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《Chinese Science Bulletin》 2014-01
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The discovery of blueschist-facies rock in Airgin Sum area, Erenhot, Inner Mongolia and its tectonic significance

LI RuiBiao;XU Bei;ZHAO Pan;TONG QinLong;ZHANG JinRui;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University;National Key Laboratory of Remote Sensing Information and Image Analysis Technology, Beijing Research Institute of Uranium Geology;  
Blueschist has been discovered in mélange of the early-middle Paleozoic Orogenic Belt in Airgin Sum area, Erenhot. Mineral chemistry analysis reveals that the blue-amphibole belongs to sodic-calcic and sodic amphiboles in this rock. The sodic-calcic amphibole can be divided into magnesiokatophorite, winchite and barroisite, while all the sodic amphiboles are magnesioriebeckite. Our research indicates that the temperature and pressure of blueschist-facies metamorphism were about 400–450°C and 0.7–1.0 GPa, respectively, which suggests a high-pressure, low-temperature metamorphic condition. The discovery of the blueschist-facies rock indicates that the early-middle Paleozoic Orogenic Belt extends 200 km to the west and the suture between North China Plate and South Mongolia Microcontinent is located from Airgin Sum to Sunid Zuoqi.
【Fund】: 国家重点基础研究发展计划(2013CB429800);; 国家自然科学基金(40872145 40821002)资助
【CateGory Index】: P542
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