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《GEOLOGY OF ANHUI》 2000-01
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ON THE FEATURES,ORIGIN AND TIME OF THE GNEISS SUITE IN THE FUCHASHAN AREA OF ANHUI

TONG Jing-song, XU Wei (Anhui Academy of Geological Survey, Hefei 230001, China)  
This paper, based on 1: 50000 scale geological mapping data, has systematically expounded the petrological, petrochemical and geochemical characteristics of a gneiss suite, a metamorphosed and deformed intrusive rock association emplaced into the Kanji and Feidong rock groups. It is affirmed to be a suite of cafe - alkaline series of cognate evolving sequence with its origin (magmatic source and structual setting, etc. ) and diagenetic time (formed in the Luliang period and was reworked by structural superimposed metamorphism in the Jinning period)being analyzed, providing an important geological basis for correct recognition of the early stage of evolution of the Wanzhong section of the Dabie - Sulu orogen.
【CateGory Index】: P588.345
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【References】
Chinese Journal Full-text Database 1 Hits
1 XU Wei1,2, DONG Jin song1, ZHU Guang2, SONG Chuan zhong2 (1 Anhui Institute of Geological Survey, Hefei 230001, Anhui; 2 Dept. of Resources and Environmental Science, Hefei University of Technology, Hefei 230000, Anhui);Characteristics of an orogen-related ductile shear zone in the Feidong area, Anhui[J];Regional Geology of China;2001-03
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1 Liu Yican 1,2 ,Xu Shutong 1,Jiang Laili 1,Wu Weipng 1 ,Su Wen 1 and Chen Guanbao 1 (1 Anhui Institute of Geology,Hefei 230001,China;2 Department of Earth and Space Sciences,University of Science and Technology of China, Hefei 230026,China);NEW PROGRESS IN RESEARCH OF THE MAFIC ULTRAMAFIC ROCK BELT IN THE NORTHERN PART OF THE DABIE MOUNTAINS[J];GEOLOGY OF ANHUI;1999-04
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