青海柴达木盆地米海矿区富钾、富锂卤水勘探方法

IF 2.2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2025-04-23 DOI:10.1002/gj.5215
Minglu Zhang, Zihao Cui, Yanjun Zhao, Nan Wang, Fojun Yao, Qiang Wang, Shengzhong Hu
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引用次数: 0

摘要

深盐湖资源的勘探与开采对缓解钾锂资源短缺具有重要意义。然而,由于技术挑战和成本限制,大规模的工业提取尚未实现。以青海省凯达盆地米海矿区为研究对象,开展了深部富钾、富锂密闭盐水勘探开发研究。米海矿区深部承压盐水储量巨大,但由于其非均质性、出水量低、开采效率极低,未得到很好的利用。以往的研究表明,矿区高产井多位于断裂带内。因此,基于“断裂带卤水循环成钾”和“陡斜集水走廊卤水储存”理论模型,提出了一种高效的勘探技术,即在高质量卤水储层发育的区域内,以活动断裂带为重点靶区。本研究采用雷达遥感解译震前和震后形变强度来推断断裂带发育区域。结合氡气测量结果,证实在关键靶区内存在一条ne向活动断层。该带为沉积中心,卤水富集,K+和Li+共富集(均呈异常高浓度),具有发现富K-Li卤水的潜力。在勘探理论的指导下,验证钻井发现,大部分井眼的卤水K-Li浓度升高(约为邻近地区的两倍),且高产水流,表明勘探取得了重大成功。已发现高产富水区分布格局及勘探预测方法对米海矿区深部卤水开发具有重要意义,在凯达盆地具有较大的推广潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Exploration Methods for Potassium-Rich and Lithium-Rich Brine in the Mihai Mining Area, Qaidam Basin, Qinghai

Exploration Methods for Potassium-Rich and Lithium-Rich Brine in the Mihai Mining Area, Qaidam Basin, Qinghai

The exploration and extraction of deep salt lake resources are of great significance for alleviating potassium and lithium resource shortages. However, large-scale industrial extraction has not been achieved due to technical challenges and cost constraints. This study focuses on the Mihai Mining District in Qaida Basin, Qinghai Province, investigating the exploration and development of deep confined brine enriched with potassium and lithium. The Mihai Mining Area boasts vast reserves of deep confined brine, however, they are not well-utilised because of their heterogeneity, low water yields, and extremely low mining efficiency. Previous studies have revealed that the high-yield wells in mining areas are located within fault zones. Therefore, based on the theoretical models of ‘brine circulation and potassium formation in fault zones’ and ‘storage of brine in steeply inclined water-collecting corridors’, an efficient exploration technique is proposed, which focuses on identifying active fault zones within areas with well-developed high-quality brine reservoirs as key target areas. This study employed radar remote sensing interpretation of pre- and post-seismic deformation intensity to infer fault zone development areas. Integrated with radon gas measurements, the results confirm the presence of a NE-striking active fault within the key target zone. Functioning as the sedimentary centre, this zone exhibits highly concentrated brine with co-enrichment of K+ and Li+ (both elements showing anomalously high concentrations), indicating high potential for K-Li-rich brine discovery. Guided by the exploration theory, verification drilling revealed brine with elevated K-Li concentrations (approximately double those in adjacent areas) and high-yield water flows in most boreholes, demonstrating significant exploration success. The distribution pattern of the discovered high-yield, water-rich areas and the exploration prediction method are of great significance for the development of deep brine in the Mihai Mining Area and have considerable potential for promotion in the Qaida Basin.

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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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