它是由印度板块在缅甸微板块下移动时发生的大型逆冲事件引起的。
It was caused by a megathrust event as the India plate moved beneath the Burma microplate.
古近纪末期逆冲构造形成机制与印度板块向欧亚板块之下俯冲的远程效应有关。
The overthrust tectonics at the end of Paleogene are related to the remote effect of subduction of Indian plate beneath Eurasian plate.
汝州煤田位于华北板块南缘逆冲推覆构造带豫西段前锋部位，区内逆冲推覆构造较发育。
The Ruzhou coalfield lies at the front part of thrusting nappe structural zone western Henan sector, south margin of the North China plate.
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