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《Acta Geoscientica Sinica》 2012-06
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The Metamorphic Evolution History of High Pressure Granulites in Chengde Area,Northern Margin of North China:Zircon Chronology and Geochemical Evidence

CHU Hang 1),WANG Hui-chu 1),WEI Chun-jing 2),LIU Huan 1),ZHANG Kuo 1) 1) Tianjin Institute of Geology and Mineral Resourses,China Geological Survey,Tianjin 300170;2) School of Earth and Space Sciences,Peking University,Beijing 100871  
High pressure granulites in Chengde area of northern Hebei province occur as tectonic lenses with weak deformation in a wide composite shear zone composed dominantly of granitic gneiss.The deep crust thermal dynamics and exhumation mechanism demonstrated by these granulites play a critical role in the study of the collisional orogenic model of North China craton and the tectonic evolution model of North China craton as a whole.According to the result of U-Pb isotopic dating for these high pressure granulites and their surrounding rocks,the age of the surrounding protolith is ca.2500 Ma.At around 2297 Ma,basic rock intruded granitic gneiss.At around 2381 Ma,subduction started,and then there occurred high-pressure-granulite-phase metamorphism.Following the subduction and a long-term crust thickening process,the exhumation at a certain point began after 2001 Ma.During the exhumation process,another basic dike invaded at around 1896 Ma.At 1885 Ma,the uplifting process and granulite-phase retrograde metamorphism took place.At 1850 Ma,a large part of North China experienced high-amphibolite phase metamorphic event including even partial melt.This event destroyed most part of the Paleoproterozoic metamorphic evolution.It can thus be seen that Paleoproterozoic geological evolution history in Chengde area or even the whole northern part of North China was not one or two phases of independent events that happened in different places.Instead,it was a complex and continuous process.Previous studies only revealed events of a few stages,whereas the high pressure granulites in Chengde area have recorded much more information.
【Fund】: 国家青年自然科学基金项目(编号:40902021);; 国家自然科学基金项目(编号:40772120);; 中国地质调查局地质大调查项目(编号:1212011121077)联合资助
【CateGory Index】: P597.3
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