Complex accumulation and leakage of YC21-1 gas bearing structure in Yanan sag, Qiongdongnan basin, South China Sea
文献类型：期刊论文
| 作者 | Su, Ao1; Chen, Honghan1; He, Cong2,3; Lei, Mingzhu4; Liu, Yanhua1 |
| 刊名 | MARINE AND PETROLEUM GEOLOGY
 |
| 出版日期 | 2017-12-01 |
| 卷号 | 88页码:798-813 |
| 关键词 | Overpressure Fluid Inclusions Water-soluble Gas Accumulation Leakage Qiongdongnan Basin |
| ISSN号 | 0264-8172 |
| DOI | 10.1016/j.marpetgeo.2017.09.020 |
| 文献子类 | Article |
| 英文摘要 | YC21-1 is a gas-bearing structure found within the Yanan sag in the Qiongdongnan Basin, South China Sea. While the structure bears many geological similarities to the nearby YC13-1 gas field, it nevertheless does not contain commercially viable gas volumes. The main reservoirs of the YC21-1 structure contain high overpressures, which is greatly different from those of the YC13-1 structure. The pressure coefficients from drillstem tests, wireline formation tests and mud weights are above 2.1. Based on well-log analysis, illite content and vitrinite reflectance data of mudstones in well YC21-1-2, combining with tectonic and sedimentation characteristics, the timing and causes of overpressure generation are here interpreted. The results indicate the existence of two overpressure segments in the YC21-1 structure. The first overpressure segment resides mainly within the lower and the middle intervals of the Yinggehai Formation, and is interpreted to have been mainly caused by clay diagenesis, while disequilibrium compaction and hydrocarbon generation may also have contributed to overpressure generation. The second overpressure segment comprising the Sanya Formation (Pressure transition zone) and the Lingshui and Yacheng Formations (Hard overpressure zone) is interpreted to owe its presence to kerogen-to-gas cracking. According to petrography, homogenization temperature and salinity of fluid inclusions, two stages of oil-gas charge occurred within the main reservoirs. On the basis of overpressure causes and oil-gas charge history, combining with restored tectonic evolution and fluid inclusion characteristics, a complex accumulation and leakage process in the YC21-1 gas bearing structure has been interpreted. Collective evidence suggests that the first oil charge occurred in the Middle Miocene (circa 16.3-11.2 Ma). Small amount of oil generation and absence of caprocks led to the failure of oil accumulation. Rapid subsidence in the Pliocene and Quaternary gave rise to a sharp increase in geo-temperature over a short period of time, leading to prolific gas-generation through pyrolysis and, consequently, overpressure within the main reservoirs (the second overpressure segment). During this period, the second gas charge occurred in the Pliocene and Quaternary (circa 4.5-0.4 Ma). The natural gas migrated in several phases, consisting of free and water soluble phases in a high-pressure environment. Large amounts of free gas are considered to have been consumed due to dissolution within formation water in highly pressured conditions. Water soluble gas could not accumulate in high point of structure. When the pore-fluid pressures in main reservoirs reached the fracture pressure of formation, free gas could leak via opened fractures within cracked caprocks. A repeated fracturing of caprocks may have consumed natural gas stored in formation water and have made water-soluble gas unsaturated. Therefore, the two factors including caprocks fracturing and dissolution of formation water are interpreted to be mainly responsible for the failure of natural gas accumulation in the YC21-1 structure. (C) 2017 Elsevier Ltd. All rights reserved. |
| WOS关键词 | HYDROCARBON FLUID INCLUSIONS ; PORE-PRESSURE PREDICTION ; PEARL RIVER MOUTH ; NATURAL GASES ; OVERPRESSURE ; PETROLEUM ; OIL ; ORIGIN ; FIELD ; GEOCHEMISTRY |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000416186000053 |
| 出版者 | ELSEVIER SCI LTD |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/82050]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Chen, Honghan; He, Cong |
| 作者单位 | 1.China Univ Geosci, Educ Minist, Key Lab Tecton & Petr Resource, Wuhan 430074, Hubei, Peoples R China 2.Chinese Acad Sci, Key Lab Petr Resources Gansu Prov, Lanzhou 730000, Gansu, Peoples R China 3.Chinese Acad Sci, Key Lab Petr Resources Res, Lanzhou 730000, Gansu, Peoples R China 4.CNOOC China Ltd, Zhanjiang Branch, Zhanjiang 524057, Guangdong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Su, Ao,Chen, Honghan,He, Cong,et al. Complex accumulation and leakage of YC21-1 gas bearing structure in Yanan sag, Qiongdongnan basin, South China Sea[J]. MARINE AND PETROLEUM GEOLOGY,2017,88:798-813. |
| APA | Su, Ao,Chen, Honghan,He, Cong,Lei, Mingzhu,&Liu, Yanhua.(2017).Complex accumulation and leakage of YC21-1 gas bearing structure in Yanan sag, Qiongdongnan basin, South China Sea.MARINE AND PETROLEUM GEOLOGY,88,798-813. |
| MLA | Su, Ao,et al."Complex accumulation and leakage of YC21-1 gas bearing structure in Yanan sag, Qiongdongnan basin, South China Sea".MARINE AND PETROLEUM GEOLOGY 88(2017):798-813. |
入库方式： OAI收割
来源：地质与地球物理研究所
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