中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Oxygen Isotope Clue to Migration of Dolomitizing Fluid as Exampled by the Changxing Formation Dolomite at Panlongdong, Northeastern Sichuan

文献类型:期刊论文

作者Zhao, Rui1; Wu, Yasheng1; Jiang, Hongxia1; Liu, Qingsong3
刊名JOURNAL OF EARTH SCIENCE
出版日期2017-04-01
卷号28期号:2页码:333-346
关键词Sichuan Basin Changxing Formation Dolomitization Oxygen Isotope Origin Migrating Direction
ISSN号1674-487X
文献子类Article
英文摘要The Upper Permian Changxing dolomite reservoirs serves as one of the most important gas and oil reservoirs in the NE Sichuan Basin. Determining the dolomitizing fluid's pathway is regarded as the key to solve the "dolomite problem" and further petroleum exploration. Outcrop samples from Upper Permian Changhsingian Panlongdong Section were studied using oxygen isotopic analysis, cathodoluminescence (CL) and major element analysis, in an attempt to determine the migration path way and properties of the dolomitizing fluid. Of the Changxing dolomite, the delta O-18 values ranged from -3.494 parts per thousand to -5.481 parts per thousand, which decreased from the top layer to the bottom in the section; the MgO contents varied from 9.24% to 21.43%, CaO contents from 28.65% to 39.87%, the CaO/MgO ratio from 1.40 to 4.31 and the MnO contents from 0.004% to 0.009 8%. The MgO contents showed a downwardly decreasing trend in the section, while the CaO/MgO showed an opposite rule. All of the dolomites looked dull or dark when they were exposed to the electron beam of the cathodoluminescence device. None of the fine-to medium grained dolomite showed a banded structure. Given that dolomitizing fluid's salinity decreased during the dolomitization process in its pathway, we concluded that the dolomitizing fluid migrated downwardly in Changxing Formation after excluding the possibility of deep burial or meteoric-marine mixing-water influences. As the dolomitizing fluid's pathway has always been difficult to be determined in highly dolomitized Formation, this study showed an important application of oxygen isotope values in resolving this problem.
WOS关键词CANADA SEDIMENTARY BASIN ; GEOCHEMICAL CHARACTERISTICS ; PLATFORM DOLOMITES ; FRESH-WATER ; HYDROTHERMAL DOLOMITE ; ORDOVICIAN CARBONATES ; FEIXIANGUAN FORMATION ; PRESQUILE BARRIER ; JIANGXI PROVINCE ; EASTERN SICHUAN
WOS研究方向Geology
语种英语
WOS记录号WOS:000398653100012
出版者CHINA UNIV GEOSCIENCES, BEIJING
资助机构National Natural Science Foundation of China(40472015 ; State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation at CDUT(PL200801) ; 40802001 ; 41372121) ; National Natural Science Foundation of China(40472015 ; State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation at CDUT(PL200801) ; 40802001 ; 41372121) ; National Natural Science Foundation of China(40472015 ; State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation at CDUT(PL200801) ; 40802001 ; 41372121) ; National Natural Science Foundation of China(40472015 ; State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation at CDUT(PL200801) ; 40802001 ; 41372121)
源URL[http://ir.iggcas.ac.cn/handle/132A11/52976]  
专题地质与地球物理研究所_中国科学院油气资源研究重点实验室
通讯作者Wu, Yasheng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714
Zhao, Rui,Wu, Yasheng,Jiang, Hongxia,et al. Oxygen Isotope Clue to Migration of Dolomitizing Fluid as Exampled by the Changxing Formation Dolomite at Panlongdong, Northeastern Sichuan[J]. JOURNAL OF EARTH SCIENCE,2017,28(2):333-346.
APA Zhao, Rui,Wu, Yasheng,Jiang, Hongxia,&Liu, Qingsong.(2017).Oxygen Isotope Clue to Migration of Dolomitizing Fluid as Exampled by the Changxing Formation Dolomite at Panlongdong, Northeastern Sichuan.JOURNAL OF EARTH SCIENCE,28(2),333-346.
MLA Zhao, Rui,et al."Oxygen Isotope Clue to Migration of Dolomitizing Fluid as Exampled by the Changxing Formation Dolomite at Panlongdong, Northeastern Sichuan".JOURNAL OF EARTH SCIENCE 28.2(2017):333-346.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。