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Discovery of deep-level foreland thrust-fold structures in Taihang Mt. and its implication for early tectonic evolution of North China
引用本文:LI Jianghai,NIU Xianglong,CHEN Zheng,Timothy M KUSKY,Ali POLAT. Discovery of deep-level foreland thrust-fold structures in Taihang Mt. and its implication for early tectonic evolution of North China[J]. 自然科学进展(英文版), 2005, 15(3): 229-238. DOI: 10.1080/10020070512331342040
作者姓名:LI Jianghai  NIU Xianglong  CHEN Zheng  Timothy M KUSKY  Ali POLAT
作者单位:Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871,China,Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871,China,Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871,China,Department of Earth and Atmospheric Sciences, Saint Louis University, St. Louis, MO 63103, USA,Department of Earth Sciences, University of Windsor, Windsor, ON, N9B 3P4, Canada
摘    要:Delineation and correlation of Dragon Spring Shear Zone with its deep-level structures at foreland have been studied by field work. This paper reports our new findings of thrust-fold structures within Taihang Neoarchean basement, which include flat thrusts,large-scale recumbent folds, subhorizontal foliation patterns, etc. It reveals that early tectonic evolution of North China clearly involves the horizontal contraction on a large scale, comparable to those of foreland of classical collisional orogenic belts. The vertical variation of structural patterns with foreland fold-thrust belt from shallow to deep levels has been documented for Taihang Mt. by structural correlation,which is associated with tectonic transposition and imbrication of basement complex with supracrustal sequences in the Neoarchean.

关 键 词:recumbent fold   shear zone   crustal thickening   collisional tectonics   foreland   Neoarchean.

Discovery of deep-level foreland thrust-fold structures in Taihang Mt. and its implication for early tectonic evolution of North China
LI Jianghai,NIU Xianglong,CHEN Zheng,Timothy M KUSKY,Ali POLAT. Discovery of deep-level foreland thrust-fold structures in Taihang Mt. and its implication for early tectonic evolution of North China[J]. Progress in Natural Science, 2005, 15(3): 229-238. DOI: 10.1080/10020070512331342040
Authors:LI Jianghai  NIU Xianglong  CHEN Zheng  Timothy M KUSKY  Ali POLAT
Affiliation:1. Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871,China
2. Department of Earth and Atmospheric Sciences, Saint Louis University, St. Louis, MO 63103, USA
3. Department of Earth Sciences, University of Windsor, Windsor, ON, N9B 3P4, Canada
Abstract:Delineation and correlation of Dragon Spring Shear Zone with its deep-level structures at foreland have been studied by field work. This paper reports our new findings of thrust-fold structures within Taihang Neoarchean basement, which include flat thrusts,large-scale recumbent folds, subhorizontal foliation patterns, etc. It reveals that early tectonic evolution of North China clearly involves the horizontal contraction on a large scale, comparable to those of foreland of classical collisional orogenic belts. The vertical variation of structural patterns with foreland fold-thrust belt from shallow to deep levels has been documented for Taihang Mt. by structural correlation,which is associated with tectonic transposition and imbrication of basement complex with supracrustal sequences in the Neoarchean.
Keywords:recumbent fold  shear zone  crustal thickening  collisional tectonics  foreland  Neoarchean
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