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现代地质 ›› 2009, Vol. 23 ›› Issue (6): 1121-1125.

• 石油地质学 • 上一篇    下一篇

塔河油田四区奥陶系古岩溶流域的倒淌河及其成因研究

 刘永立1,2, 蔡忠贤1,3   

  1. 1中国地质大学 资源学院,湖北 武汉430074;2中国石化西北油田分公司 勘探开发研究院,新疆 乌鲁木齐830011;
    3中国地质大学 构造与油气资源教育部重点实验室,湖北 武汉430074
  • 收稿日期:2009-05-15 修回日期:2009-07-25 出版日期:2009-12-29 发布日期:2012-02-16
  • 作者简介:刘永立,男,硕士,1982年出生,石油地质学专业,主要从事碳酸盐岩储层地质学方面的研究工作。 Email:liuyongli526@126.com。
  • 基金资助:

    国家“973”项目(2005CB422105)

The Inverted River and Its Origin in Palaeo-karst Drainage Basin of Ordovician in Block 4, Tahe Oilfield

 LIU  Yong-Li1,2, CAI  Zhong-Xian1,3   

  1. 1Faculty of Resources, China University of Geosciences, Wuhan, Hubei430074, China;
    2Research Institute of Petroleum Exploration & Production, Northwest Oilfield Company, SINOPEC, Urumqi, Xinjiang830011, China;
    3Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan, Hubei430074, China
  • Received:2009-05-15 Revised:2009-07-25 Online:2009-12-29 Published:2012-02-16

摘要:

在现代岩溶区,由于构造运动、岩性差异以及地貌起伏等因素,常常出现水系袭夺现象,并随之伴生一系列反常的水文地貌现象,如分水岭迁移和破坏、袭夺肘、风峡、断头河和倒淌河等。基于三维地震资料,应用层拉平技术、精细相干分析技术及相关地震成图技术,对塔河油田四区中—下奥陶统顶部海西早期的岩溶古地貌和古水系进行了恢复识别,发现也存在类似的反常水文地貌现象。借鉴现代水系袭夺理论,证实了塔河油田四区东部岩溶流域早期为南向汇流结构,而后期由于构造运动引起西北部侵蚀基准面下降,并通过地下途径对邻近南向流域北缘进行逐步袭夺,形成了大型倒淌河,再现了本区岩溶古水系及流域的阶段性演化过程,从而为揭示塔河油田奥陶系古岩溶发育规律提供了重要的依据。

关键词: 倒淌河, 水系袭夺, 古岩溶, 奥陶系, 塔河油田

Abstract:

Because of structure movement, lithology diversity, morphologic prominence, etc, river system capture usually appears in modern karst drainage basin, accompanied by a series of peculiar hydrogeomorphic phenomenon like divide move- damage, capturing elbow, wind gap, beheaded river and inverted river, etc. Based on 3D seismic data, by applying flattening, accurate coherence analysis and seismic imaging, the karst palaeogeomorphology and palaeodrainage pattern are described and recognized, where the peculiar hydrogeomorphic phenomenon is discovered. In the light of the theory on modern river system capture, it had been south- confluence structure in the east of Block 4, Tahe Oilfield. Then, the base level of erosion had declined in the northwest, and the north border of south-confluence drainage basin was captured by underground way, so the inverted river was builtup. The evolutionary process of karst palaeodrainage pattern and drainage basin were reappeared, supplying a signi
ficant foundation for revealing Ordovician palaeo-karst built-up regular pattern for Tahe Oilfield.

Key words: inverted river, river system capture, palaeo-karst, Ordovician, Tahe Oilfield

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