资源环境科技发展态势分析平台

We re-evaluate 357 Jurassic-Holocene paleomagnetic datasets from Tibet-Indochina and compare them with present-day GPS velocity field. SE Tibet NW of the East Himalaya Syntaxis (EHS) underwent 20°-30° counterclockwise rotations around 50 Ma, and mostly clockwise rotations after 40 Ma. NE of the EHS, post-50 Ma clockwise rotation occurred, whereas highly scattered clockwise rotations took place on northern Indochina at 25-15 Ma, after a remagnetization episode. We suggest that the indentation of Greater India NE corner at ∼50 Ma resulted in a wide orogenic reentrant characterized by opposite rotations at orocline limbs. Rotations East of EHS after 40 Ma were likely due to local strike-slip fault activity. After 30 Ma, the ongoing India collision fragmented Indochina into km-scale blocks that experienced independent rotations. The present-day clockwise rotation pattern around the EHS started at 15-10 Ma along with eastward Tibet crustal spreading, and has not produced yet a detectable paleomagnetic rotation.