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小秦岭地体褶皱特征及其形成机制
引用本文:裴锋敏.小秦岭地体褶皱特征及其形成机制[J].河南国土资源,1997(3).
作者姓名:裴锋敏
作者单位:河南省地矿厅地调一队
摘    要:小秦岭地体中的褶皱包括露头褶皱和宏观褶皱,组成褶皱的面理为次生构造面理。露头褶皱为地壳早期在伸展机制下发生左行张扭剪切作用产生的构造形迹;宏观褶皱为侵入岩浆穹起、底辟作用向外扩张空间推拉围岩形成的构造格局

关 键 词:褶皱特征,形成机制,左行张扭,侵入岩,小秦岭地体

THE FOLD FEATURES AND MECHANISM OF FORMATION OF XIAOQINLING TERRANE
Pei,Fengmin.THE FOLD FEATURES AND MECHANISM OF FORMATION OF XIAOQINLING TERRANE[J].Henan Land & Resources,1997(3).
Authors:Pei  Fengmin
Abstract:The fold in the Xiaoqinling terrane included the outcrop fold and macrofold, and the foliation formed by the fold was the secondary structural foliation. The outcrop fold was a structural feature formed by the crust occurred the left lateral tenso shear shearing under the extentional mechanism in the early period. The macrofold was a tectonic framework formed by the uplift of invasive magma and by spreading space outward and compressing wallrock of diapirism.
Keywords:fold  features    mechanism  of  formation    left  lateral  tenso  shear    intrusive  rock    Xiaoqinling  terrane  
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