Petrogenesis and evolution of late Mesozoic granitic magmatism in the;Hohhot metamorphic core complex, Daqing Shan, North China
Guo, Lei6; Wang, Tao; Castro, Antonio; Zhang, Jinjiang; Liu, Jiang; Li, Jianbo
刊名INTERNATIONAL GEOLOGY REVIEW
2012
卷号54期号:16页码:1885-1905
关键词late Mesozoic contraction late Mesozoic extension granitic magmatism deep-crust partial fusion shallow-crust partial fusion granitoid geochemistry Sr-Nd-Hf isotopes
ISSN号019AG
英文摘要Late Mesozoic granitoid plutons of four distinct ages intrude the lower plate of the Hohhot metamorphic core complex along the northern margin of the North China craton. The plutons belong to two main groups: (1) Group I, deformed granitoids (148 and 140 Ma subgroups) with high Sr, LREE, and Na2O, low Y and Yb contents, high Sr/Y and La/Yb ratios, weak or no Eu anomalies, low Rb/Ba ratios, similar initial Sr-87/Sr-86 values (0.7064-0.7071) and low Mg-# (<37 mostly, 100 x molar MgO/MgO + FeOt); (2) Group II, non-deformed granitoids (132 and 114 Ma subgroups) with low Sr, relatively low Na2O, high Y and Yb contents, pronounced negative Eu anomalies, high Rb/Ba ratios, and initial Sr-87/Sr-86 values (0.7098-0.7161). The two groups share geochemical similarities in epsilon(Nd)(t) (-11.3 to -15.4) and T-DM2 ages (1.85-2.18 thousand million years) as well as Hf isotopic ratios in zircons. Geochemical modelling (using the MELTS code) suggests that similar sources but different depths of magma generation produced the early, high-pressure low-Mg adakitic granitoids and late, low-pressure granitoids with A-type characteristics. The early granitoids likely represent a partially melted, deep-seated, thickened lower continental crust that involved a minor contribution from young materials, whereas the later group partially melted at shallower depths. This granitic magmatic evolution coincided with the tectonic transition from crustal contraction to extension.
学科主题火成岩岩石学
WOS关键词THICKENED CONTINENTAL-CRUST ; EARLY CRETACEOUS GRANITOIDS ; PB ZIRCON ; GEOCHRONOLOGY ; CU-AU MINERALIZATION ; U-PB ; INNER-MONGOLIA ; EASTERN ; CHINA ; DABIE OROGEN ; EXTENSIONAL TECTONICS ; TRACE-ELEMENT
WOS研究方向Geology
语种英语
出版者The authors thank Drs Ying Tong, Lei Zhang, and Bo Zhang for their;fruitful discussion and research cooperation. They are grateful to;Professor Hegner for the isotopic composition analytical work, and for;the geochemical data analytical work of Acme Analytical Laboratories;Ltd. (Vancouver, BC, Canada), and for the Hf isotopic data analytical;work of the Institute of Mineral Resources, Chinese Academy of;Geological Sciences. The work was supported by the National Natural;Science Foundation of China (NSFC grants 41002073, 90714006, and;91114206), the Basic Research Fund of the Institute of Geology, Chinese;Academy of Geological Sciences (project No. J0913), SinoProbe-08-01-03;and the China Geological Survey Project (1212011085474, 1212011120135,;and 1212010811033).
WOS记录号WOS:000309708700003
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/39852]  
专题中国地质调查局西安地质调查中心
作者单位1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China.
2.Chinese Acad Geol Sci, Key Lab Earthprobe & Geodynam, Beijing 100037, Peoples R China.
3.Univ Huelva, Dept Geol, Huelva 21071, Spain.
4.Peking Univ, Sch Earth & Space Sci, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China.
5.E China Inst Technol, Fuzhou 344000, Jiangxi, Peoples R China.
6.中国地质科学院地质研究所
推荐引用方式
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Guo, Lei,Wang, Tao,Castro, Antonio,et al. Petrogenesis and evolution of late Mesozoic granitic magmatism in the;Hohhot metamorphic core complex, Daqing Shan, North China[J]. INTERNATIONAL GEOLOGY REVIEW,2012,54(16):1885-1905.
APA Guo, Lei,Wang, Tao,Castro, Antonio,Zhang, Jinjiang,Liu, Jiang,&Li, Jianbo.(2012).Petrogenesis and evolution of late Mesozoic granitic magmatism in the;Hohhot metamorphic core complex, Daqing Shan, North China.INTERNATIONAL GEOLOGY REVIEW,54(16),1885-1905.
MLA Guo, Lei,et al."Petrogenesis and evolution of late Mesozoic granitic magmatism in the;Hohhot metamorphic core complex, Daqing Shan, North China".INTERNATIONAL GEOLOGY REVIEW 54.16(2012):1885-1905.
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