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《Geotectonica Et Metallogenia》 2004-04
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CHARACTERISTICS AND ORIGIN OF HIGH-NA ADAKITE-LIKE ROCKS: THE LATE CRETACEOUS ZHANTANG ANDESITES IN THE HUICHANG BASIN, JIANGXI PROVINCE

CAI Zhiyong~(1,2), XIONG Xiaolin~1 and SUN Sancai~3 (1.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China;2.Northwestern Hubei Survey of Geology and Mineral Resources, Xiangfan, HB 441003, China)  
The Zhantang andesites occur in the Cretaceous Huichang Basin, Eastern Nanling Range of SE China, and were formed under an intracontinental, extensional tectonic setting that was not associated with subduction. They are high-Na (up to 8.46% Na_2O), high-Al trondhjemitic rocks, with high concentrations of Sr and Ba, low concentrations of MgO, CaO, Cr, Co Ni, Y and HREE, and high Sr/Y and La/Yb and low Rb/Sr ratios. Partial melting of mantle lithosphere, magmatic mixing or fractional crystallization cannot explain the origin of these compositionally distinctive magmas, while partial melting of garnet-containing basaltic protolith such as subducted slab or basaltic underplate can account for many features of these magmas. The high Na, Al and high Sr/Y and La/Yb features of the Zhantang andesites are similar to those of adakite resulted from slab-derived melting. However, the Zhantang andesites were not derived from subducted slab. As compared with adakite, they are much higher in Na_2O but lower in CaO. The ε_(Nd)(t) (-2.3~-3.8) and initial ()~(87)Sr/~(86)Sr (0.707~0.708) are also significantly different from those of most adakites which have like-MORB isotopic compositions. These chemical and isotopic data together with the geological setting suggest that subducted slab was not involved in producing these magmas. Alternative derivation of these magmas is therefore the partial melting of underplated basaltic lower crust. Partial melt composition of basalt is closely related to source composition. The high Na_2O and low CaO signature for the Zhantang magmas suggests a compositionally particular source. Comparison shows that the Zhantang andesites are generally compositionally similar to the high-pressure partial melts of the alkali-rich, high Na_2O and low CaO basalt (Rapp and Watson, 1995). We therefore suggest that the Zhantang high-Na and low-Ca adakite-like magmas were produced, at a pressure high enough to stabilize garnet (≥10×~8 Pa), by melting of an alkali-rich basaltic (amphibolitic) underplate. The melting probably took place in response to the continued magma underplating and thickening at the base of the crust of the Eastern Nanling Range.
【Fund】: 中科院知识创新工程项目(KZCX2-102;KZCX2-SW-117)资助.
【CateGory Index】: P588.1
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2 ZHANQ Qi,JIN WeiJun,WANG YuanLong,LI ChengDong and JIA XiuQin 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China 3.Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100039,China;Discussion of north boundary of the East China Plateau during late Mesozoic Era[A];[C];2008
3 ZHANG Qi,WANG Yuan-long,JIN Wei-jun,JIA Xiu-qin,LI Cheng-dong 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100039,China; 3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China;Criteria for the recognition of pre-,syn-and post-orogenic granitic rocks.[A];[C];2009
4 ZHANG Qi,WANG Yan,JIN Wei-jun, WANG Yuan-long,LI Cheng-dong,XIONG Xiao-lin 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China; 3.Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China;Mountain range in northern North China during the Early Mesozoic:evidence from granite.[A];[C];2009
5 MAO QiGui,XIAO WenJiao,HAN ChunMing,SUM Min,YUAN Chao,ZHANG JiEn,AO SongJian and LI JiLiang 1.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.China Non-Ferrous Metals Resource Geological Survey,Beijing 100012,China 3.Beijing Institute of Geology for Mineral Resources,Beijing 100012,China 4.Department of Earth Science,The University of Hong Kong,Kong,China 5.Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;Discovery of Middle Silurian adakite granite and its tectonic significance in Liuyuan area,Beishan Moutains,NW China[A];[C];2011
