Global Geology 2016, 19(2) 69-77 DOI:     ISSN: 1673-9736 CN: 22-1371/P

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Keywords
Daqingshan area
high- grade metamorphic rocks
deformation
strain
partial melting
Authors
SHAO Yilun
LIU Yongjiang
JIA Jie
LI Weimin and JIN Wei
PubMed
Article by Shao Y
Article by Liu Y
Article by Jia J
Article by Li WAJW

Genesis of lower strain S- L- type tectonites in Daqingshan area,Inner Mongolia

SHAO Yilun, LIU Yongjiang, JIA Jie, LI Weimin and JIN Wei

1. College of Earth Sciences,Jilin University,Changchun 130061,China; 2. China- Japan Union Hospital of Jilin University,Changchun 130033,China

Abstract

Usual ductile shear zone has relatively high strain magnitude. However,for high- grade metamorphic rocks in Daqingshan area,the related strain is very low with weakly developed lineation. Significantly,the fi- nite strain type with a K- value slightly lower than 1 and is characterized by compressional strain. Because the special tectonic environment with high temperature,the percentage of melt is relatively higher,which leads to a series of microscopic phenomenon such as multi- grain quartz bands,feldspar three edges equilibrium- like tex- ture,granular flow,etc. As a consequence,the tectonites in the studied area illustrate a unique character: ob- vious rheological meso- deformation structure but with very weak intracrystalline micro- deformation.

Keywords Daqingshan area   high- grade metamorphic rocks   deformation   strain   partial melting  
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