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《Acta Petrologica Et Mineralogica》 2006-03
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Syn-deformational granites of the Longquanguan ductile shear zone and their monazite electronic microprobe dating

ZHAO Lan, ZHANG Jin-jiang and Liu Shu-wen(Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing, 100871, China)  
A series of prolonged granitic intrusions occur along the foliation of the Longquanguan ductile shear zone. Petrological and structural characteristics show that they are possibly syn-deformational granites resulting from partial melting of the country rock caused by shearing. The electronic microprobe dating of monazites from these granites shows that the major deformation episode took place at 1?877~1?846 Ma, the second deformation episode occurred at 1?812~1?782 Ma, and the fluid activities happened in the late stage at about 1?725 Ma . The major deformation of the Longquanguan ductile shear zone occurred synchronously with the tectonic events in the central zone of the North China craton in the Late Paleoproterozoic, and this shear zone seems to have been one of the main shear zones formed by the collision of eastern and western blocks.
【Fund】: 国家自然科学基金重大国际合作项目(40420120135)
【CateGory Index】: P588.121
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