Geological conditions evaluation and favorable areas selection of the shale gas from Longmaxi Formation in the Northeast of Yunnan

被引:0
作者
Zhang, Xu [1 ,2 ]
Liu, Cheng-Lin [1 ,2 ]
Zhu, Yan-Ming [3 ,4 ]
Wang, Yang [3 ,4 ]
Fu, Chang-Qing [3 ,4 ]
机构
[1] Key Laboratory of Shale Oil and Gas Survey and Evaluation, Chinese Academy of Geological Sciences, Beijing
[2] Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing
[3] School of Resources and Geosciences, China University of Mining and Technology, Xuzhou
[4] Key Laboratory of Coalbed Methane Resources and Reservoir Formation Process, The Ministry of Education, China University of Mining and Technology, Xuzhou
关键词
Favorable area; Longmaxi Formation; Northeast of Yunnan; Shale gas;
D O I
10.11764/j.issn.1672-1926.2015.06.1190
中图分类号
学科分类号
摘要
According to measured profiles and lab tests in the Longmaxi Formation of the northeast of Yunnan, TOC and maturity of the samples were determined. And also, the shale gas reservoirs were investigated by XRD, high pressure mercury intrusion, gas absorption and scanning electron microscope. Besides the above methods, isothermal absorption is also used to evaluate the favorable area in the study area. The results show that: (1)the black shales are distributed in the lower segment of Longmaxi Formation, and the average thickness is more than 30 m and it gradually increases from southeast to northwest in the study area. With Yanjin and Daguan counties as the center, the burial depth of strata increases outward. (2)Regionally, TOC of shale increases from south to north, and it is more than 2% in the northwest of Yanjin and the north of Weixin. Vertically, TOC of shale is more than 2% in lower segment of Longmaxi Formation, but less than 1% in the upper segment of Longmaxi Formation. The measured average vitrinite reflectance of shales is 3.6%, showing that the shales are at the over-mature stage. (3)The shales have more brittle minerals in the study area, so the reservoirs are easy to be artificially fractured. Compared with the major gas shales in the north American, clay mineral contents are higher but brittle minerals (quartz, et al.) and carbonate minerals (calcite, et al.) are less in the study area. (4)Mercury injection experiments show that the pores are mainly transition pores and micro pores, but the pore opening degree decreases from the bottom to top in the Longmaxi Formation. Liquid nitrogen adsorption experiments indicate that pores with diameters less than 20nm are better developed in the transition pores and micro pores. Moreover, the two ends of pores are open, with the shapes of cylinders, cones, parallel plates, and a certain amount of flask pores. Measured pore specific surface area is 6.479-17.329cm2/g, with the mean of 11. 425cm2/g. The pore volume is 0.006-0.016cm3/g. The pore average size is 3.256-4.367nm. (5)Isothermal adsorption experiments show that maximum absorbed gas content of the shales in Longmaxi Formation can attain 3.21cm3/g. Comprehensively, this paper has selected three favorable areas for shale gas, including the area between Yanjin and Suijiang county, the northeast of Daguan and the southwest of Weixin. ©, 2015, Science Press. All right reserved.
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页码:1190 / 1199
页数:9
相关论文
共 35 条
[11]  
Zhu Y., Chen S., Fang J., Et al., The geologic background of Siluric shale-gas reservoiring in Szechwan, China, Journal of China Coal Society, 35, 7, pp. 1160-1164, (2010)
[12]  
Lang X., Ye X., Zhang J., Et al., Evaluation of preservation conditions of Lower Paleozoic marine shale gas reservoirs in the northern part of Dianqianbei Depression, Marine Origin Petroleum Geology, 16, 4, pp. 11-21, (2011)
[13]  
Yang Z., Teng G., Li Z., An example of shale gas selected marine area model of Lower Cambrian on the Middle and Upper Yangtze, Natural Gas Geoscience, 22, 1, pp. 8-14, (2011)
[14]  
Hu L., Zhu Y., Chen S., Et al., Resource potential analysis of shale gas in Lower Cambrian Qiongzhusi Formation in Middle & Upper Yangtze region, Journal of China Coal Society, 37, 11, pp. 1871-1877, (2012)
[15]  
Ma W., Liu S., Huang W., Et al., Mud shale reservoirs characteristics of Qiongzhusi Formation on the margin of Sichuan Basin, China, Journal of Chengdu University of Technology: Science & Technology Edition, 39, 2, pp. 182-189, (2012)
[16]  
Zhao P., Li X., Tian X., Et al., Study on micropore structure characteristics of Longmaxi Formation shale gas reservoirs in the southern Sichuan Basin, Natural Gas Geoscience, 25, 6, pp. 947-956, (2014)
[17]  
Guo T., Liu R., Implications from marine shale gas exploration breakthrough in complicated structure area at high thermal stage: Taking Longmaxi Formation in well JY1 as an example, Natural Gas Geoscience, 24, 4, pp. 643-651, (2013)
[18]  
Bi H., Jiang Z., Li P., Et al., Adsorption characteristic and influence factors of Longmaxi shale in southeastern Chongqing, Natural Gas Geoscience, 25, 2, pp. 302-310, (2014)
[19]  
Yunnan Bureau of Geology and Mineral Resources, Regional Geology of Yunnan Province, (1990)
[20]  
Yunnan Bureau of Geology and Mineral Resources, Lithostratigraphy of Yunnan Province, (1996)