Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1306/0504171612517157 |
Evolution of formation waters in the Permian Basin, United States: Late Permian evaporated seawater to Neogene meteoric water | |
Saller, Arthur H.1,2; Stueber, Alan M.3,4,5 | |
2018-03-01 | |
发表期刊 | AAPG BULLETIN |
ISSN | 0149-1423 |
EISSN | 1558-9153 |
出版年 | 2018 |
卷号 | 102期号:3页码:401-428 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | Understanding subsurface waters is important for hydrocarbon exploration and development. Waters from the Permian Basin were collected and analyzed for stable isotopes, ionic concentrations, and strontium isotopes to determine their origin. Three main geochemical groups of waters are present. Group 1 has high delta O-18 and delta D values with high total dissolved solids (TDS; 100-240 g/L), including high concentrations of Na+, Cl-, and Br-. Group 1 waters contain distinctly less sodium (Na+) thanchlorine (Cl-) on a molar basis, similar to modern seawater. Group 2 and 3 waters have low delta O-18 and dD values. Group 2 waters have relatively low TDS (4-75 g/L). Group 3 waters have high TDS (170-225 g/L), Na+ and Cl- in approximately equal molar amounts, and low Br- concentrations. Group 1 waters are interpreted as forming from highly evaporated seawater during precipitation of uppermost Permian salts. Because of their high density, those waters displaced preexisting formation waters throughout the Permian Basin during the latest Permian. Waters in groups 2 and 3 came mainly from precipitation in the mountains of southeast New Mexico. Those mountains formed during Neogene tectonic uplifts. Group 3 waters acquired their Na+ and Cl- by dissolution of upper Permian salt. Many group 2 and 3 waters acquired their Ca2+ and SO42- by dissolution of Permian anhydrite or gypsum. Some waters contain a mixture of these groups. Understanding the origin of subsurface waters helps predict subsurface salinity, aquifer drive, sulfate reduction, chemical reactions during water injection, and chemistry of diagenetic waters. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000430928900003 |
WOS关键词 | CANADA SEDIMENTARY BASIN ; SOUTHEASTERN NEW-MEXICO ; ISOLATION PILOT-PLANT ; ALBERTA BASIN ; WEST TEXAS ; SEA-WATER ; PALO-DURO ; ORIGIN ; USA ; GEOCHEMISTRY |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/24420 |
专题 | 地球科学 |
作者单位 | 1.Cobalt Int Energy, 920 Mem City Way,Suite 100, Houston, TX 77024 USA; 2.4827 Kirkwall Dr, Sugar Land, TX 77479 USA; 3.Miami Univ, Oxford, OH 45056 USA; 4.Louisiana State Univ, Baton Rouge, LA 70803 USA; 5.Southern Illinois Univ, Edwardsville, IL USA |
推荐引用方式 GB/T 7714 | Saller, Arthur H.,Stueber, Alan M.. Evolution of formation waters in the Permian Basin, United States: Late Permian evaporated seawater to Neogene meteoric water[J]. AAPG BULLETIN,2018,102(3):401-428. |
APA | Saller, Arthur H.,&Stueber, Alan M..(2018).Evolution of formation waters in the Permian Basin, United States: Late Permian evaporated seawater to Neogene meteoric water.AAPG BULLETIN,102(3),401-428. |
MLA | Saller, Arthur H.,et al."Evolution of formation waters in the Permian Basin, United States: Late Permian evaporated seawater to Neogene meteoric water".AAPG BULLETIN 102.3(2018):401-428. |
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