| 西藏扎布耶超大型锂、硼矿床地质背景及其形成演化 |
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| 引用本文： | 刘喜方,郑绵平.西藏扎布耶超大型锂、硼矿床地质背景及其形成演化[J].化工矿产地质,1999,21(2):65-68. |
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| 作者姓名： | 刘喜方 郑绵平 |
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| 作者单位： | [1]中国地质大学 [2]中国地质科学院矿床地质研究所 |
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| 基金项目： | 国家自然科学基金!49672115 |
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| 摘 要： | 扎布耶盐湖位于青藏高原腹地，是一个现代盐湖矿床。通过对扎布耶湖区的各时代地层、岩浆作用，变质作用及构造特征的调查，并根据湖泊沉积特征的综合分析研究，得知自更新世晚期扎布耶及周边泛河湖区以来，呈现湖泊退缩、咸化的演化趋势。Li、B等成矿元素可能源于底部岩石、深部流体及湖中及湖周的泉华及泉水。
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| 关 键 词： | 扎布耶盐湖 地层 岩浆活动 变质作用 构造 形成演化 |
GEOLOGICAL SETTING AND MINERALIZING EVOLUTION OF SUPER LARGE Li, B DEPOSIT, ZABUYE, TIBET |
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| Liu XiFang.GEOLOGICAL SETTING AND MINERALIZING EVOLUTION OF SUPER LARGE Li, B DEPOSIT, ZABUYE, TIBET[J].Geology of Chemical Minerals,1999,21(2):65-68. |
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| Authors: | Liu XiFang |
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| Abstract: | Zabuye saline lake, situated in the hinterland of Tibet plateau, is a contemparysaline lake deposit. In thispaper, on the base of field work, valuable studies were performed on the stratigraphy, magmatism,metamorphisrn and tectonic characteristics around Zabuye lake. According to the lacustrine sedimentary characteristics,the mineralizing evolution of the saline lake was stated and some possible origins of the metallogenic materialswere pointed out. |
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| Keywords: | Zabuye saline lake stratisraphy magmatism metamorphism tectonism mineralizing evolution |
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