中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Petrogeochemical characteristics of the Paleoproterozoic high-pressure mafic granulite and calc-silicate from the Nanshankou of the Jiaobei terrane

文献类型:期刊论文

作者Li XuPing1; Liu Yun1; Guo JingHui2; Li HongKui3,4; Zhao GuoChun5
刊名ACTA PETROLOGICA SINICA
出版日期2013-07-01
卷号29期号:7页码:2340-2352
关键词Hp Mafic Granulite Calc-silicate Geochemistry Nanshankou Jiaobei Terrane
文献子类Article
英文摘要The Paleoproterozoic HP mafic granulite and cab-silicate were found from Laixi, Jiaobei terrane, consisting of almandine dominated garnet-augite-ferrohypersthene and grossular-zoisite-prehnite-albite respectively. Mineralogical and petrological studies show that the calc-silicate formed after the HP mafic granulite by processes combined retrogressive metamorphism with Ca alteration. The HP mafic granulites records four stage geological processes, including pre-granulite facies, peak granulite facies, retrogressive combined with Ca alteration and complete Ca alteration processes with mineral assemblages as Cpx + Pl + Qtz (M-1), Grt + Cpx + Rt + Qtz (M-2), Cpx + Pl + Opx + Ilm + Mgt + Ep (M-3) and Grs + Zo + Prh + Ab + Cal (M-4). The HP mafic granulite is rich in LIL elements Ba, Rb, K, Rh, Th and depleted in HFS elements Nb, Zr, Ti and Y, having LREE rich right-inclined REE pattern and showing island-arc basaltic characteristics. Further studies by using discrimination diagrams, the HP mafic granulite presents island-arc tholeiitic characteristics, probably formed in the back-arc extension tectonic setting. After formation of the mafic rock, it experienced granulitic facies metamorphism during collisional convergence of the Jiao-Liao-Ji orogenic belt and afterwards experienced retrogressive and Ca alteration processes during the lift of the belt.
WOS关键词NORTH CHINA CRATON ; LIAO-JI BELT ; PB ZIRCON GEOCHRONOLOGY ; U-TH-PB ; TECTONIC IMPLICATIONS ; KEY ISSUES ; METAMORPHIC EVOLUTION ; SHANDONG PENINSULA ; PELITIC GRANULITES ; EASTERN SHANDONG
WOS研究方向Geology
语种英语
WOS记录号WOS:000322926000006
源URL[http://ir.iggcas.ac.cn/handle/132A11/62654]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位1.Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Shandong Inst, Jinan 250013, Peoples R China
4.Lab Geol Sci, Jinan 250013, Peoples R China
5.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
推荐引用方式
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Li XuPing,Liu Yun,Guo JingHui,et al. Petrogeochemical characteristics of the Paleoproterozoic high-pressure mafic granulite and calc-silicate from the Nanshankou of the Jiaobei terrane[J]. ACTA PETROLOGICA SINICA,2013,29(7):2340-2352.
APA Li XuPing,Liu Yun,Guo JingHui,Li HongKui,&Zhao GuoChun.(2013).Petrogeochemical characteristics of the Paleoproterozoic high-pressure mafic granulite and calc-silicate from the Nanshankou of the Jiaobei terrane.ACTA PETROLOGICA SINICA,29(7),2340-2352.
MLA Li XuPing,et al."Petrogeochemical characteristics of the Paleoproterozoic high-pressure mafic granulite and calc-silicate from the Nanshankou of the Jiaobei terrane".ACTA PETROLOGICA SINICA 29.7(2013):2340-2352.

入库方式: OAI收割

来源:地质与地球物理研究所

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