Triassic tectonics of the Ailaoshan Belt (SW China): Early Triassic collision between the South China and Indochina Blocks, and Middle Triassic intracontinental shearing
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文摘

The collision between Indochina and S. China blocks was accommodated by a southwestward subduction.

A ductile top-to-the-NE ductile shearing characterizes the Ailaoshan Belt.

The Early Triassic collision triggered late-orogenic crustal melting, followed by Middle Triassic top-to-the-NE shearing.

A detail tectonic correlation between the Ailaoshan and Vietnam belts is provided.

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