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Meng Zifang. Paleomagnetic Study of the Devonian System in Tarim Basin, China[J]. Acta Sedimentologica Sinica, 1993, 11(3): 88-92.
Citation: Meng Zifang. Paleomagnetic Study of the Devonian System in Tarim Basin, China[J]. Acta Sedimentologica Sinica, 1993, 11(3): 88-92.
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Paleomagnetic Study of the Devonian System in Tarim Basin, China

  • Lanzhou Institute of Geology. Chinese Academy of Scienes

  • Received Date: 1993-01-05
  • Publish Date: 1993-09-10
  • Based on results from 41 oriented cores collected from northwestern and southwestern margins of the Tarim Basin, this paper presents a brief introduction of our recent study on the Devonian System therein. Paleomagnetic data suggest that paleolatitude of the southwestern margin was much lower than that of the norhwestern margin (about 12°). The former was amalgamated to the later during rapid northward drifting of the Tarim Block happening within Carbono-Devonian period. This kind of differential motions among sub -units of the block should be a significant element on tectonic evolution and evaluation of oil and gas within the western part of the Tarim Basin.
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    [2] 林金录，1985，地，地质.7卷1期.81-83页.
    [3] 刘椿等,1986，地质科学13期，232-235页。
    [4] 李燕平等.1988，长春地质学院学报，18卷4期,447-469页.
    [5] 李燕平等,1989，地质学报，3期.193-203页.
    [6] 孟自芳.1991，地质论评.37卷2期.103-108页.
    [7] 孟自芳.1992.科学通报.37卷7期，537-640页.
    [8] 孟自芳等.1992，中国科学(B辑),5期.531-536页。
    [9] 张学斌等.1991，地质论评.37卷2期.160-164页。
    [10] Pruner.p.，1987. Tectonophysics,139, p. 155-167.
    [11] Pruner.P.1987.Tectonophysics.139.p.123-132.
    [12] Khramov, A. N.，1990. Tectonophysics,184, p. 101-109
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  • Received:  1993-01-05
  • Published:  1993-09-10

Paleomagnetic Study of the Devonian System in Tarim Basin, China

  • Lanzhou Institute of Geology. Chinese Academy of Scienes
  • Received Date: 1993-01-05
  • Publish Date: 1993-09-10

Abstract: Based on results from 41 oriented cores collected from northwestern and southwestern margins of the Tarim Basin, this paper presents a brief introduction of our recent study on the Devonian System therein. Paleomagnetic data suggest that paleolatitude of the southwestern margin was much lower than that of the norhwestern margin (about 12°). The former was amalgamated to the later during rapid northward drifting of the Tarim Block happening within Carbono-Devonian period. This kind of differential motions among sub -units of the block should be a significant element on tectonic evolution and evaluation of oil and gas within the western part of the Tarim Basin.

Meng Zifang. Paleomagnetic Study of the Devonian System in Tarim Basin, China[J]. Acta Sedimentologica Sinica, 1993, 11(3): 88-92.
Citation: Meng Zifang. Paleomagnetic Study of the Devonian System in Tarim Basin, China[J]. Acta Sedimentologica Sinica, 1993, 11(3): 88-92.
shu

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