Douglas W W, John M H. 1991. Generation and migration of petroleum from abnormally pressured fluid compartment:discussions and replies. AAPG Bulletin, 75(2): 326~338.
[5]
Du Xu, Zheng Hongyin, Jiao Xiuqiong. 1995. Abnormal pressure and hydrocarbon accumulation. Earth Science Frontiers, 2 (3 ~ 4):137~148 (in Chinese with English abstract).
[6]
Guan Shuwei, Wang Xin, Yang Shufeng, et al. 2003. 3-D structural analysis on the Kuqa\'s Qiulitg anticline zone of the southern Tianshan Mountains, China. Geological Review, 49(5): 464~473 (in Chinese with English abstract).
[7]
Ma Qifu, Chen Sizhong, Zhang Qiming, et al. 2000. Abnormal high pressure basin and oil & gas distribution. Beijing: Geological Publishing House (in Chinese).
[8]
Pi Xuejun, Xie Huiwen, Zhang Cun, et al. 2002. The forming mechanism of abnormal high pressure and its effect on formation of oil and gas reservoir in Kuqa foreland thrust zone. Chinese Science Bulletin, 47 (Supp.): 84~ 90 (in Chinese).
Song Yan, Xia Xinyu, Hong Feng, et al. 2002. Characteristics of abnormal high pressure and mode of natural gas formation in foreland basin. Chinese Science Bulletin, 47(Supp. ):70~76 (in Chinese).
[16]
Xia Xinyu, Song Yan, Fang Dequan. 2001. Influence of tectonic uplift on formation pressure and genesis of the abnormal pressure in Kela-2 gas field. Natural Gas Industry, 21 (1): 30~ 34 (in Chinese with English abstract).
[17]
Xu Guosheng, Kuang Jianchao, Li Jianlin, et al. 2000. Research on the genesis of abnormal high pressure in the foreland basin to the north of Tianshan. Journal of Chengdu University of Technology,27(3):255~262(in Chinese with English abstract).
[18]
Xu Shilin, Lu Xiuxiang, Pi Xuejun, et al. 2002. Abnormally high pressure and its effect on reservoir formation of Kelasu tectonic zone in Kuqa depression in Xinjiang. Geoscience, 16 (3): 282~287 (in Chinese with English abstract).
[19]
Zhu Yuxin, Shao Xinjun, Yang Siyu, et al. 2000. Characteristics and genesis of the abnormal pressure in Kela-2 gas field. Journal of Southwest Petroleum Institute, 22 (4) : 9 ~ 13 (in Chinese with English abstract).