摘要
根据地球卫星遥感影象、地物波谱测定以及地貌景观、古水系演化和地面地质调查等资料的综合研究表明 ,柴达木盆地察尔汗盐湖矿区北部外围地带存在一种新的成因类型的盐湖———沙下盐湖。通过对其主体物质结构和成盐环境的初步分析 ,认为其主要成盐方式呈现为复式成盐建造系统 ,为在我国广大的内陆盆地寻找同一类型的地下卤水矿产资源提供了科学依据 ,具有理论意义和经济价值。
Based on the synthetical data from the remote images,geological section,geomorphologic landscape,ancient water system evolution and surface feature spectrum etc,the study indicates that there is an undersand lake in the northern peripberal belt of Qarhan Salt Lakes of Qaidam Basin. From the preliminary analysis of the main body material structure and the salt-forming environment in the undersand lake, the author considered that the major salt-forming fashion showed the complex salt-forming formation, It proveded scientific basis to find the mineral resources of the undergroand brine of the same type in the vast inland basin in our country .It has theoretical importance and economic value.
出处
《海湖盐与化工》
2000年第2期1-4,12,共5页
Sea-Lake Salt and Chemical Industry
基金
国家八五攻关项目! (85- 80 2 - 1)
