Andesite in the Chiang Khong–Lampang–Tak igneous zone erupted at Late Triassic period.
Geochemical data suggest the volcanic rocks formed in a post-collisional setting.
The formation of the rocks was related to the upwelling of the asthenospheric mantle.
Chiang Khong–Lampang–Tak igneous zone can link with the Lancangjiang igneous zone.
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