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《Journal of Jilin University(Earth Science Edition)》 2008-02
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Dolomitization Characteristics of Carbonate Rock in Xisha Islands and Its Formation:A Case Study of Well Xichen-1

WEI Xi1,2,JIA Cheng-zao1,MENG Wei-gong21.Postdoctoral Program of RIPED,PetroChina,Beijing 100083,China2.Postdoctoral Workstation of Liaohe Oilfield Subcompany,PetroChina,Panjin,Liaoning 124010,China  
Carbonate rock strata in well Xichen-1,Xisha islands consist of 3 layers of dolostone and 4 layers of limestone.In dolostone layers,the micritic dolomite,containing 91.1%-100% of dolomite,can distribute in all kinds of contents such as framework grains and inter-grain fillings.Isotopes of the dolomite are as follows,δ13C varies from 0.80‰ to 3.16‰,averaging 2.24‰;δ18O varies from 0.56‰ to 5.23‰,averaging 2.56‰.These characteristics reflect that dolomitization occurred in synsedimentary heavy brine environment when paleosalinity is 36.88% and paleotemperature is 1.07℃.The limestone layers with dominant calcsparite contain dolomite in general less than 25%,in which dolomite are concentrated in pore or fissure fillings and absent in framework grains.The fluid inclusion homogenization temperature measured in domolite range 102.5-296℃ with an average of 156.3℃;the salinity is 0.55%-6.25%,averaging 3.75%;the density is 0.95-0.99 g/cm3,averaging 0.97 g/cm3;the pressure is 20.65-42.65 MPa,averaging 33.65 MPa.These characteristics reflect that dolomitization may be in connection with post diagenetic hydrothermal event.
【Fund】: 国家自然科学基金重点项目(40234048);; 中国地质大学(北京)优秀博士论文扶持奖励基金([2005]115号)
【CateGory Index】: P588.245
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