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地质论评  2001 

花岗岩拓扑学的研究展望

Keywords: 花岗岩大地构造环境拓扑学处理成因克幔相互作用热流传递机理

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Abstract:

花岗岩拓扑学(granitetopology)着重阐明花岗岩区域岩石成因及其与大地构造环境的联系,花岗岩是多种地质因素及其相互作用的产物,总体上受壳幔相互作用中热流传递机理的控制,这种热扰动和相继的热松弛与地表的大地构造环境又有重要的联系,根据目前研究,花岗岩的区域岩石成因和大地构造环境的联系实际上仅同大地构造旋回中由某种热扰动所引起的某一构造阶段有关,因而一个大的构造单元往往可以出现一系列不同成因的花岩类型及其组合。

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