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Huang Huafang, Yang Zhanlong, Peng Zuolin. Paleomagnetic Study on the Oil-Gas Geology of the Ordos Basin[J]. Acta Sedimentologica Sinica, 1995, 13(4): 161-168.
Citation: Huang Huafang, Yang Zhanlong, Peng Zuolin. Paleomagnetic Study on the Oil-Gas Geology of the Ordos Basin[J]. Acta Sedimentologica Sinica, 1995, 13(4): 161-168.

Paleomagnetic Study on the Oil-Gas Geology of the Ordos Basin

  • Received Date: 1994-12-02
  • Publish Date: 1995-12-10
  • The results of paleomagnetic research show that the Ordos Basin was located within the paleolatitude of 14°~20°N during the Cambrian and Early-middle Ordovician Periods with a warmer and moist climate, of which the littoral-neritic sedimentary strata in the north and south margins were very rich in organic materials, being favorable fields to find Early Paleozoic oil and gas. From the Late Ordovician to Early Carboniferous, the Ordos Basin may have a large-scale N-S horizontal tectonic displacement. In the Late Carboniferous and Permian Period, the location of Ordos Basin was at around 20°N with widespread limnogenic deposits,being important source rocks of Coal-oil and coal-gas. From the Triassic to Jurassic Period,the Ordos Basin was located at 24°~31°N. And the change of arid and humid climate and the differential tectonic rotations among the Ordos Block and other blocks resulted in favorable conditions for oil and gas formation and accumulation within the marginal areas of the basin. Thus, much more Mesozoic oil and gas reources should be found hopefully.
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    2.方大钧等,1988,山西宁武盆地三叠纪、侏罗纪古地磁结果的构造意义,科学通报,33(2):133-135。

    3.E. A.黑尔伍德著,舒孝敬译,1991,磁性地层学,地质出版社。

    4.Zhao X. X. et al.,1987,Palaeotnagnetic constrains on collision and rotation of North and South China, Nature, 327.141-144.

    5.林金录,1987,中国古地磁数据表(1),地质科学,(2):183-187。

    6.林金录,1989,中国古地磁数据表(2),地质科学,(4):400-404。

    7.McElhinny, M. W. et al.,1981,Fragmentation of Asia in the Permian. Nature, 293. 212-216.

    8.孟自芳等,1990,酒西盆地晚二叠纪古地磁极及其大地构造意义,沉积学报,8(3):58-65。

    9.孟自芳,1992,河西走廊晚二叠世红层的古地磁结果,科学通报,137(7):637 - 640。

    10. 孟自芳等,1992,河西走廊上志留统古地磁结果的大地构造意义,中国科学(B),(5):531- 536。

    11.黄华芳等,1993,酒西盆地南缘推筱构造及其含油领域,石油与天然气地质,14(3), 181-190。
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  • Received:  1994-12-02
  • Published:  1995-12-10

Paleomagnetic Study on the Oil-Gas Geology of the Ordos Basin

Abstract: The results of paleomagnetic research show that the Ordos Basin was located within the paleolatitude of 14°~20°N during the Cambrian and Early-middle Ordovician Periods with a warmer and moist climate, of which the littoral-neritic sedimentary strata in the north and south margins were very rich in organic materials, being favorable fields to find Early Paleozoic oil and gas. From the Late Ordovician to Early Carboniferous, the Ordos Basin may have a large-scale N-S horizontal tectonic displacement. In the Late Carboniferous and Permian Period, the location of Ordos Basin was at around 20°N with widespread limnogenic deposits,being important source rocks of Coal-oil and coal-gas. From the Triassic to Jurassic Period,the Ordos Basin was located at 24°~31°N. And the change of arid and humid climate and the differential tectonic rotations among the Ordos Block and other blocks resulted in favorable conditions for oil and gas formation and accumulation within the marginal areas of the basin. Thus, much more Mesozoic oil and gas reources should be found hopefully.

Huang Huafang, Yang Zhanlong, Peng Zuolin. Paleomagnetic Study on the Oil-Gas Geology of the Ordos Basin[J]. Acta Sedimentologica Sinica, 1995, 13(4): 161-168.
Citation: Huang Huafang, Yang Zhanlong, Peng Zuolin. Paleomagnetic Study on the Oil-Gas Geology of the Ordos Basin[J]. Acta Sedimentologica Sinica, 1995, 13(4): 161-168.
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