Impact of fluorine-bearing hydrothermal fluid on deep burial carbonate reservoirs: A case study from the Tazhong area of Tarim Basin, northwest China
文献类型：期刊论文
| 作者 | Jia, Lianqi1; Cai, Chunfang2,3,4; Li, Kaikai5,6; Liu, Lijing1; Chen, Zhipeng7; Tan, Xianfeng8 |
| 刊名 | MARINE AND PETROLEUM GEOLOGY
 |
| 出版日期 | 2022-05-01 |
| 卷号 | 139页码:14 |
| 关键词 | Deep burial Carbonate reservoir Fluid inclusion Rare earth element and yttrium Tazhong area Tarim basin |
| ISSN号 | 0264-8172 |
| DOI | 10.1016/j.marpetgeo.2022.105579 |
| 英文摘要 | Deep burial carbonate reservoirs (>4000 m) have great potential of reserves for oil and gas exploration, although the matrix reservoirs generally become extremely heterogeneous and tight due to various diagenesis. Hydro thermal dissolution is supposed to be important for formation of high-quality deep burial carbonate reservoirs. However, few studies have focused on influence of minor fluorine-bearing fluid on carbonate reservoir quality. This study integrates petrography, geochemistry and fluid inclusion data to understand impact of fluorine bearing fluid on deep burial carbonate reservoirs. Mineralogy and mineral distribution suggest that fluorite and concomitant calcite are found in the Ordovician and Cambrian strata of the whole Tazhong area, especially in the vicinity of faults. Calcite associated with fluorite is probably derived from progressive mixture between formation water and fluorine-bearing hydrothermal fluid, which is supported by REY pattern of concomitant calcite, surrounding limestone and fluorite, and fluid inclusion microthermometric data of concomitant calcite and fluorite. Fluorine-bearing hydrothermal fluid was responsible for the concomitant C2 calcite of high Y/Ho ratio. Therefore, the superchondritic Y/Ho ratio of concomitant calcite can be probably used as proxy for identifying distribution of minor fluorine-bearing hydrothermal fluid. For thick fluorite bed, influx of fluorite rich fluid resulted in surrounding limestone dissolution and altered zones between fluorite and limestone. This process simultaneously improves porosity and permeability of high-energy sedimentary facies reservoirs. In contrast, the fluorine-rich hydrothermal fluid through the low-energy sedimentary facies mainly enhanced permeability of the tight carbonate reservoirs rather than porosity. For widespread tight reservoir of high-energy and low-energy sedimentary facies, even minor fluorite-bearing fluids still enhance permeability. The fluorine bearing hydrothermal fluid may influence carbonate reservoirs away from hydrothermal-altered zones. Significance of minor fluorine-bearing hydrothermal fluid for widespread tight carbonates has probably been underestimated for deep burial carbonate reservoir. |
| WOS关键词 | RARE-EARTH-ELEMENT ; MESOGENETIC DISSOLUTION ; ORDOVICIAN CARBONATES ; DOLOMITE RESERVOIRS ; POROSITY CREATION ; FE OXYHYDROXIDE ; VEIN SYSTEM ; GEOCHEMISTRY ; DOLOMITIZATION ; DIAGENESIS |
| 资助项目 | National Natural Science Foundation of China[41972143] ; National Natural Science Foundation of China[41502148] ; National Natural Science Foundation of China[41672143] ; National Natural Science Foundation of China[41730424] ; National Natural Science Foundation of China[42072127] ; National Natural Science Foundation of China[41502004] ; National Science and Technology Major Project of China on Petroleum Study[2017ZX05008003-040] ; [42072127and 41502004] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000780384700002 |
| 出版者 | ELSEVIER SCI LTD |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study ; National Science and Technology Major Project of China on Petroleum Study |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/105110]  |
| 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 | Jia, Lianqi; Cai, Chunfang |
| 作者单位 | 1.Northwest Univ, State Key Lab Continental Dynam & Dept Geol, Xian 710069, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 4.Yangtze Univ, Key Lab Oil & Gas Resources & Explorat Technol, Wuhan 430100, Peoples R China 5.China Univ Geosci Beijing, Sch Energy Resources, Beijing 100083, Peoples R China 6.Minist Educ, Key Lab Marine Reservoir Evolut & Hydrocarbon Enr, Beijing, Peoples R China 7.Xian Shiyou Univ, Sch Earth Sci & Engn, Xian 710065, Peoples R China 8.Chongqing Univ Sci & Technol, Coll Petr & Nat Gas Engn, Chongqing 401331, Peoples R China |
| 推荐引用方式 GB/T 7714 | Jia, Lianqi,Cai, Chunfang,Li, Kaikai,et al. Impact of fluorine-bearing hydrothermal fluid on deep burial carbonate reservoirs: A case study from the Tazhong area of Tarim Basin, northwest China[J]. MARINE AND PETROLEUM GEOLOGY,2022,139:14. |
| APA | Jia, Lianqi,Cai, Chunfang,Li, Kaikai,Liu, Lijing,Chen, Zhipeng,&Tan, Xianfeng.(2022).Impact of fluorine-bearing hydrothermal fluid on deep burial carbonate reservoirs: A case study from the Tazhong area of Tarim Basin, northwest China.MARINE AND PETROLEUM GEOLOGY,139,14. |
| MLA | Jia, Lianqi,et al."Impact of fluorine-bearing hydrothermal fluid on deep burial carbonate reservoirs: A case study from the Tazhong area of Tarim Basin, northwest China".MARINE AND PETROLEUM GEOLOGY 139(2022):14. |
入库方式： OAI收割
来源：地质与地球物理研究所
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