6 LI JiLei~(1,2),QIAN Qing~1,GAO Jun~1,SU Wen~1,ZHANG Xi~(1,2),LIU Xin~(1,2) and JIANG Tuo~(1,2) 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China;Geochemistry,zircon U-Pb ages and tectonic settings of the Dahalajunshan volcanics and granitic intrusions from the Adengtao area in the Southeast Zhaosu,western Tianshan Mountains[A];[C];2011
7 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
8 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,China Geology Survey,Tianjin 300170,China;Revisiting the new classification of granitic rocks based on whole-rock Sr and Yb contents:Index.[A];[C];2011
9 DUAN XiaoXia,LIU JianMing,WANG YongBin,ZHOU LingLi,LI YongGui,LI Bin,ZHANG Zhuang and ZHANG ZuoLun 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China 3.Dandong Qingchengzi Mining Co,LTD.,Dandong 118107,China 4.China Railway Resources Exploration Company,Beijing 100039,China;Geochronology,geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield,Liaoning[A];[C];2013
10 Tuo Jiang;Jun Gao;Reiner Klemd;Qing Qian;Xi Zhang;Xianming Xiong;Xinshui Wang;Zhou Tan;Bangxue Chen;Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences;University of Chinese Academy of Sciences;GeoZentrum Nordbayem,Universitt Erlangen-Nmberg,Schlossgarten 5a,91054 Erlangen,Germany;College of Resource and Environment Engineering,Guizhou University;School of Geology and Exploration,Xinjiang University;;Paleozoic ophiolitic melanges from the South Tianshan Orogen,NW China:Geological,geochemical and geochronological implications for the geodynamic setting[A];[C];2015
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 DENG Jin-fu, WU Zong-xu(China University of Geology, Beijing 100083, China);LITHOSPHERIC THINNING EVENT IN THE LOWER YANGTZE CRATON AND Cu-Fe METALLOGENIC BELT IN THE MIDDLE AND LOWER YANGTZE RIVER REACHES[J];Geology of Anhui;2001-02
2 Wu Fuyuan,Sun Deyou (Changchun University of Science and Technology,Changchun 130026);THE MESOZOIC MAGMATISM AND LITHOSPHERIC THINNING IN EASTERN CHINA[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;1999-04
3 Li Kun-ying, Shen Jia-lin and Wang Xiao-ping;Isotopic geochronology of Mesozoic terrestrial volcanic rocks in the Zhe-jiang-Fujian-Jiangxi area[J];Journal of Stratigraphy;1989-01
4 Li Xianhua Zhao Zhenhua Gui Xuntang Yu Jinsheng(Institute of Geochemistry, Guangzhou Branch, Academia Sinica, 510640);Sm-Nd ISOTOPIC AND ZIRCON U-Pb CONSTRAINTS ON THE AGE OF FORMATION OF THE PRECAMBRIAN CRUST IN SOUTHEAST CHINA[J];Geochimica;1991-03
5 Zhang Yuquan; Xie Yingwen; Liang Huaying; Qiu Huaning; Li Xianhua (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)Sun-Lin Chung (Department of Geology, Taiwan University, Taipei 10770);PETROGENESIS SERIES AND THE ORE-BEARING PORPHYRIES OF THE YULONG COPPER ORE BELT IN EASTERN TIBET[J];Geochimica;1998-03
6 WANG Qiang;WANG Ren-jing;QIU Jia-xiang;ZHAO Zhen-hua;SANG Long-kang; HU Zheng-xiang;DAI Sheng-qian;HE Yong;ZHOU Guo-hua;XU Wei; WANG Jian-xin;QI Xian-mao;ZHANG Shun-jin (1. Guangzhou Institute of Ceochemistry, Chinese Academy of Sciences, Cuangzhou 510640;Petrogenesis of Jiuzihe granites in the core of Dabie Mountains[J];GEOCHIMICA;2000-02
7 WANG Qiang,ZHAO Zhen-hua,XIONG Xia o-lin,XU Ji-feng (Guangzhou Institute of Geochemistr y,Chinese Academy of Sciences,Guangzhou510640,China);Melting of the underplated basaltic lower crust:Evidence from the Shaxi adakitic sodic quartz diorite-porphyrites,Anhui Province,China[J];Geochimica;2001-04
8 Li Wuping 1,2 , Wang Tao 3, Wang Xiaoxia 2 (1.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou510640, China; 2.Department of Earth Science, Chang’an University, Xi’an710054, China; 3.Department of Geology , Peiking;SOURCE OF HUICHIZI GRANITOID COMPLEX PLUTON IN NORTHERN QINLING,CENTRAL CHINA: CONSTRAINED IN ELEMENT AND ISOTOPIC GEOCHEMISTRY[J];;2001-03
9 Li Guangming(Chengdu Institute of Geology and Mineral Resources, Chengdu 610082);PETROLOGIC FEATURES AND GENESIS OF CENOZOIC VOLCANIC ROCKS, QIANGTANG AREA,NORTHERN TIBETAN PLATEAU[J];GEOLOGY-GEOCHEMISTRY;2000-02
10 Liu Yongsheng Gao Shan (Faculty of Earth Sciences,China University of Geosciences,Wuhan,430074);ANATEXIS OF THE CONTINENTAL CRUST AND GRANITES AS TRACERS OF LOWER CRUSTAL COMPOSITION[J];GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION;1998-03
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