Burial hydrothermal dissolution fluid activity and its transforming effect on the reservoirs in Ordovician in Central Tarim
文献类型：期刊论文
| 作者 | Yang HaiJun1; Li KaiKai2; Pan WenQing1; Xiao ZhongYao1; Cai ChunFang2 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2012-03-01 |
| 卷号 | 28期号:3页码:783-792 |
| 关键词 | Thermochemical sulfate reduction (TSR) Strike-slip fault Hydrothermal Karst Central Tarim |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | Detailed studies of homogenization temperatures of fluid inclusions, distribution and geochemistry characters of hydrothermal minerals provide insights into chemical, distribution and flowing characteristics of hydrothermal/burial dissolution fluid in Central Tarim. Result shows that the activity of the fluid was prevalent in Ordovician strata, which significantly improved the carbonate reservoirs associated and broaded petroleum exploration prospect. In addition, the aforementioned fluid was inclined to inject into the reservoirs at NE-SW trending strike-slip fault zones, i. e., TZ45 and TZ82-16 well areas. The current study further claims that the prior karst cavity systems would have been destroyed by intensely compaction during the burial process. However, the surviving cavity systems may have also been preferential channels for the flow of hydrothermal/burial dissolution fluid, which would have expanded pore spaces. Therefore, great attention shall be paid to the activities of tensional faults under the compression set such as strike-slip fault zones, as well as their conduction effect of hot fluid. By interpolation, it should be attached importance to the superimposition effect of multiple stages of distinctive fluids on the reservoirs, which may be the potential exploration targets. |
| WOS关键词 | THERMOCHEMICAL SULFATE REDUCTION ; CARBONATE RESERVOIR ; BASIN ; CHINA ; DOLOMITE ; FIELD ; AREA |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000303640700007 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/84616]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Yang HaiJun |
| 作者单位 | 1.PetroChina, Tarim Oilfield Co, Res Inst Petr Explorat & Dev, Korla 841000, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yang HaiJun,Li KaiKai,Pan WenQing,et al. Burial hydrothermal dissolution fluid activity and its transforming effect on the reservoirs in Ordovician in Central Tarim[J]. ACTA PETROLOGICA SINICA,2012,28(3):783-792. |
| APA | Yang HaiJun,Li KaiKai,Pan WenQing,Xiao ZhongYao,&Cai ChunFang.(2012).Burial hydrothermal dissolution fluid activity and its transforming effect on the reservoirs in Ordovician in Central Tarim.ACTA PETROLOGICA SINICA,28(3),783-792. |
| MLA | Yang HaiJun,et al."Burial hydrothermal dissolution fluid activity and its transforming effect on the reservoirs in Ordovician in Central Tarim".ACTA PETROLOGICA SINICA 28.3(2012):783-792. |
入库方式： OAI收割
来源：地质与地球物理研究所
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