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《Geotectonica Et Metallogenia》 2008-01
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GEOCHEMISTRY OF PENGGUAN COMPLEX IN THE LONGMENSHAN REGION,WESTERN SICHUAN PROVINCE,SW CHINA:PETROGENESIS AND TECTONIC IMPLICATIONS

ZHANG Pei,ZHOU Zuyi,XU Changhai and ZHANG Qinglin(State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China)  
The Pengguan complex,located in the Longmenshan thrust belt,western margin of the Yangtze block,SW China,was formed during the Neoproterozoic.Major and trace element abundances are reported,and the source and tectonic significance of the complex are discussed in this paper.The complex is dominantly composed of acid-intermediate intrusive rocks.12 samples from the Pengguan complex show variable major oxides with SiO2 ranging from 57.70% to 71.90%.The rocks have relative high Na2O contents(K2O/Na2O=0.31~0.85),δ values vary from 1.33 to 2.28 and A/CNK ratios from 0.93 to 1.08,indicating calc-alkaline series metaluminous to weak peraluminous granitoids for the Pengguan complex.The rocks have relative low abundance of REE(∑REE=76.25×10-6~139.80×10-6)with variable differentiation between LREE and HREE(LaN/YbN=3.86~35.23)and weak negative to positive Eu anomalies(δEu=0.70~1.86).The rocks are enriched in Rb,Sr,Ba,K and depleted in Nb,Ta,P,Y.Most samples have relatively high Mg# values(45)and Sr/Y ratios(20.03~111.34)compared to crust-derived calc-alkaline granitoids.Moreover,the Pengguan rocks show the affinity with the adjacent adakitic Xuelongbao plutonic complex.The geochemical features suggest that the Pengguan complex was generated by mixing of the underplated mantle-derived magma and the melting of lower crust.Combined with previous study,we consider the Neoproterozoic extensive igneous rocks along the western margin of the Yangtze block were formed in a subducted-related volcanic arc environment.
【Fund】: 国家自然科学基金项目(40621063)资助
【CateGory Index】: P588.121;P595
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1 ZHANG Qi Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;The central belt of the North China Craton during Paleoproterozoic is an orogenic belt?[A];[C];2012
2 ZHANG Qi~1,JIN Weijun~1,LI Chengdong~2,WANG Yan~3 and WANG Yuanlong~1 (1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China;3.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640,Guangdong,Cnina);Granitic Rocks and Their Formation Depth in the Crust[A];[C];2012
3 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);GUESS ON THE SILURIAN-DEVONIAN NORTH CHINA HIGHLAND:EVIDENCE FROM THE INFORMATION OF GANSU[A];[C];2012
4 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Are-discussion on the classification of granites and their relationship with Cu-Au and W-Sn mineralization:A reply to the comments by Messrs Hua Renmin and Wang Denghong about"Zhang Qi et al(2010):Relationship between granitic rocks and Au-Cu-W-Sn minerali[A];[C];2012
5 Zhang Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Reappraisal of the origin of C-type adakitic rocks from East China[A];[C];2012
6 ZHANG Qi,JIN WeiJun,LI ChengDong and WANG YuanLong 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China;On the classification of granitic rocks based on whole-rock Sr and Yb concentrationsⅢ:Practice[A];[C];2011
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Liu Jiayuan(Institute of Hidden Ore Deposits Prognostication,Gullin College of Geology);TECTONIC EVOLUTION AND GENETIC TYPES OF THE PRECAMBRIAN GRANITOIDS IN SOUTH CHINA AND THEIR RELATIONSHIPS WITH MINERALIZATION[J];GEOLOGY OF ANHUI;1994-Z1
2 Hou Wei Chen Huifang Liang Xinquan Wang Kefu(Changsha Institute of Geote ctonics, Academia Sinica);THE ESTABLISHMENT OF PRECA MBRIAN STRATA AND NEW RECOGNITION OF THE GEOTECTONIC EVOLUTION IN HAINAN ISLAND[J];;1992-02
3 Song Hongbiao;Liu Shugen;THE RELATION OF GRAVITY AND AEROMAGNETIC FIELD AND DEEP STRUCTURE IN MIDDLE-NORTHERN LONGMENSHAN MOUNTAINS[J];;1991-01
4 Sun Chuanming;PROTEROZOIC OPHIOLITES IN WESTERN SICHUAN AND THE PROTEROZOIC OROGENIC BELT ON THE WEST BORDER OF YANGTZE PALEO-PLATE[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;1994-04
5 Lin Maobing; Ma Yongwang;A DISCUSSION ON THE TECTONIC CHARACTERISTICS OF PENG-GUAN COMPLEX IN LONGMEN MOUNTAINS[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;1995-01
6 LIANG Xinquan HOU wei CHEN Huifang(Changsha Institute of Geotectonics, Academia Sinica);CHARACTERISTICS OF THE GEZHEN BRITTLE-DUCTILE SUPERIMPOSITION SHEAR ZONE AND ITS SIGNIFICANCE FOR ORE FORM ATION[J];Geotectonica Et Metallogenia;1990-03
7 DING Shijiang (Hainan Exploration Institute of Geosciences, Haikou 570005);THE GEOLOGICAL CHARACTERISTICS OF GEZHEN INTRUSIVE MASS IN WESTERN HAINAN AND ITS SIGNIFICANCE[J];Geotectonica Et Metallogenia;1995-04
8 XU De ru, LIANG Xing quan, TANG Hong feng (Changsha Institute of Geotectonics, Academia Sinica, Changsha 410013, China);GEOCHEMICAL CHARACTERISTICS OF METAMORPHIC BASIC VOLCANICS FROM THE BAOBAN GROUP,WESTERN HAINAN AND ITS TECTONIC IMPLICATIONS[J];Geotectonica Et Metallogenia;2000-04
9 XU De-ru, LIANG Xing-quan, CHENG Guang-hao, HUANG Zhi-long, HU Hui-dong (Changsha Institute of Geotectonics, Academica Sinica, Changsha 410013, China; 2. institute of Geochemistry, Academica Sinica, Guiyang 550002, China);RESEARCH ON THE GEOCHEMISTRY AND GENESIS OF MESOPROTEROZOIC GRANITES ON HAINAN ISLAND[J];Geotectonica Et Metallogenia;2001-04
10 XIAO Yong-jun 1,2,CHEN Guang-hao1,FU Gong-gu1 (1.Changsha Institute of Geotectonics,Chinese Academy of Sciences,Changsha410013,China;2.Post-graduate School of the Chinese Academy of Sciences,Beijing100039);DISCUSSION ON THE TECTONOMETALLOGENIC BACKGROUND OF THE DAWAN GOLD ORE DISTRICT,NORTHEASTERN HUNAN PROVINCE[J];Geotectonica Et Metallogenia;2002-02
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