引用本文:曾胜强, 陈文彬, 冯兴雷.羌塘盆地热觉茶卡-藏夏河地区泉水水化学特征及其地质意义[J].沉积与特提斯地质,2021,41(4):536-543.[点击复制]
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羌塘盆地热觉茶卡-藏夏河地区泉水水化学特征及其地质意义
曾胜强1,陈文彬1,2,冯兴雷1,2
0
(1. 中国地质调查局成都地质调查中心, 四川 成都 610081;
2. 自然资源部沉积盆地与油气资源重点实验室, 四川 成都 610081)
摘要:
泉水的水化学特征可以反映氧化-还原环境和水动力条件,近年来被广泛地用于石油、天然气以及天然气水合物的找矿工作中。本文对羌塘盆地热觉茶卡—藏夏河地区37处泉水和13件地表水进行了水化学特征、水溶性烃类气体特征和水中氢氧同位素特征分析,结果表明,羌塘盆地热觉茶卡—藏夏河地区的水型主要为Na2SO4型和MgCl2型,其次为NaHCO3型和CaCl2型。矿化度普遍较高,说明该区具有较好的保存条件。铵根离子的平均含量为0.895μg/g,在藏夏河地区高达7.381μg/g,表明在藏夏河东部地区有机质相对较为丰富,这与区域上发育的富有机质页岩结果一致。氢氧同位素结果显示,该区水体的氢氧同位素落在了大气降水线附近,表明水体的来源主要受大气降水的补给。另外,采集的9个泉水样品中均检测出一定含量的水溶甲烷,在白云湖地区的甲烷含量相对较高,显示出较好的油气潜力。综合研究表明,藏夏河东和白云湖地区具有良好的油气烃源岩条件,保存条件较好,显示出良好的油气和天然气水合物资源前景。
关键词:  羌塘盆地  泉水  水化学特征  氢氧同位素
DOI:10.19826/j.cnki.1009-3850.2021.08001
附件
投稿时间:2020-12-23修订日期:2021-04-15
基金项目:中国地质调查局调查项目(编号:GZH201400301、DD20190116)资助的成果
Chemical characteristics of fountains in Rejuechaka-Zangxiahe area of the Qiangtang Basin and their geological implications
ZENG Shengqiang1, CHEN Wenbin1,2, FENG Xinglei1,2
(1. Chengdu Center, China Geological Survey, Chengdu 610081, China;
2. Key Laboratory of Sedimentary Basin and Oil and Gas Resources, Ministry of Natural Resources, Chengdu 610081, China)
Abstract:
Recent years, the chemical characteristics of fountains, which can reflect the redox environment and hydrodynamic conditions, have been widely used in prospecting for petroleum, natural gas and natural gas hydrate. In this paper, 37 samples of fountains and 13 samples of surface water have been collected from Rejuechaka-Zangxiahe areas of the Qiangtang Basin to analyze their chemical compositions, isotopic compositions of hydrogen and oxygen, and contents of aqueous hydrocarbon gases. The results show that the water types are mainly Na2SO4 type and MgCl2 type, with subordinate NaHCO3 type and CaCl2 type. The general high mineralized degrees of the fountains reveal a good preservation condition in the area. The average content of the ammonium ion is 0.895 μg/g. In Zangxiahe area, the ammonium ion content is up to 7.381μg/g, which is consistent with the widespread organic-rich shale in the area, indicating the relatively high organic matter content. The isotopic results of hydrogen and oxygen show that the H and O isotopes of the water are near the precipitation line, indicating that the fountains originate from meteoric water. In addition, a certain content of aqueous methane has been detected in nine fountains, and the content is relatively high in Baiyun Lake area, showing a good hydrocarbon potential. The comprehensive study reveals that the Zangxiahe and Baiyun Lake areas in the Qiangtang Basin have good source rocks and good preservation conditions, showing a good prospect for oil, gas and gas hydrate resources.
Key words:  Qiangtang Basin  Fountains  hydrochemistry  hydrogen and oxygen isotopes

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