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  4. 岩石圈演化国家重点实验室
CONTRASTING STYLES OF PERALUMINOUS S-TYPE AND I-TYPE GRANITIC MAGMATISM: IDENTIFICATION AND IMPLICATIONS FOR THE ACCRETIONARY HISTORY OF THE CHINESE SOUTH TIANSHAN

文献类型：期刊论文

作者Tao, Zaili2,3; Yin, Jiyuan2,5; Xia, Wenjiao4,6; Seltmann, Reimar7; Chen, Wen2; Sun, Min5; Wang, Tao2; Yuan, Chao8; Thomson, Stuart N.1; Chen, Yuelong3
刊名AMERICAN JOURNAL OF SCIENCE
出版日期2022-02-01
卷号322期号:2页码:280-312
关键词Peraluminous granitoids South Tianshan Orogen Belt Metasedimentary rocks Slab roll-back
ISSN号0002-9599
DOI10.2475/02.2022.06
英文摘要Peraluminous granitoids have aluminum saturation indices (A/CNK) higher than 1.0, which overlap to some extent between S- and I-type granitoids. However, their source and petrogenesis are still disputed. For example, whole-rock compositions alone are not always a valid way to discriminate the sources of peraluminous granitoids. To identify the geochemical affinities, source and petrogenesis of the peraluminous granitoids, we present new geochemical data, in situ zircon U-Pb ages and Hf-O isotopic data, and whole-rock Sr-Nd isotopic data for the peraluminous granitoids in the South Tianshan Orogen Belt (STOB), Northwesten China. Zircon U-Pb ages suggest that these peraluminous granitoids were emplaced in the latest Carboniferous (ca. 299 Ma). They contain the diagnostic mineral muscovite and have high delta O-18(Zrn) values (>8.0 %) demonstrating a close affinity with S-type granitoids. Their low epsilon Nd(t) values (-5.3 to -7.6), combined with variable zircon epsilon Hf(t) values (-0.35 to -10.18), indicate that these S-type granitoids were likely derived from partial melting of metasedimentary rocks. In addition, inherited zircon cores from the S-type granitoids have variable delta O-18 values (6.34-10.5 %) and zircon epsilon Hf(t) values (-4.3 to +16.3), with age populations (ca. 400 to 500 Ma) similar to those of detrital zircons from late Carboniferous metasedimentary rocks in the region. These data show that the S-type granitoids were dominantly derived from late Carboniferous metasedimentary rocks rather than Precambrian crustal materials. The studied granitoids have a transitional composition between I- and S-type granitoids, which could be related to low compositional maturity of the late Carboniferous metasedimentary source. According to the spatial and temporal distribution and petrogenesis of the Carboniferous intrusive rocks in the STOB, we propose that a slab rollback model can account for the generation of late Carboniferous S-type granitoids in the STOB.
WOS关键词ASIAN OROGENIC BELT ; A-TYPE GRANITES ; PALEOZOIC TECTONIC EVOLUTION ; U-PB GEOCHRONOLOGY ; HF-O ISOTOPES ; WESTERN TIANSHAN ; CRUSTAL GROWTH ; TIEN-SHAN ; NW CHINA ; FRACTIONAL CRYSTALLIZATION
资助项目National Key R&D 445 Program of China[2017YFC0601206] ; National Science Foundation of China[41888101] ; National Science Foundation of China[41822204] ; National Science Foundation of China[41830216] ; National Science Foundation of China[41873060] ; National Key Research and Development Project "Key scientific issues of transformative technology"[2019YFA0708601] ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources[J1901-5] ; China Geological Survey[DD20221649] ; Hong Kong RGC grants[17303415] ; Hong Kong RGC grants[17302317] ; Natural Environment Research Council[NE/P017452/1]
WOS研究方向Geology
语种英语
WOS记录号WOS:000800658900004
出版者AMER JOURNAL SCIENCE
资助机构National Key R&D 445 Program of China ; National Key R&D 445 Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Key Research and Development Project "Key scientific issues of transformative technology" ; National Key Research and Development Project "Key scientific issues of transformative technology" ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; China Geological Survey ; China Geological Survey ; Hong Kong RGC grants ; Hong Kong RGC grants ; Natural Environment Research Council ; Natural Environment Research Council ; National Key R&D 445 Program of China ; National Key R&D 445 Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Key Research and Development Project "Key scientific issues of transformative technology" ; National Key Research and Development Project "Key scientific issues of transformative technology" ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; China Geological Survey ; China Geological Survey ; Hong Kong RGC grants ; Hong Kong RGC grants ; Natural Environment Research Council ; Natural Environment Research Council ; National Key R&D 445 Program of China ; National Key R&D 445 Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Key Research and Development Project "Key scientific issues of transformative technology" ; National Key Research and Development Project "Key scientific issues of transformative technology" ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; China Geological Survey ; China Geological Survey ; Hong Kong RGC grants ; Hong Kong RGC grants ; Natural Environment Research Council ; Natural Environment Research Council ; National Key R&D 445 Program of China ; National Key R&D 445 Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Key Research and Development Project "Key scientific issues of transformative technology" ; National Key Research and Development Project "Key scientific issues of transformative technology" ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources ; China Geological Survey ; China Geological Survey ; Hong Kong RGC grants ; Hong Kong RGC grants ; Natural Environment Research Council ; Natural Environment Research Council
源URL[http://ir.iggcas.ac.cn/handle/132A11/106018]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Yin, Jiyuan
作者单位1.Univ Arizona, Dept Geosci, 1040 E 4th St, Tucson, AZ 85721 USA
2.Chinese Acad Geol Sci, Inst Geol, Minist Nat Resources, Key Lab Deep Earth Dynam, Beijing 100037, Peoples R China
3.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.Univ Hong Kong, Dept Earth Sci, Pokflam Rd, Hong Kong, Peoples R China
6.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
7.Nat Hist Museum, Dept Earth Sci, Ctr Russian & Cent EurAsian Mineral Studies CERCA, London SW7 5BD, England
8.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
推荐引用方式
GB/T 7714		 Tao, Zaili,Yin, Jiyuan,Xia, Wenjiao,et al. CONTRASTING STYLES OF PERALUMINOUS S-TYPE AND I-TYPE GRANITIC MAGMATISM: IDENTIFICATION AND IMPLICATIONS FOR THE ACCRETIONARY HISTORY OF THE CHINESE SOUTH TIANSHAN[J]. AMERICAN JOURNAL OF SCIENCE,2022,322(2):280-312.
APA Tao, Zaili.,Yin, Jiyuan.,Xia, Wenjiao.,Seltmann, Reimar.,Chen, Wen.,...&Xia, Xiaoping.(2022).CONTRASTING STYLES OF PERALUMINOUS S-TYPE AND I-TYPE GRANITIC MAGMATISM: IDENTIFICATION AND IMPLICATIONS FOR THE ACCRETIONARY HISTORY OF THE CHINESE SOUTH TIANSHAN.AMERICAN JOURNAL OF SCIENCE,322(2),280-312.
MLA Tao, Zaili,et al."CONTRASTING STYLES OF PERALUMINOUS S-TYPE AND I-TYPE GRANITIC MAGMATISM: IDENTIFICATION AND IMPLICATIONS FOR THE ACCRETIONARY HISTORY OF THE CHINESE SOUTH TIANSHAN".AMERICAN JOURNAL OF SCIENCE 322.2(2022):280-312.

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来源：地质与地球物理研究所

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