Source and Formation of Boron Deposits in Mahai Basin on the Northern Qinghai-Tibet Plateau: Clues from Hydrochemistry and Boron Isotopes

IF 1.7 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Honglu Xiang, Qishun Fan, Qingkuan Li, Yongsheng Du, Guang Han, Jiubo Liu, Hongkui Bai
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Abstract

There are typical salt lake-type borate deposits in the northern Qaidam Basin, which are mainly distributed in Da Qaidam Lake (DQL), Xiao Qaidam Lake, and Mahai Basin (MHB). DQL has deposited famous solid borates and enriched a large number of brine boron deposits. It is the earliest industrial production base in China. Nanbaxian (NBX) to the west of DQL is a unique area where solid borates are deposited in MHB. Although there are three salt lakes in the MHB, borate deposits were only deposited in the salt pits of NBX, and the formation process of these borate deposits remains to be clarified. In this study, the major elements, boron contents, and d11B values in the water and sediments of NBX were investigated in conjunction with the B-Na-Mg equivalence diagrams and relevant data from other salt lakes to elucidate the source of boron in MHB and the depositional conditions of borate minerals in NBX. The results are as follows: (1) The source of boron in NBX differs from that in three salt lakes in MHB. The source in NBX is mainly constrained by the weathering and fluid-rock (Boron-bearing ultra-high pressure metamorphic belt) interaction, while that in Dezongmahai and Niulangzhinv–Balunmahai lakes are primarily controlled by river water and anticlinal brine, respectively. (2) The high boron content (0.28 to 41.38 mg/L) and low d11B values (- 34.71‰ to - 6.14‰) of the water-soluble phase of sediments in NBX are consistent with geochemical characteristics (d11B: - 23.67‰ to - 3.0‰) of borates in DQL, demonstrating that the re-dissolution of borate deposits in NBX. (3) Deposition of borate minerals in the MHB requires ionic equivalents of Mg, Na, and B to 0.02 to 0.4, 0.25 to 0.75, and 0.2 to 0.7, respectively. Additionally, the brine hydrochemistry in which the borate are deposited must be of the carbonate or sulfate type, and the brine water should be greater than 8 in pH and 400 mg/L in boron content. This study provides a theoretical basis for exploring and exploiting salt lake-type borate deposits.

Abstract Image

青藏高原北部马海盆地硼矿床的来源与形成:水化学和硼同位素提供的线索
柴达木盆地北部有典型的盐湖型硼酸盐矿床,主要分布在大柴达木湖(DQL)、小柴达木湖和马海盆地(MHB)。大柴旦湖沉积了著名的固体硼酸盐,并富集了大量卤水硼矿床。它是中国最早的工业生产基地。大庆西部的南八仙(NBX)是 MHB 中沉积固体硼酸盐的独特区域。虽然马鬃山坝有三个盐湖,但硼酸盐矿床只沉积在南八仙的盐坑中,这些硼酸盐矿床的形成过程仍有待澄清。本研究结合B-Na-Mg当量图和其他盐湖的相关数据,对NBX水体和沉积物中的主要元素、硼含量和d11B值进行了研究,以阐明MHB中硼的来源和NBX中硼酸盐矿物的沉积条件。研究结果如下(1)NBX 的硼源与 MHB 三个盐湖的硼源不同。NBX的硼源主要受风化作用和流体-岩石(含硼超高压变质带)相互作用的制约,而德宗玛海和牛郎金佛-巴伦玛海湖泊的硼源分别主要受河水和反斜面卤水的控制。(2)NBX沉积物水溶相硼含量高(0.28~41.38 mg/L),d11B值低(-34.71‰~-6.14‰),与DQL中硼酸盐的地球化学特征(d11B:-23.67‰~-3.0‰)一致,表明NBX中硼酸盐沉积的再溶解作用。(3) 在MHB中沉积硼酸盐矿物需要镁、纳和硼的离子当量分别为0.02至0.4、0.25至0.75和0.2至0.7。此外,沉积硼酸盐的盐水水化学类型必须是碳酸盐或硫酸盐类型,盐水的 pH 值应大于 8,硼含量应大于 400 毫克/升。这项研究为勘探和开采盐湖型硼酸盐矿床提供了理论依据。
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来源期刊
Aquatic Geochemistry
Aquatic Geochemistry 地学-地球化学与地球物理
CiteScore
4.30
自引率
0.00%
发文量
6
审稿时长
1 months
期刊介绍: We publish original studies relating to the geochemistry of natural waters and their interactions with rocks and minerals under near Earth-surface conditions. Coverage includes theoretical, experimental, and modeling papers dealing with this subject area, as well as papers presenting observations of natural systems that stress major processes. The journal also presents `letter''-type papers for rapid publication and a limited number of review-type papers on topics of particularly broad interest or current major controversy.
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