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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2015  >  37(4): 407-417
Xu Zhengyu, Yao Genshun, Liang Xing, Xiong Shaoyun, He Yong, Zhang Jiehui, Wang Gaocheng, Liao Yong, Shi Yuanhui. Shale gas preservation conditions in the Lower Paleozoic, Yangtze block[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(4): 407-417. doi: 10.11781/sysydz201504407
Citation: Xu Zhengyu, Yao Genshun, Liang Xing, Xiong Shaoyun, He Yong, Zhang Jiehui, Wang Gaocheng, Liao Yong, Shi Yuanhui. Shale gas preservation conditions in the Lower Paleozoic, Yangtze block[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(4): 407-417. doi: 10.11781/sysydz201504407
shu

Shale gas preservation conditions in the Lower Paleozoic, Yangtze block

doi: 10.11781/sysydz201504407
  • 1.

    Hangzhou Research Institute of Petroleum Geology, Research Institute of Petroleum Exploration and Development, PetroChina, Hangzhou, Zhejiang 310023, China

  • 2. Zhejiang Oilfield Company, PetroChina, Hangzhou, Zhejiang 310013, China

  • 3. Jianghan Petroleum Engineering Co., Ltd., SINOPEC, Qianjiang, Hubei 433123, China

  • Received Date: 2014-05-28
  • Rev Recd Date: 2015-06-04
  • Publish Date: 2015-07-28
    Abstract
  • Two sets of organic-rich shale developed in the Yangtze block during the Early Paleozoic. The first set was in the Lower Cambrian Niutitang Formation, while the second set was in the Upper Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation. The shales experienced four stages of orogenic events, including the Guangxi, Indosinian, Yanshanian and Himalayan. Shales are well-preserved in the Upper Yangtze region and to the west of the middle Yangtze region, where only two or three phases of deformation took place. The shale gas content is high, showing a good potential for exploration. In the east of the middle Yangtze region and the west of the lower Yangtze region, shale gas preservation conditions are poorer due to three or four phases of deformation. As a result, the shale gas content is lower as is the exploration potential. In the east of the lower Yangtze region and in the periphery orogenic front of the Yangtze block, four phases of deformation took place, which led to the poorest preservation conditions for shale gas. As to the whole Yangtze block, the residual synclines are most favorable for shale gas preservation.

     

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