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GUOZe-qing, ZHONGJian-hua, LIUWei-hong, WENZhi-feng, LIU Zu-han, WANG Hai-qiao. Reservoir Characteristicsand Significance of Tertiary Lacustrain Reef in Western Qaidam[J]. Acta Sedimentologica Sinica, 2004, 22(3): 425-433.
Citation: GUOZe-qing, ZHONGJian-hua, LIUWei-hong, WENZhi-feng, LIU Zu-han, WANG Hai-qiao. Reservoir Characteristicsand Significance of Tertiary Lacustrain Reef in Western Qaidam[J]. Acta Sedimentologica Sinica, 2004, 22(3): 425-433.

Reservoir Characteristicsand Significance of Tertiary Lacustrain Reef in Western Qaidam

  • Received Date: 2003-09-09
  • Rev Recd Date: 2003-11-19
  • Publish Date: 2004-09-10
  • In the western Qaidam basin, Tertiary lacustrine reef has been discovered recently in several kilometers strata from the lower member of lower Ganchaigou formation to lower Youshashan formation in Ganchaigou area. On the basis of numerous observations on outcrop, thin sections and casting sections of the reef, and the application of various analytical techniques including analysis of capillary pressure curve and pattern analysis of pore structure, reservoir characteristics of reef have been thoroughly studied. The reef has complex types of pores, such as skeletal pores, intraparticle pores, moldic pores and corroded cavities, and so on. The reef underwent four diagenetic period, such as syngenetic, eogenetic, telogenetic, and hypergene diagenetic period. The formation of the pores are mainly affected by the cementation and dissolution with few primary pores, however, the secondary pores are abundant and form excellent reservoir for oil and gas. The discovery of the Tertiary lacustrine reef in the Qaidam Basin is of important practical significance for the exploration and development of the Qinghai oilfield.
  • [1] 钟建华,温志峰,郭泽清,等.柴达木盆地西部古近纪-新近纪早期湖泊生物礁研究.地质学报(英文版),2004,78(3):736~743[Zhong Jianhua, Wen Zhifeng, Guo Zeqing, et al. Paleogene and early Negene lacustrine reefs in the western Qaidam Basin, China. Acta Geologica Sinica(English Edition),2004,78(3):736~743]
    [2] 库兹涅佐夫 B Γ.礁地质学及礁的含油气性. 北京:石油工业出版社,1983. 111~114[ B.Γ.КУЭНЕЦОВ. ГЕОЛОГИЯРИФОВИИХНЕФТЕГАЭОНОСНОТь.Beijing: Petroleum Industry Press,1983.111~114]
    [3] Riding R. Structure and composition of organic reefs and carbonate mud mounds: concepts and categories. Earth-Science Reviews, 2002,58(1-2):163~231
    [4] Dill R F, Shinn E A, Jones A T, Kelly K, Steinen R P. Giand subtidal stromatolites forming in normal alinity waters. Nature, 1986, 324(6):55~58
    [5] Aitken J D. Classification and environmental significance of cryptalgal limestone and dolomites, with illustration from the Cambrian and Ordovician of Southwestern Alberta. Journal of Sedimentary Petrology, 1967, 37:1163~1178
    [6] James N P, Chopuette P W. Diagenesis-5,limestone: introduction. Geoscience Canada, 1983, 10: 159~161
    [7] 强子同. 碳酸盐岩储层地质学. 山东东营:石油大学出版社,1989. 46~49 [Qiang Zitong. Reservoir geology of carbonate. Dongying Shandong: University of Petroleum Press, 1989, 46~49]
    [8] 陈子炓,寿建峰,斯春松,等. 柴达木盆地花土沟油区上干柴沟组-下油砂山组碳酸盐岩储层特征.成都理工学院学报, 2001, 28(1):53~58 [Chen Ziliao, Shou Jianfeng, Si Chunsong, et al. Carbonate rock reservoir of Shangganchaigou formation and Xiayoushashan formation in neogene Huatugou oil field,Western Qaidam basin. Journal of Chengdu University of Technology, 2001, 28(1):53~58]
    [9] Badiozamani K. The dorag dolomitization model-application to the Middle Ordovician of Wisconsin. Journal Sedimentary Petrology, 1973, 43: 965~984
    [10] 胡明毅,朱忠德,杨威,等. 湖北宜昌早奥陶世生物礁储层特征及控制因素. 江汉石油学院学报, 1998, 20 (4):7~11 [Hu Mingyi, Zhu Zhongde, Yiang Wei, et al. Reservoir characteristics and genesis of lower Ordovician reefs in Yichang, Hubei province. Journal of Jianhan Petroleum Institute, 1998, 20 (4):7~11]
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  • Received:  2003-09-09
  • Revised:  2003-11-19
  • Published:  2004-09-10

Reservoir Characteristicsand Significance of Tertiary Lacustrain Reef in Western Qaidam

Abstract: In the western Qaidam basin, Tertiary lacustrine reef has been discovered recently in several kilometers strata from the lower member of lower Ganchaigou formation to lower Youshashan formation in Ganchaigou area. On the basis of numerous observations on outcrop, thin sections and casting sections of the reef, and the application of various analytical techniques including analysis of capillary pressure curve and pattern analysis of pore structure, reservoir characteristics of reef have been thoroughly studied. The reef has complex types of pores, such as skeletal pores, intraparticle pores, moldic pores and corroded cavities, and so on. The reef underwent four diagenetic period, such as syngenetic, eogenetic, telogenetic, and hypergene diagenetic period. The formation of the pores are mainly affected by the cementation and dissolution with few primary pores, however, the secondary pores are abundant and form excellent reservoir for oil and gas. The discovery of the Tertiary lacustrine reef in the Qaidam Basin is of important practical significance for the exploration and development of the Qinghai oilfield.

GUOZe-qing, ZHONGJian-hua, LIUWei-hong, WENZhi-feng, LIU Zu-han, WANG Hai-qiao. Reservoir Characteristicsand Significance of Tertiary Lacustrain Reef in Western Qaidam[J]. Acta Sedimentologica Sinica, 2004, 22(3): 425-433.
Citation: GUOZe-qing, ZHONGJian-hua, LIUWei-hong, WENZhi-feng, LIU Zu-han, WANG Hai-qiao. Reservoir Characteristicsand Significance of Tertiary Lacustrain Reef in Western Qaidam[J]. Acta Sedimentologica Sinica, 2004, 22(3): 425-433.
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