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Xie Xiaoan, Wany Rende, Li Guangwen, Lu Huafu. The Origin of Erosional Valley of Southern Mangar Sag in Tarim Basin and Anal ysis about its Petroleum Geol ogy Significance[J]. Acta Sedimentologica Sinica, 1996, 14(2): 41-46.
Citation: Xie Xiaoan, Wany Rende, Li Guangwen, Lu Huafu. The Origin of Erosional Valley of Southern Mangar Sag in Tarim Basin and Anal ysis about its Petroleum Geol ogy Significance[J]. Acta Sedimentologica Sinica, 1996, 14(2): 41-46.

The Origin of Erosional Valley of Southern Mangar Sag in Tarim Basin and Anal ysis about its Petroleum Geol ogy Significance

  • Received Date: 1995-12-02
  • Tarim hasin, which is located in the northwest area of China, is the largest intracratonic petroliferous basin in China. There are strong energy seismic waves intercalated between Tg5;Tg5 seismic reflecting layers (the Middle and Upper Ordovician) in the most seismic sections of southern Mangar Sag in the basin. The abnormal reflected waves are present not only in north一south sections,but also in west一east ones. Closed net tracing correlation can be conducted in Mangar area with a size of about 30,000 square kilometers, indicating that these geological interfaces do exist underground.Based on the analysis of seismic reflection characteristics, geodynamic aspects of this basin,and the theory about under current of deoCearl,it is considered that the Lower Paleo-zoic eroxional valley of Mangar Sag in Tarim basin was caused by the erosion truncation of un-der current of deep ocean. Dnder current of deep ocean is another kind of current of deep wa-ier besides turhidity one. "hhc under current may erode most area of continental rise,and trun-Fate deep gullet and even much older sediments. In the large erosional valley,it may be de-posited various kinds of sediments,including a small scale volcanic rock. Wells Tazh ong 31and 33,which take anomaly body as the drilling object,penetrated the formation (Tg5 wave group) of a deep water sediment of dark gray shale with interhedded thin fine sand and silt,and thin (only 10 miters)andesite. Mangar sag is one oI the most important hydrocarbon一bearing depressions in the basin,and recent一year一exploration has proved that Cambrian and Ordovician are the most important source rocks in cast Tarim basin. So the crosional valley is located at perspective position near the oil source. It is possible to form lithologic deposits. Bi-tuminous sand and oil tract have been shown from siliirian to Llpper Ordovician in wells Tazhong 31 and 33.and a little dense oil has been got in well Tazhong 31.Above all,petroleum geological conditions of the erosional valley are extremely supprior and it may become an important ob.lect of oil and gas exploration in Tarim basin.
  • [1] 1.王仁德,满加尔凹陷古生代等深积岩及其含油气性,新疆石油地质,1995, 16(2)。

    2.杨克明,熊水旭等,中国西北地区板i!勾造与盆地类型,石油与天然气地质,1992, 23(1)。

    3.肖序常,汤耀庆等,新疆北部及其邻区大地构造,北京:地质出版社,1992。

    4.C. D. Hollister,深海等深积岩的概念,见:姜衍文,吴智勇等编,深海等深流沉积研究进展,西安:西北大学出版社,1993。

    5.陈汉林,方大钧等,从古地磁结果探讨塔里木板块与华北板块的相互关系,南京大学学报(地球科学).1994, 6(2)。

    6.方大钩,杨树峰等,中国气大板块晚古生代、中生代古地磁结果与构造演化、相互关系的初探,见:李清波,戴金星等主编,现代地质学研究文集(上),南京:南京大学出版社,1992。
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  • Received:  1995-12-02

The Origin of Erosional Valley of Southern Mangar Sag in Tarim Basin and Anal ysis about its Petroleum Geol ogy Significance

Abstract: Tarim hasin, which is located in the northwest area of China, is the largest intracratonic petroliferous basin in China. There are strong energy seismic waves intercalated between Tg5;Tg5 seismic reflecting layers (the Middle and Upper Ordovician) in the most seismic sections of southern Mangar Sag in the basin. The abnormal reflected waves are present not only in north一south sections,but also in west一east ones. Closed net tracing correlation can be conducted in Mangar area with a size of about 30,000 square kilometers, indicating that these geological interfaces do exist underground.Based on the analysis of seismic reflection characteristics, geodynamic aspects of this basin,and the theory about under current of deoCearl,it is considered that the Lower Paleo-zoic eroxional valley of Mangar Sag in Tarim basin was caused by the erosion truncation of un-der current of deep ocean. Dnder current of deep ocean is another kind of current of deep wa-ier besides turhidity one. "hhc under current may erode most area of continental rise,and trun-Fate deep gullet and even much older sediments. In the large erosional valley,it may be de-posited various kinds of sediments,including a small scale volcanic rock. Wells Tazh ong 31and 33,which take anomaly body as the drilling object,penetrated the formation (Tg5 wave group) of a deep water sediment of dark gray shale with interhedded thin fine sand and silt,and thin (only 10 miters)andesite. Mangar sag is one oI the most important hydrocarbon一bearing depressions in the basin,and recent一year一exploration has proved that Cambrian and Ordovician are the most important source rocks in cast Tarim basin. So the crosional valley is located at perspective position near the oil source. It is possible to form lithologic deposits. Bi-tuminous sand and oil tract have been shown from siliirian to Llpper Ordovician in wells Tazhong 31 and 33.and a little dense oil has been got in well Tazhong 31.Above all,petroleum geological conditions of the erosional valley are extremely supprior and it may become an important ob.lect of oil and gas exploration in Tarim basin.

Xie Xiaoan, Wany Rende, Li Guangwen, Lu Huafu. The Origin of Erosional Valley of Southern Mangar Sag in Tarim Basin and Anal ysis about its Petroleum Geol ogy Significance[J]. Acta Sedimentologica Sinica, 1996, 14(2): 41-46.
Citation: Xie Xiaoan, Wany Rende, Li Guangwen, Lu Huafu. The Origin of Erosional Valley of Southern Mangar Sag in Tarim Basin and Anal ysis about its Petroleum Geol ogy Significance[J]. Acta Sedimentologica Sinica, 1996, 14(2): 41-46.
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