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    库车褶皱冲断带克拉苏三角带及其油气潜力

    杨明慧 金之钧 吕修祥 孙冬胜

    杨明慧, 金之钧, 吕修祥, 孙冬胜, 2002. 库车褶皱冲断带克拉苏三角带及其油气潜力. 地球科学, 27(6): 745-750.
    引用本文: 杨明慧, 金之钧, 吕修祥, 孙冬胜, 2002. 库车褶皱冲断带克拉苏三角带及其油气潜力. 地球科学, 27(6): 745-750.
    YANG Ming-hui, JIN Zhi-jun, LÜ Xiu-xiang, SUN Dong-sheng, 2002. Kelasu Triangle Zone and Its Hydrocarbon Potential in Kuqa Thrust-and-Fold Belts, Tarim Basin. Earth Science, 27(6): 745-750.
    Citation: YANG Ming-hui, JIN Zhi-jun, LÜ Xiu-xiang, SUN Dong-sheng, 2002. Kelasu Triangle Zone and Its Hydrocarbon Potential in Kuqa Thrust-and-Fold Belts, Tarim Basin. Earth Science, 27(6): 745-750.

    库车褶皱冲断带克拉苏三角带及其油气潜力

    详细信息
      作者简介:

      杨明慧(1962-), 男, 副教授, 1998年毕业于中国地质大学(武汉), 获理学博士学位, 目前主要从事盆地分析方面的研究工作

    • 中图分类号: P618.130.2

    Kelasu Triangle Zone and Its Hydrocarbon Potential in Kuqa Thrust-and-Fold Belts, Tarim Basin

    • 摘要: 塔里木盆地库车褶皱冲断带克拉苏构造带在古近系膏盐岩之下发育克拉苏三角带.克拉苏三角带发育时代约在中新世中期, 位于古近系膏盐岩和侏罗系煤系之间, 为Ⅱ类三角带.上新世时, 该三角带底部被突破, 库车褶皱冲断带前缘扩展至秋里塔格构造.克拉苏三角带的发展与超压封套的发生有关; 突破层位在伊-蒙混层向伊利石的转换边界.克拉苏三角带深层是有利的油气勘探目标.

       

    • 图  1  三角带构造分类

      Fig.  1.  Classification of triangle zones

      图  2  库车前陆褶皱冲断带构造纲要

      1.南天山造山带; 2.凸起; 3.研究区; 4.构造单元分界线; 5.褶皱; 6.调节构造

      Fig.  2.  Schematic map of Kuqa foreland thrust-and-fold belts

      图  3  克拉苏三角带构造解释

      (地震剖面BC95-198.5, 位置见图 2)

      Fig.  3.  Tectonic interpretation of Kelasu triangle zone

      图  4  改进的楔冲作用模式[5]

      Fig.  4.  Model of improved tectonic wedging[5]

      图  5  克参1井蒙-伊转换界线与滑脱层位关系

      Fig.  5.  Smectite-illite transition in KC1 well and its relationship with decollement layer

      表  1  库车前陆褶皱冲断带构造扩展年代[20]

      Table  1.   Tectonic expanded ages of Kuqa foreland thrust-and-fold belt[20]

    • [1] Gordy P L, Frey F R, Norris D K. Geological guide for the CSPG 1977: Waterdon-Glacier Park field conference[M]. Canadian Society of Petroleum Geology. [s. l.]: [s. n.], 1977.
      [2] Butler RWH. Thrusttectonics: a personal view[J]. Geological Magazine, 1985, 122: 223-232. doi: 10.1017/S0016756800031435
      [3] Morley C K. A classification of thrust front[J]. AAPG Bull, 1986, 70: 12-25.
      [4] Jones P B. Oil and gas beneath east-dipping underthrust faults in the Alberta Foothills, Canada[A]. In: Powers P B, ed. Geologic studies of the Cordilleran thrust belt[C]. [s. l.]: [s. n.], 1982.
      [5] Jones P B. Triangle zone geometry, terminology and kinematics [J]. Bulletin of Canadian Petroleum Geology, 1996, 44(2): 139-152.
      [6] 杨明慧. 陆内前陆盆地褶皱冲断带构造特征———塔里木盆地库车坳陷例析[D]. 北京: 石油大学, 2002.

      YANG MH. Structural characteristic of fold-and-thrust belt in intracontinental foreland basin— a case study fromKuqa depression in Tarim basin, China[D]. Beijing: University of Petroleum, 2002.
      [7] Avouac J P, Tapponnier P T, Bai M, et al. Active thrusting and folding along the northern Tienshan and Late Conozoic rotation of the Tarim relative to Dzhungaria and Kazakhstan[J]. J Geophys Res, 1993, 98: 6755-6840. doi: 10.1029/92JB01963
      [8] 贾承造. 中国塔里木盆地构造特征与油气[M]. 北京: 石油工业出版社, 1997.

