陆源咸水湖
又称陆源盐湖(terrigenous salt lake)。陆地上形成的咸水湖。湖水中离子主要是由入湖河流与地下水携带而来。它主要分布于干旱与半干旱地区。在湿润与半湿润地区，如果在一湖泊流域的范围内分布有岩盐地层，有时也能形成咸水湖。中国青海省的茶卡盐池、内蒙古的吉兰泰盐池、山西运城解池等都是陆源咸水湖。
23
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contributed at 2011-10-11
Classification(s)
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Earth System(in Chinese) Geomorphology
Detailed Description
| English |
|---|
| Name | terrigenous saltwater lake |
| Chinese |
|---|
| Name | 陆源咸水湖 |
| Description | 又称陆源盐湖(terrigenous salt lake)。陆地上形成的咸水湖。湖水中离子主要是由入湖河流与地下水携带而来。它主要分布于干旱与半干旱地区。在湿润与半湿润地区，如果在一湖泊流域的范围内分布有岩盐地层，有时也能形成咸水湖。中国青海省的茶卡盐池、内蒙古的吉兰泰盐池、山西运城解池等都是陆源咸水湖。 |
How to Cite
NNU_Group (2011). 陆源咸水湖, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/234f1977-4a86-4637-bf1e-241c3c32c711
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