塔里木盆地油气勘探成果与勘探方向
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摘要
自1989年4月10日塔里木油田分公司成立以来,在塔里木盆地前陆区库车坳陷、台盆区碳酸盐岩和台盆区碎屑岩3个领域取得了辉煌的勘探成果,累计探明油气地质储量28.8×108t当量,成为"西气东输"主力气源地,建成中国陆上第三大油气田。30年勘探实践中,对前陆区库车坳陷、西南坳陷,台盆区碳酸盐岩、台盆区碎屑岩油气地质认识不断深化,明确了库车坳陷、台盆区和西南坳陷三大含油气系统的烃源岩、储盖组合、构造样式、圈闭类型和油气藏模式。塔里木盆地剩余勘探潜力大,下一步要继续精细勘探库车坳陷克拉苏构造带、塔北隆起西部碎屑岩、塔北—满西奥陶系一间房组,发现落实规模储量;要加大库车坳陷秋里塔格构造带、北部构造带侏罗系,台盆区奥陶系深层、寒武系盐下,西南坳陷山前等领域的研究和勘探力度,实现接替领域的战略突破。
Ever since the foundation of Tarim Oilfield Company on April 10, 1989, great achievements have been obtained in 3 major fields: Kuqa foreland depression, carbonate rocks and clastics in the platform region with the cumulative proved oil and gas reserves amounting to 2.88 billion tons(equivalent). Tarim oilfield has become the major source area for the West-to-East natural gas transmission project and the third large oil and gas field in the mainland China. During the past 30 years of exploration practice, geological understandings about the foreland Kuqa depression, Southwest depression, carbonate rocks in the platform region and clastics in the platform region were continuously deepened, and the source rock, reservoir-cap rock assemblage, structure style, trap and reservoir model were identified for the 3 petroleum systems such as Kuqa depression, platform region and Southwest depression. The remaining exploration potentials of Tarim basin are enormous. The fine exploration should be carried out in the Kelasu tectonic belt of Kuqa depression, clastics in the western Tabei uplift, Ordovician Yijianfang formation in Tabei—Manxi area. The researches and exploration of Qiulitage tectonic belt in Kuqa depression, Jurassic series in the northern tectonic belt, Ordovician deep series in the platform region, Cambrian subsalt strata and piedmont area in the Southwest depression should be strengthened and the strategic breakthrough can be made.
Ever since the foundation of Tarim Oilfield Company on April 10, 1989, great achievements have been obtained in 3 major fields: Kuqa foreland depression, carbonate rocks and clastics in the platform region with the cumulative proved oil and gas reserves amounting to 2.88 billion tons(equivalent). Tarim oilfield has become the major source area for the West-to-East natural gas transmission project and the third large oil and gas field in the mainland China. During the past 30 years of exploration practice, geological understandings about the foreland Kuqa depression, Southwest depression, carbonate rocks in the platform region and clastics in the platform region were continuously deepened, and the source rock, reservoir-cap rock assemblage, structure style, trap and reservoir model were identified for the 3 petroleum systems such as Kuqa depression, platform region and Southwest depression. The remaining exploration potentials of Tarim basin are enormous. The fine exploration should be carried out in the Kelasu tectonic belt of Kuqa depression, clastics in the western Tabei uplift, Ordovician Yijianfang formation in Tabei—Manxi area. The researches and exploration of Qiulitage tectonic belt in Kuqa depression, Jurassic series in the northern tectonic belt, Ordovician deep series in the platform region, Cambrian subsalt strata and piedmont area in the Southwest depression should be strengthened and the strategic breakthrough can be made.
引文
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[12]李勇,漆家福,师俊,等.塔里木盆地库车坳陷中生代盆地性状及成因分析[J].大地构造与成矿学,2017,41(5):829-842.LI Yong,QI Jiafu,SHI Jun,et al. Characteristics of Mesozoic basin in Kuqa depression,Tarim basin[J]. Geotectonica et Metallogenia,2017,41(5):829-842.
[13]卢华复,陈楚铭,刘志宏.库车再生前陆逆冲带的构造特征与成因[J].石油学报,2000,21(3):18-24.LU Huafu,CHEN Chuming,LIU Zhihong. The structural features and origin of the Kuqa rejuvenation foreland thrust belt[J]. Acta Petrolei Sinica,2000,21(3):18-24.
[14]卢华复,贾承造,贾东,等.库车再生前陆盆地冲断构造楔特征[J].高校地质学报,2001,7(3):257-271.LU Huafu,JIA Chengzao,JIA Dong,et al. Features of the thrust wedge of deformation belt in Kuqa rejuvenation foreland basin[J].Geological Journal of China Universities,2001,7(3):257-271.
[15]汤良杰,贾承造,皮学军,等.库车前陆褶皱带盐相关构造样式[J].中国科学D辑:地球科学,2003,33(1):38-46.TANG Liangjie,JIA Chengzao,PI Xuejun,et al. Salt related structure of Kuqa foreland fold belt[J]. Science in China Series D:Earth Sciences,2003,33(1):38-46.
[16]尹宏伟,王哲,汪新,等.库车前陆盆地新生代盐构造特征及形成机制:物理模拟和讨论[J].高校地质学报,2011,17(2):308-317.YIN Hongwei,WANG Zhe,WANG Xin,et al. Characteristics and mechanics of Cenozoic salt-related structures in Kuqa foreland basins:insights from physical modeling and discussion[J]. Geological Journal of China Universities,2011,17(2):308-317.
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