Research Article
Origin of Boron and Brine Evolution in Saline Springs in the Nangqen Basin, Southern Tibetan Plateau
| | Saline spring | Location | Rock type | Age |
| | Dagai | N32° 12′ 15.1′′ E96° | Sandstone + mudstone | Paleogene | | Riazhong | N32° 15′ 58.8′′ E96° | Sandstone, gypsum + mudstone | Paleogene | | Niuriwa | N32° 08′ 38.7′′ E96° | Sandstone, gypsum + mudstone | Paleogene | | Duolunduo | N32° 04′ 48.5′′ E96° | Sandstone, volcanic rock + mudstone | Paleogene | | Baizha | N31° 56′ 02.6′′ E96° | Sandstone + mudstone | Paleogene | | Ranmu | N32° 26′ 43.1′′ E95° | Clay | Paleogene | | Gayang | N32° 03′ 47.9′′ E95° | Sandstone + mudstone | Paleogene |
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