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《Geological Bulletin of China》 2007-05
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Structure of metamorphic strata of the khondalite series in the Daqingshan-Wulashan area,central Inner Mongolia,China,and their geodynamic implications.

XU Zhong-yuan,LIU Zheng-hong,YANG Zhen-sheng,WU Xin-wei,CHEN Xiao-feng College of Earth Science,Jilin University,Changchun 130061,Jilin,China  
Study of the high-grade metamorphic complex in the Daqingshan-Wulashan area,Inner Mongolia,indicates that the khondalite series in the area has undergone subhorizontal bedding-parallel dêcollement deformation and then modification by the dome-fold structure and nearly E-W-trending steeply dipping foliation belts.The former resulted in "omission of strata and hiatal contact of originally separated layers,which in space is indicated by the structure of metamorphic strata formed in the early stage by stacking of subhorizontal podiform bodies with nearly E-W-trending long axes.The stacking of the nearly E-W-trending steeply dipping foliation belts in the late stage caused the metamorphic strata to occur as irregular bands,patches or lenses and various metamorphic units and series to occur in a jigsaw-like form and interlock each other.It is concluded that the khondalite series underwent at least two orogenic cycles.The subhorizontal bedding-parallel dêcollement deformation structure and its corresponding structure of metamorphic strata are the product of the late stage of the first orogenic cycle,while the nearly E-W-trending steeply dipping foliation belts and their corresponding structure of metamorphic strata are attributed to the second orogenic cycle.
【Fund】: 国家自然科学基金项目(编号:40572117);; 中国地质调查局区域地质调查项目(编号:J5.3.4 200113000021)联合资助
【CateGory Index】: P588.3
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