【摘 要】
：
青藏高原是我国重要的盐湖资源分布区,区域内盐湖资源主要分布在柴达木盐地和羌塘高原,具集中带状分布、资源储量巨大和共生特色资源三大特点。柴达木盆地盐湖总体上以富含钾
【机 构】
：
中国地质大学(北京)地球科学与资源学院,中国地质科学院矿产资源研究所,
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青藏高原是我国重要的盐湖资源分布区,区域内盐湖资源主要分布在柴达木盐地和羌塘高原,具集中带状分布、资源储量巨大和共生特色资源三大特点。柴达木盆地盐湖总体上以富含钾、镁、硼、锂、钠为特点,称为钾镁盐湖;羌塘高原盐湖以贫钾,富含硼、锂、铯等为特点,称为特种盐湖。
The Qinghai-Tibet Plateau is an important distribution area of salt lake resources in our country. Salt lake resources in the region are mainly distributed in the Qaidam salt field and the Qiangtang Plateau. They have three major characteristics: a concentrated belt-shaped distribution, huge resource reserves and symbiotic characteristic resources. The salt lake in the Qaidam Basin is generally characterized by potassium, magnesium, boron, lithium and sodium, and is called potassium-magnesium lake. The salt lake in the Qiangtang Plateau is characterized by poor potassium and boron, lithium and cesium, salt lake.
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