreases. The illite may be terrestrial origin.
  • [1] 1 黄杏珍，邵宏舜，顾树松等.柴达木盆地的油气形成与寻找油气田方向，兰州:甘肃科学技术出版社，1993. 80-106

    2 Weaver C E. C1ays,Muds,and Shales. Elsevier Science PublishingCompany Inc. 1989. 270---278

    3 华保钦，林锡祥.柴达木盆地异常地层压力及其成因探讨.沉积学报，1983,1(4061-78

    4 于升松·柴达木盆地盐湖水化学特征，海洋与湖沼.1984,1(40340---358

    5 徐放.柴达木盆地某些盐湖沉积剖面中粘土矿物的初步研究.沉积学报.1983,1(30 123-128
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Publishing history
  • Received:  1997-03-06
  • Revised:  1997-12-30
  • Published:  1998-03-10

Study on Diagenesis in the Slope of the Saline Lake Basin:An Example From the Tertiary of the Aer jin Slope in Caidam Basin

  • Geoscience Department Uaiversity of Petroleum Beijing 102200
  • Received Date: 1997-03-06
  • Rev Recd Date: 1997-12-30
  • Publish Date: 1998-03-10

Abstract: The Tertiary in the Aerjin Slope in Caidam Basin is characterized by strong carbonate recrystallization，weak compaction, weak quartz overgrowth and enrichment of the early-stage carbonate. The carbonate ce-ment,influenced by the salinity to some degree,is mainly inorganic with few relation to biogas. In muds clayassemblage is illite-illite/montmorillonite-chlorite. With the increase of depth the relative content of illite fluc-tuates and that of chlorite decreases. The illite may be terrestrial origin.

Li Yumei, Zhao Chenglin. Study on Diagenesis in the Slope of the Saline Lake Basin:An Example From the Tertiary of the Aer jin Slope in Caidam Basin[J]. Acta Sedimentologica Sinica, 1998, 16(1): 126-131.
Citation: Li Yumei, Zhao Chenglin. Study on Diagenesis in the Slope of the Saline Lake Basin:An Example From the Tertiary of the Aer jin Slope in Caidam Basin[J]. Acta Sedimentologica Sinica, 1998, 16(1): 126-131.
shu

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