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剑川盆地位于云南省西北部,地处云南高原与青藏高原交界处的横断山脉中段东侧。在大地构造上处于三江褶皱系的金沙江优地槽褶皱带与杨子地台的盐源—丽江台缘褶皱带交界处,红河断裂带之东缘。本区新构造运动十分强烈,而且剑川盆地和整个云南高原在隆起成因、隆起时间及隆起幅度等方面均与青藏高原有密切联系。
The Jianchuan Basin is located in the northwestern Yunnan Province, east of the middle section of the Hengduan Mountains at the junction of the Yunnan Plateau and the Qinghai-Tibet Plateau. In the geotectonic structure, the Jinshajiang Youdian fold belt in the Sanjiang fold system and the Yanyuan-Lijiang platform fold belt junction of Yangzi platform and the eastern margin of the Honghe fault zone. Neotectonic movement in this area is very strong, and the Jianchuan Basin and the entire Yunnan Plateau are closely linked with the Qinghai-Tibet Plateau in terms of uplift origin, uplift time and uplift amplitude.