Pore Structure Characterization of Clay Minerals in the Lower Karamay Formation Conglomerate Reservoir in the Junggar Basin and its Impact on Hydrocarbon Storage and Seepage
文献类型:期刊论文
作者 | Abitkazy, Taskyn2,3; Du SH(杜书恒)1; Xu, Feng2; Shi, Yongmin3 |
刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION |
出版日期 | 2021-04-01 |
卷号 | 95期号:2页码:558-569 |
ISSN号 | 1000-9515 |
关键词 | oil conglomerate clay minerals micro-nano pore reservoir characterization Triassic Xinjiang |
DOI | 10.1111/1755-6724.13887 |
通讯作者 | Du, Shuheng(dushuheng@imech.ac.cn) |
英文摘要 | The micro-nano pore structure of conglomerate in the Lower Karamay Formation of the Xinjiang Oilfield, Junggar Basin, northern China is characterized to predict its impact on fluid reserves and seepage. Authigenic clay minerals are mainly kaolinite (67%), followed by an illite/smectite mixed layer (18%), illite (10%), and chlorite (5%). For kaolinite, pore throats between 0-200 nm are dominant, accounting for 90% of the total pore throats. For illite/smectite mixed layer, pore throats also between 0-200 nm account for nearly 80%, while pore throats between 200-500 nm only account for 15%. For illite, pore throats below 100 nm account for about 80%, while pore throats in the range of 100-500 nm only account for 20%. For chlorite, most throats are below 200 nm. The pore roundness of illite is the highest, while the pore roundness of chlorite is relatively lower. The lower limits of the dynamic and static pore throat radii are 42.128 nm and 72.42 nm, respectively. The theoretical contribution rates of the illite/smectite mixed layer, kaolinite, illite and chlorite to storage/seepage are 60%/45.86%, 52.72%/38.18%, 37.07%/28.78% and 32.97%/26.3%, respectively. Therefore, the contribution rates of clay minerals in the study area are as follows: illite/smectite mixed layer, kaolinite, illite and chlorite. |
分类号 | Q3 |
WOS关键词 | MOLECULAR-DYNAMICS ; QUALITY EVOLUTION ; WATER SENSITIVITY ; CARDIUM FORMATION ; FORMATION DAMAGE ; SANDSTONES ; DIAGENESIS ; SHALE ; POROSITY ; THROAT |
资助项目 | PetroChina Innovation Foundation[2019D-5007-0214] ; National Mega Project of Oil and Gas[2017ZX05013005-009] |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000653317300016 |
资助机构 | PetroChina Innovation Foundation ; National Mega Project of Oil and Gas |
其他责任者 | Du, Shuheng |
源URL | [http://dspace.imech.ac.cn/handle/311007/86910] |
专题 | 力学研究所_非线性力学国家重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Mech, State Key Lab Nonlinear Mech, Beijing 100190, Peoples R China 2.CNPC, Res Inst Petr Explorat & Dev Co Ltd, Beijing 100083, Peoples R China; 3.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China; |
推荐引用方式 GB/T 7714 | Abitkazy, Taskyn,Du SH,Xu, Feng,et al. Pore Structure Characterization of Clay Minerals in the Lower Karamay Formation Conglomerate Reservoir in the Junggar Basin and its Impact on Hydrocarbon Storage and Seepage[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2021,95(2):558-569. |
APA | Abitkazy, Taskyn,杜书恒,Xu, Feng,&Shi, Yongmin.(2021).Pore Structure Characterization of Clay Minerals in the Lower Karamay Formation Conglomerate Reservoir in the Junggar Basin and its Impact on Hydrocarbon Storage and Seepage.ACTA GEOLOGICA SINICA-ENGLISH EDITION,95(2),558-569. |
MLA | Abitkazy, Taskyn,et al."Pore Structure Characterization of Clay Minerals in the Lower Karamay Formation Conglomerate Reservoir in the Junggar Basin and its Impact on Hydrocarbon Storage and Seepage".ACTA GEOLOGICA SINICA-ENGLISH EDITION 95.2(2021):558-569. |
入库方式: OAI收割
来源:力学研究所
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