Origin and migration of brines from Paleozoic strata in Central Tarim, China: constraints from Sr-87/Sr-86, delta D, delta O-18 and water chemistry | |
Cai, CF; Franks, SG; Aagaard, P | |
刊名 | APPLIED GEOCHEMISTRY |
2001-07-01 | |
卷号 | 16期号:9-10页码:1269-1284 |
ISSN号 | 0883-2927 |
文献子类 | Article |
英文摘要 | Chemistry of major and minor elements, Sr-87/Sr-86, deltaD, and delta O-18 of oilfield waters, and Sr-87/Sr-86 of whole rock were measured from Paleozoic strata in the Central Tarim basin, NW China. The aim is to elucidate the origin and migration of formation water and its relation to petroleum migration. High salinity oilfield waters in Carboniferous, Silurian and Ordovician reservoirs have maintained the same Na/Cl ratio as seawater, indicative of subaerially evaporated seawater. Two possible sources of evaporitic water are Carboniferous (C-u) and Cambrian, both of which contain evaporitic sediments. Geographic and stratigraphic trends in water chemistry suggest that most of the high salinity water is from the Cambrian. Strontium, H and O isotopes as well as ion chemistry indicate at least 3 end member waters in the basin. High-salinity Cambrian evaporitic water was expelled upward into Ordovician, Silurian and Carboniferous reservoirs along faults and fractures during compaction and burial. Meteoric water has likely invaded the section throughout its history as uplift created subaerial unconformities. Meteoric water certainly infiltrated Silurian and older strata during development of the C-III unconformity and again in recent times. Modern meteoric water enters Carboniferous strata from the west and flows eastward, mixing with the high salinity Cambrian water and to a lesser degree with paleometeoric water. The third rad member is highly radiogenic, shale-derived water which has migrated eastward from the Awati Depression to the weal. Enrichment of Ca and Sr and depletion of K, Mg, and SO4 relative to the seawater evaporation trajectory suggest waters were affected by albitization of feldspars, dolomitization, illitization of smectite, and SO4 reduction. The mixing of meteoric water occurred subsequently to seawater evaporation, main water-rock interactions, and brine migration. The direction of brine migration is consistent with that of petroleum migration, suggesting water and petroleum have followed the same migration pathways. (C) 2001 Elsevier Science Ltd. All rights reserved. |
WOS关键词 | SALINE FORMATION WATERS ; SEDIMENTARY BASIN ; ISOTOPE GEOCHEMISTRY ; MICHIGAN BASIN ; USA ; STRONTIUM ; EVOLUTION ; HISTORY |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000168492800022 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/77233] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Cai, CF |
作者单位 | 1.CAS, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Rock Fluid Syst Inc, Plano, TX 75023 USA 3.Univ Oslo, Dept Geol, N-0316 Oslo, Norway |
推荐引用方式 GB/T 7714 | Cai, CF,Franks, SG,Aagaard, P. Origin and migration of brines from Paleozoic strata in Central Tarim, China: constraints from Sr-87/Sr-86, delta D, delta O-18 and water chemistry[J]. APPLIED GEOCHEMISTRY,2001,16(9-10):1269-1284. |
APA | Cai, CF,Franks, SG,&Aagaard, P.(2001).Origin and migration of brines from Paleozoic strata in Central Tarim, China: constraints from Sr-87/Sr-86, delta D, delta O-18 and water chemistry.APPLIED GEOCHEMISTRY,16(9-10),1269-1284. |
MLA | Cai, CF,et al."Origin and migration of brines from Paleozoic strata in Central Tarim, China: constraints from Sr-87/Sr-86, delta D, delta O-18 and water chemistry".APPLIED GEOCHEMISTRY 16.9-10(2001):1269-1284. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
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。
修改评论