• The Core Journal of China
  • Included in Chinese Scientific and Technical Papers and Citations Database
  • Included in Chinese Science Citation Database (CSCD)
  • Included in Chemical Abstracts (CA)
  • Included in Scopus
Advanced Search
ZHAN Wang-zhong, HE Yong-zhong, CHEN Wen-bin, ZHU Xun. Restoration of the palaeo-fluid pressures from the Suowa Formation in the Esima area, Qiangtang Basin[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(3): 56-61.
Citation: ZHAN Wang-zhong, HE Yong-zhong, CHEN Wen-bin, ZHU Xun. Restoration of the palaeo-fluid pressures from the Suowa Formation in the Esima area, Qiangtang Basin[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(3): 56-61.

Restoration of the palaeo-fluid pressures from the Suowa Formation in the Esima area, Qiangtang Basin

More Information
  • Received Date: July 29, 2013
  • Revised Date: August 03, 2013
  • Published Date: September 29, 2013
  • The restoration of the palaeo-fluid pressures is explored on the basis of the examination of the fluid inclusions samples from the Suowa Formation reservoirs, Esima area, Qiangtang Basin. There occurred three phases of hydrocarbon charging, of which the second phase of hydrocarbon charging is believed to be the main period for the accumulation in the study area. The timing of the three phases of hydrocarbon generation and accumulation is based on the burial history of the hydrocarbon reservoirs. The palaeo-fluid pressure data are obtained by using the PVT thermodynamic simulation of the fluid inclusions. The results of research for the stratigraphic evolution in the Suowa Formation show that the regional structures and geothermal evolution may be the main controlling factors for the palaeo-fluid pressures. The palaeo-fluid pressures have gone through three stages of evolution:the overpressure systems during the early stage of the hydrocarbon generation, normal hydrostatic pressure systems during the culmination, and low pressure systems during the decline of hydrocarbon generation.
  • Related Articles

    [1]Shui leilei, Liang ru, Meng Xianghao, Guo Laiyuan, Xu Kewei. Characteristics of fluid inclusions in quartz fractures in Ledong area of Yinggehai Basin and its constraints on gas accumulation[J]. Sedimentary Geology and Tethyan Geology, 2020, 40(1): 45-52. DOI: 10.19826/j.cnki.1009-3850(2020)01-0045-08
    [2]Yang Ping, LiuJia-hong, Yang Fei, Wang Zheng-jiang, He Jiang-lin. Fluid inclusions in authigenic quartz and hydrocarbon accumulation in the Dengying Formation in Renhuai,northern Guizhou[J]. Sedimentary Geology and Tethyan Geology, 2018, 38(2): 82-93.
    [3]SHI Mei-feng, FAN Wen-yu, LIN Fang-cheng, WANG Hong, CONG Feng, ZHU Hua-ping. Fluid inclusion analysis and origin of the Pilok tin-tungsten deposit in western Thailand[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(2): 97-104.
    [4]JIA Bin, WEN Hua-guo, LI Ying-bo, LIU Ya-peng, WANG Tao. Fluid inclusions in the salt minerals from the Permian Fengcheng Formation in the Urho region, Junggar Basin, Xinjiang[J]. Sedimentary Geology and Tethyan Geology, 2015, 35(1): 33-42.
    [5]CHEN Yuan-yuan, WANG Guo-zhi, WANG Dong, WANG Dong, WANG Ying-jun. Fluid inclusions from the Palaeozoic hydrocarbon reservoirs in eastern Tarim Basin,Xinjiang[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(4): 68-72.
    [6]WANG Chun-lian, HOU Zhong-jian, LIU Li-hong. Fluid inclusions and hydrocarbon accumulation in the eighth member of the Lower Shihezi Formation in northwestern Ordos Basin[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(3): 63-70.
    [7]LIANG Shu-yi, JIANG You-lu, QIU Dong-zhou. The pressure systems and dynamic mechanisms for oil and gas accumulation in the Boxing region,Shandong[J]. Sedimentary Geology and Tethyan Geology, 2005, 25(4): 78-82.
    [8]SUN Zhi-ming, LI Xing-zhen, SHEN Gan-fu, DU De-xun, JIANG Xin-sheng. Fluid inclusions from the Xuelongshan ductile shear zone, Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(3): 82-86.
    [10]Xiao Linping. THERMODYNAMIC MODEL FOR EXPERIMENTAL SIMULATION OF DISSOLUTION OF THE CARBONATE ROCKS IN THE BURIAL ENVIRONMENTS:AN EXAMPLE FROM THE FIFTH MEMBER OF THE LOWER DEVONIAN MAJIAGOU FORMATION IN THE SHAANXI-GANSU-NINGXIA BASIN[J]. Sedimentary Geology and Tethyan Geology, 1997, 17(4): 57-70.

Catalog

    Article views (135) PDF downloads (76) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return