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华北克拉通原型盆地及岩浆活动时空演化对克拉通破坏的制约

, PP. 1396-1409

Keywords: 华北克拉通,中生代,浅部地质,原型盆地,时空演化

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Abstract:

?原型沉积盆地及岩浆活动时空演化过程能够为华北克拉通破坏提供有效的制约.总体上,华北克拉通破坏表现出自下而上、由边缘至腹地逐渐渗透以及时空不均一性特点.华北东部腹地可能在早-中侏罗世已经遭到破坏,破坏过程受到周边多板块作用的共同制约.古亚洲洋板块的俯冲至少使华北克拉通北缘遭到破坏,扬子板块的碰撞对克拉通破坏的影响是深远的,控制了晚三叠世-中侏罗世构造岩浆活动的时空演化,Izanagi板块和古太平洋板块的俯冲起到了决定性作用,导致华北克拉通最终被破坏.克拉通破坏的主导机制可能是热机械-化学侵蚀机制.

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