      JIA C Z. The structural features and hydrocarbon of the Tarim basin, China[M]. Beijing: Petroleum Industry Press, 1997.
      [9] 刘志宏, 卢华复, 贾承造, 等. 库车前陆盆地克拉苏构造带的构造特征与油气[J]. 长春科技大学学报, 1999, 29 (3): 215-221. doi: 10.3969/j.issn.1671-5888.1999.03.002

      LIUZ H, LUHF, JIA C Z, et al. Structural characteristics and its relation with hydrocarbon of Kelasu tectonic zone in Kuqa foreland basin[J]. Journal of Changchun University of Science and Technology, 1999, 29(3): 215-221. doi: 10.3969/j.issn.1671-5888.1999.03.002
      [10] 卢华复, 陈楚铭, 刘志宏, 等. 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. doi: 10.3321/j.issn:0253-2697.2000.03.004

      LU H F, CHEN C M, LIU Z H, et al. Structural features and origin of the Kuqa rejuvenation foreland thrust belt[J]. Acta Petrolei Sinica, 2000, 21(3): 18-24. doi: 10.3321/j.issn:0253-2697.2000.03.004
      [11] 汪新, 贾承造, 杨树锋. 南天山库车褶皱冲断带构造几何学和运动学[J]. 地质科学, 2002, 37(3): 372-384. doi: 10.3321/j.issn:0563-5020.2002.03.014

      WANG X, JIA C Z, YANG S F. Geometry and kinematics of the Kuqa fold-and-thrust belt in the southern Tianshan[J]. Scientia Geologica Sinica, 2002, 37(3): 372-384. doi: 10.3321/j.issn:0563-5020.2002.03.014
      [12] Teal P R. The triangle zone at Cabin Creek, Alberta[A]. In: Bally A W, ed. Seismic expression of structural style [C]. AAPG Studies in Geology Series, 1983, 15: 3.
      [13] Banks C J, Warburton J. "Passive-roof" duplex geometry in the frontal structures of the Kirthar and Sulaiman mountain belts, Pakistan[J]. J Structural Geology, 1986, 8: 229237.
      [14] Cooper M A. Passive-roof duplexes and pseudo-passive-roof duplexes atmountain front: a review[J]. Bulletin of Canadian Petroleum Geology, 1996, 44(2): 410-421.
      [15] Price RA. The southeastern Canadian Cordillera: thrustfaulting, tectonic wedging, and delamination of the lithosphere [J]. J Structural Geology, 1986, 8: 239-254. doi: 10.1016/0191-8141(86)90046-5
      [16] 卢华复, 贾东, 陈楚铭, 等. 库车新生代构造性质和变形时间[J]. 地学前缘, 1999, 6(4): 215-221. doi: 10.3321/j.issn:1005-2321.1999.04.003

      LU H F, JIA D, CHEN C M, et al. Nature and timing of the Kuqa Cenozoic structures[J]. Earth Science Frontiers, 1999, 6(4): 215-221. doi: 10.3321/j.issn:1005-2321.1999.04.003
      [17] Lawton D C, Spratt D A, Hopkins J C. Tectonic wedging beneath the Rocky Mountains foreland basin, Alberta, Canada [J]. Geology, 1994, 22: 519-522.
      [18] Jadoon I A K, Frisch W. Hinterland-vergent tectonic wedge below the Riwat thrust, Himalayan foreland, Pakistan: implications for hydrocarbon exploration[J]. AAPG Bull, 1997, 81(3): 438-448.
      [19] Couzens B A, Wiltschko D V. The control of mechanical stratigraphy on the formation of triangle zones[J]. Bulletin of Canadian Petroleum Geology, 1996, 44(2): 165-179.
      [20] Romas V A. Andean foothills structures in northern Magallanes basin, Argentina[J]. AAPG Bull, 1989, 73: 887903.
      [21] Hubbert M K, Rubey W W. Role of fluid pressure in mechanics of overthrustfaulting[J]. Geological Society ofAmerican Bull, 1959, 70: 115-166. doi: 10.1130/0016-7606(1959)70[115:ROFPIM]2.0.CO;2
      [22] Davis D, Suppe J, Dahlen F A. Mechanics of fold-and-thrust belts and accretionary wedges[J]. J Geophys Res, 1983, 88: 1153-1172. doi: 10.1029/JB088iB02p01153
      [23] Sanderson D A, Spratt D A. Triangle zone and displacement transfer structures in the eastern front ranges, southern Canadian Rocky Mountains[J]. AAPG Bull, 1992, 76: 828839.
      [24] 夏新宇, 宋岩, 房德权. 构造抬升对地层压力的影响及克拉2气田异常压力成因[J]. 天然气工业, 2001, 21 (1): 30-34. doi: 10.3321/j.issn:1000-0976.2001.01.006

      XIA X Y, SONG Y, FANG D Q. Influence of tectonic uplift on formation pressure and genesis of the abnormal pressure in Kela-2 gas field[J]. Natural Gas Industry, 2001, 21(1): 30 doi: 10.3321/j.issn:1000-0976.2001.01.006
      [25] Chenevert M E, Gatlin C. Mechanical anisotropies of laminated sedimentary rocks[J]. Journal of the Society of Petroleum Engineers, 1965, 5: 67-77. doi: 10.2118/890-PA
      [26] Bruce C H. Smectite dehydration— its relation to structural development and hydrocarbon accumulation in northernGulf of Mexico basin[J]. AAPG Bull, 1984, 68: 673-683.
      [27] 赵杏媛, 王行信, 张有瑜, 等. 中国含油气盆地粘土矿物[M]. 武汉: 中国地质大学出版社, 1995.

      ZHAO X Y, WANG X X, ZHANG YY, et al. Clay minerals in petroliferous basin of China[M]. Wuhan: China University of Geosciences Press, 1995.
      [28] 曾联波, 金之钧, 汤良杰, 等. 柴达木盆地北缘油气分布的构造控制作用[J]. 地球科学———中国地质大学学报, 2001, 26(1): 54-58. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200101010.htm
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    • 收稿日期:  2002-08-12
    • 刊出日期:  2002-11-25

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