DYNAMOMETAMORPHIC COMPLEXES AND STRUCTURAL ZONING OF IRTYSH SHEAR ZONE

作     者：Zinoviev S.V. Chikov B.M. LiZhichun 

作者机构：Instituteof GeologySB of RASRussiaInstituteof GeologySB of RASRussiaChangshaInstitute of GeotectonicsCASChangsha410013HunanChina 

出 版 物：《Geotectonica et Metallogenia》 (大地构造与成矿学（英文版）)

年 卷 期：1996年第20卷第Z1期

页      面：124-125页

学科分类：0709[理学-地质学] 081803[工学-地质工程] 07[理学] 08[工学] 0818[工学-地质资源与地质工程] 

主　　题：幻山 

摘      要：Irtysh shear zone is a stretched, but relatively narrow nearfault tectonic zone, which ischaracterized by the following features: a) general sturcture anisotropy (310-320o) with pre-dominance of symmetrical relationships of planar and linear types; b) predominant develop-ment of bended blastomyolnite, blastocataclasite and metamelange fomations; c)regional,but non-uniform foliation of ricks and general manifestation of structures of the shearingflow; d) separation of numerous lenses of mingmatite-like and pegmatoid formations, smallintrusions of leucocratic granites, granite-porphyres and granite-aplites and dike-like bodiesof gabbro-dyabaes and ultrabasic rlcks, rarely.