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Du Xiaodi, Wang Pujun, Kuang Lichun, Wang Dongpo. The Reconstruction and Origin of Sealevel Changes ofSinian Period to Dovinian Period in Tarim Basin[J]. Acta Sedimentologica Sinica, 1997, 15(3): 14-17.
Citation: Du Xiaodi, Wang Pujun, Kuang Lichun, Wang Dongpo. The Reconstruction and Origin of Sealevel Changes ofSinian Period to Dovinian Period in Tarim Basin[J]. Acta Sedimentologica Sinica, 1997, 15(3): 14-17.

The Reconstruction and Origin of Sealevel Changes ofSinian Period to Dovinian Period in Tarim Basin

  • Received Date: 1996-08-10
  • Publish Date: 1997-09-10
  • Based on sequence stratigraphy work for the outcrops in Tarim Basin, The author sets up theSealevel changes curve of sinian period to Devonian period. Then the author studies the relationship be-tween oxygen isotope and sealevel changes and finds the oxygen isotope ratio' s increase and decredse in-dicating the sealevel' s down and up. The correctness of sealevel changes curve is tested and verified bythe result of oygen isotope. The ranges of sealevel changes are calculated. Finally the author elaboratesthe formation mechanism of sealevel changes of Sinian period to Devonian period in Tarim Basin.
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    [2] 马世鹏等. 西昆仑山北坡的震旦系. 新疆地质, 1989, 7( 4): 50~ 54.
    [3] 白玉雷等. 新疆柯坪地区上震旦统— 奥陶系碳氧同位素地层标准剖面,塔里木盆地油气勘探论文集. 乌鲁木齐: 新疆科技卫生出版社, 1992, 73 ~ 76.
    [4] 张恺. 论塔里木盆地类型、演化特征及含油气远景评价. 石油与天然气地质, 1990, 11( 1): 1 ~ 7.
    [5] Epstein S and Mayeda T K. 1953, Variations of the O 18 /O 18 ra-tio in natural waters, Geochim. Cosmochim. Acta, 1973, 4: 80 ~85.
    [6] Redfield A C and Friedman I. Factors affecting the distributionof deuterium in the ocean. In: symposium on marine geo chem-istry, university of Rhode Is Land, Occasional Publication,1965, 3: 30 ~ 35.
    [7] PauLi Abell, stanley M. Awramik, Robert H. Osborne andsterling Tomellini. 1982, Plio-Pleistocene lacustrine stromato-lites from lake Turkana, Kenya. Morpholog y, stratig raphy andstable isotopes, sedimentary Geolog y, 1982, 32( 1): 110 ~ 114.
    [8] Vail, P E, Mitchun, R M and Thompson, S. Seismic stratig ra-phy and global changes of sea level, A APG, 1977, 26( 2): 235.
    [9] Van steenwinkel, M. Sequence stratigraphy from" spot" out-crops-example a carbonate-dominated setting: Dev onian-Car-boniferous transition, Dinant synclinorium( Belgium), Sedimen-tary Geology, 1990, 69( 1): 3 ~ 4.
    [10] Degens, E T and Epstein S. Relationship between,O 18 /O 18 ra-tio in coexisting Carbonates, Cherts and diatomites, AAPG,1962, 46( 4): 30 ~ 36.
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  • Received:  1996-08-10
  • Published:  1997-09-10

The Reconstruction and Origin of Sealevel Changes ofSinian Period to Dovinian Period in Tarim Basin

Abstract: Based on sequence stratigraphy work for the outcrops in Tarim Basin, The author sets up theSealevel changes curve of sinian period to Devonian period. Then the author studies the relationship be-tween oxygen isotope and sealevel changes and finds the oxygen isotope ratio' s increase and decredse in-dicating the sealevel' s down and up. The correctness of sealevel changes curve is tested and verified bythe result of oygen isotope. The ranges of sealevel changes are calculated. Finally the author elaboratesthe formation mechanism of sealevel changes of Sinian period to Devonian period in Tarim Basin.

Du Xiaodi, Wang Pujun, Kuang Lichun, Wang Dongpo. The Reconstruction and Origin of Sealevel Changes ofSinian Period to Dovinian Period in Tarim Basin[J]. Acta Sedimentologica Sinica, 1997, 15(3): 14-17.
Citation: Du Xiaodi, Wang Pujun, Kuang Lichun, Wang Dongpo. The Reconstruction and Origin of Sealevel Changes ofSinian Period to Dovinian Period in Tarim Basin[J]. Acta Sedimentologica Sinica, 1997, 15(3): 14-17.
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