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WANG Xing tao, ZHANG Qing shi, ZHANG Ji, ZHOU Shu xin, LI Jing wei. Character Study and Analysis of Dolomite of Mesozoic in Qingzang Plateau[J]. Acta Sedimentologica Sinica, 2000, 18(4): 555-559.
Citation: WANG Xing tao, ZHANG Qing shi, ZHANG Ji, ZHOU Shu xin, LI Jing wei. Character Study and Analysis of Dolomite of Mesozoic in Qingzang Plateau[J]. Acta Sedimentologica Sinica, 2000, 18(4): 555-559.

Character Study and Analysis of Dolomite of Mesozoic in Qingzang Plateau

  • Received Date: 1999-08-31
  • Rev Recd Date: 1999-12-27
  • Publish Date: 2000-08-10
  • After dolomites of Qiangtang Basin and Cuoqin Basin in Qingzang Plateau are observed and described in the field, vertical and horizontal distribution rules of dolomite in the study area are reduced. Applying structure index, cathode shining index and oxygen isotope index, genesis of dolomite are effectively judged by use of systematically indoor analysis and laboratory test method. Then it is concluded that dolomites of the study area are all produced by metasomatism or dolomitation, not originally. According to size and shape of crystals and inner structure of dolomites, dolomiting phase are divided into three phases: quasi-contemporaneous phase, diagenesis and catagenesis. Features of each phase are introduced. It is found that dolomites formed in diagenesis can be a good reservoir rock.Through selecting typical sections, two kinds of genetic models of dolomite in the study area are put forward, i.e. capillary concentration model and mixed water model.
  • [1] Longrman N W. Carbonate diagenetic textures from near surface diagenetic environment[J]. AAPG Bull. 1980,64:461~487
    [2] 冯增昭等.中国沉积学[M].北京:石油工业出版社,1994.10.212~224
    [3] Degens E T, Epstein S. Oxygen and carbon isotope ratios in coexisting calcites and dolomites from recent and ancient sediments[J]. Geochim. Cosmochim. Acta 1964,28: 23~ 44
    [4] 冯增昭.华北地台早古生代岩相古地理研究[M].北京:地质出版社,1990.95~113
    [5] 弗里德曼G M,桑德斯J E白云岩的成因及产状[M].冯增昭译.第一版.北京:石油工业出版社,1978.1~39
    [6] Hsu K J, Siegenthaler C. Preliminary experiments on hydrodymmic movement induced by evaporation and their bearing on the dolomite problem[J]. Sedimentology, 1969,1~2:11 ~25
    [7] Bathurst R G C. Carbonate sediments and their diagenesis, Developments in sedimentology[M]. Els. Publ. Com. 1971,12:1~ 7
    [8] 福克RL,兰德LS.控制白云石结晶的两个因素:Mg/Ca比值和盐度[A]王尧译.国外地质.1977.10:105~136
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  • Received:  1999-08-31
  • Revised:  1999-12-27
  • Published:  2000-08-10

Character Study and Analysis of Dolomite of Mesozoic in Qingzang Plateau

Abstract: After dolomites of Qiangtang Basin and Cuoqin Basin in Qingzang Plateau are observed and described in the field, vertical and horizontal distribution rules of dolomite in the study area are reduced. Applying structure index, cathode shining index and oxygen isotope index, genesis of dolomite are effectively judged by use of systematically indoor analysis and laboratory test method. Then it is concluded that dolomites of the study area are all produced by metasomatism or dolomitation, not originally. According to size and shape of crystals and inner structure of dolomites, dolomiting phase are divided into three phases: quasi-contemporaneous phase, diagenesis and catagenesis. Features of each phase are introduced. It is found that dolomites formed in diagenesis can be a good reservoir rock.Through selecting typical sections, two kinds of genetic models of dolomite in the study area are put forward, i.e. capillary concentration model and mixed water model.

WANG Xing tao, ZHANG Qing shi, ZHANG Ji, ZHOU Shu xin, LI Jing wei. Character Study and Analysis of Dolomite of Mesozoic in Qingzang Plateau[J]. Acta Sedimentologica Sinica, 2000, 18(4): 555-559.
Citation: WANG Xing tao, ZHANG Qing shi, ZHANG Ji, ZHOU Shu xin, LI Jing wei. Character Study and Analysis of Dolomite of Mesozoic in Qingzang Plateau[J]. Acta Sedimentologica Sinica, 2000, 18(4): 555-559.
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