[1] Wang Guanmin. Tectonic-sedimentary evolution of the Cuoqin basin and TTS hydrocarbon potential[J]. Acta Petrolei Sinica,2001,22(1):31-35.[王冠民.西藏措勤盆地构造沉积演化及含油气远景[J].石油学报,2001,22(1):31-35.]
[2] The Minerals Office of Tibet Municipality. Geology of Tibet Municipality [M]. Beijing: The Publishing House of Geosciences, 1993. 137-225. [西藏自治区地质矿产局.西藏自治区区域地质志[M].北京:地质出版社,1993. 137-225.]
[3] Liang Digang, Zhang Shuichang, Zhang Baomin, et al. Understanding on marine oil generation in China based on Tarim basin[J]. Earth Science Frontiers,2000,7(4):534-547.[梁狄刚,张水昌,张宝民,等.从塔里木盆地看中国海相生油问题[J].地学前缘,2000,7(4):534-547.]
[4] Tu Jianqi, Jin Kuili. Study and comparison on some important indicators with reference to the degree of organic maturation of marine hydrocarbon-source rocks[J]. Advances in Earth Sciences,1999,14(1):18-23.[涂建琪,金奎励.表征海相烃源岩有机质成熟度的若干重要指标的对比与研究[J].地球科学进展,1999,14(1):18-23.]
[5] Song Quanyou, Ren YongJun. The evaluation of lower cretaceous Duoba formation source rocks in Cuoqin basin, Qingzang plateau[J]. Northwest Geoscience,1999,20(1):27-33. [宋全友,任拥军.青藏措勤盆地早白垩世多巴组烃源岩评价[J].西北地质科学,1999,20(1):27-33.]
[6] Song Quanyou, Chen Qinghua, Chen Shuping. Characteristics of cap rocks in Cuoqin basin,Tibet[J]. Journal of Geomechanics, 1998,4(3):64-69.[宋全友,陈清华,陈书平.西藏措勤盆地盖层条件分析[J].地质力学学报,1998,4(3):64-69.]
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