• 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
WANG Wen-zhi, TIAN JING-chun, ZHANG Xiang, LUO Yang, YANG Wei, TAN Xian-feng. Reservoir characteristics and controlling factors of the 6th member of the Xujiahe Formation in the Guanyinchang-Washi region, southern Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(1): 38-43.
Citation: WANG Wen-zhi, TIAN JING-chun, ZHANG Xiang, LUO Yang, YANG Wei, TAN Xian-feng. Reservoir characteristics and controlling factors of the 6th member of the Xujiahe Formation in the Guanyinchang-Washi region, southern Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(1): 38-43.

Reservoir characteristics and controlling factors of the 6th member of the Xujiahe Formation in the Guanyinchang-Washi region, southern Sichuan

More Information
  • Received Date: March 19, 2011
  • Revised Date: March 24, 2011
  • Published Date: March 29, 2012
  • The petrology, porosity, permeability and controlling factors are explored on the basis of the field investigation, core observation, microscopic examination and well logs from the 6th member of the Xujiahe Formation in the Guanyinchang-Washi region, southern Sichuan. The lithology in the study area mainly consists of medium-to fine-grained feldspathic litharenite and lithic quartz sandstone, with the porosity ranging between 6% and 10% and an average of 7.3%, and with the permeability ranging between 0.03×10-3μm2 and 0.9×10-3μm2 and an average of 0.177×10-3μm2. The reservoirs cited above belong to the typical low-porosity and lowpermeability reservoirs with intergranular and intragranular solution openings. In a planar view, the physical properties of the reservoirs tend to be controlled by sedimentary facies,and vertically, they become sharply poorer due to compaction and cementation with the increase of depths. On the whole, the physical properties of the reservoirs tend to be improved by the rim cementation of chlorite, dissolution of feldspar and tectonism in the study area.
  • Related Articles

    [1]LEI Chuanyang, WANG Bo, LIU Zhaoxin, FAN Min, XIE Haiyang, HAO Jinbo. Development of fluvial terraces in Chengdu Plain: Implications for the paleoclimate and Neotectonic Movement[J]. Sedimentary Geology and Tethyan Geology, 2024, 44(1): 20-33. DOI: 10.19826/j.cnki.1009-3850.2022.07003
    [2]LIANG Lei, XU Guoqiang, HUANG Wuxuan, LIANG Dingyong, LI Sunxiong, HAO Qiang, HUANG Rong. Environmental evolution and its driving mechanisms of southeastern Beibu Gulf since the Last glacial period[J]. Sedimentary Geology and Tethyan Geology, 2023, 43(4): 702-711. DOI: 10.19826/j.cnki.1009-3850.2021.09001
    [3]LI Qiang, ZHANG Ji, CHEN Sihong, TANG Jizhang, PU Wenbin. Investigation and evaluation of shallow geothermal energy resources in key areas of Chengdu[J]. Sedimentary Geology and Tethyan Geology, 2023, 43(2): 271-282. DOI: 10.19826/j.cnki.1009-3850.2023.04004
    [4]Wang Bo, Lei Chuanyang, Liu Zhaoxin, Fan Min, Wang Xingqiang, Ye Fanzhong, Zhang Kun. A geological 3D modeling method of comprehensive geological section for Chengdu[J]. Sedimentary Geology and Tethyan Geology, 2021, 41(1): 112-120. DOI: 10.19826/j.cnki.1009-3850.2020.11003
    [5]Liu Xiaoli. Sedimentary microfacies of the first member of Badaowan Formation in Mahu SAG, Dzungar Basin: Taking well TX1 as an example[J]. Sedimentary Geology and Tethyan Geology, 2021, 41(1): 100-105. DOI: 10.19826/j.cnki.1009-3850.2020.09001
    [6]WANG Yuke, CHEN Hao, FENG Xinglei, CHEN Ming, WANG Donghui. Sedimentary characteristics and engineering geological significance of the middle Pleistocene Hejiang Formation in the eastern suburb platform on the Chengdu Plain, Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2019, 39(3): 33-39.
    [7]DENG Cheng-wen, ZHANG Xia, LIN Chun-ming, XU Zhen-yu, YU Jin. Grain size analysis and environmental evolution indicated by the ZK01 borehole samples in the Changjiang delta since the latest glacial maximum[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(3): 37-46.
    [8]HE Bi, ZHU Li-dong, YANG Wen-guang, FU Shun, ZHANG Qing, TAO Gang, LI Chao, LI Du-wen, TIAN Guang-long, XIE Long. Discovery and geological significance of the Holocene seismites in the Jinsha site in Chengdu, Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(1): 62-69.
    [9]LI Jian-zhong, GUO Yang, YU Tuan, ZHU Hua-ping, WANG Sheng-wei. Earthquakes:An insight[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(1): 58-64.
    [10]DONG Shun-li, LI Yong, QIAO Bao-cheng, MA Bo-lin, ZHANG Yi, CHEN Hao, YAN Liang. Analysis of the new activity of the buried faults in the Chengdu Basin after the 8.0 magnitude Wenchuan earthquake[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(3): 1-7.

Catalog

    Article views (76) PDF downloads (71) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return