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Metamorphic P-T-t paths of pelitic granulites of the Taihua metamorphic complex in the Mts. Huashan area and tectonothermal implications for the Palaeoproterozoic Trans-North China Orogen

文献类型：期刊论文

作者Wang, Guo-Dong1,2; Wang, Hao Y. C.2; Chen, Hong-Xu2; Lu, Jun-Sheng3; Zhang, Bo4; Van Tho Pham2; Zhang, Ji-Jun5; Zhang, Qing6; Wu, Chun-Ming2
刊名PRECAMBRIAN RESEARCH
出版日期2017-03-01
卷号290页码:147-162
关键词Pelitic Granulites Taihua Metamorphic Complex Metamorphic P-t-t Path North China Craton
ISSN号0301-9268
DOI10.1016/j.precamres.2016.12.008
文献子类Article
英文摘要Metamorphic evolution and geochronology of pelitic granulites were reported for the first time in the Taihua metamorphic complex, Mts. Huashan area, southern segment of the trans-North China Orogen (TNCO). Three generations of metamorphic mineral assemblages are recognized: (1) the prograde metamorphic mineral assemblages (M-1) are represented by mineral inclusions within the garnet porphyroblasts; (2) the metamorphic peak assemblage (M-2) are the garnet porphyroblasts and minerals in the matrix (biotite + orthopyroxene + plagioclase + quartz + I(-feldspar + ilmenite + zircon + magnetite); and (3) the retrograde metamorphic mineral assemblages (M-3) are represented by the symplectic assemblages around the garnet porphyroblasts, resulted from decomposition reactions between garnet rims and neighboring minerals in the matrix. Calculated by both conventional thermobarometry and pseudo section modeling in the NCKFMASHT system using the Perple_X technique, the P-T conditions of these three metamorphic stages are constrained to be of 4-5 kbar/520-530 degrees C for the M1 stage, 6.88.6 kbar/730-810 degrees C for the M-2 stage and 4.1-6.4 kbar/570-740 degrees C for the M3 stage, respectively. The derived clockwise P-T paths imply that the Mts. Huashan terrane involved in the subduction and subsequent collision between the Eastern and Western Blocks of the North China Craton (NCC) along the Palaeoproterozoic Trans-North China Orogen (TNCO). High resolution SIMS U-Pb dating of metamorphic zircons reveals the metamorphic ages of 1.85-1.82 Ga. Combined with geochronological data from the literature, it is concluded that the tectonothermal evolution between the Eastern and Western Blocks started as early as similar to 1.97 Ga and lasted as late as 1.80 Ga. Furthermore, the eastern Taihua complex records older metamorphic ages and higher peak metamorphic pressures than those of the western Taihua complex, possibly suggesting an eastward subduction model for the TNCO. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词HIGH-PRESSURE GRANULITES ; PALEOPROTEROZOIC TECTONIC EVOLUTION ; TEMPERATURE-TIME PATHS ; U-PB ; ZIRCON GEOCHRONOLOGY ; HENGSHAN COMPLEX ; HENAN PROVINCE ; SANGGAN AREA ; CENTRAL ZONE ; LITHOTECTONIC ELEMENTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000394475100010
出版者ELSEVIER SCIENCE BV
资助机构National Natural Science Foundation of China(41225007 ; 40872125 ; 41130314) ; National Natural Science Foundation of China(41225007 ; 40872125 ; 41130314) ; National Natural Science Foundation of China(41225007 ; 40872125 ; 41130314) ; National Natural Science Foundation of China(41225007 ; 40872125 ; 41130314)
源URL[http://ir.iggcas.ac.cn/handle/132A11/52983]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Wang, Guo-Dong
作者单位1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth Sci, POB 4588, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
4.China Corp Coal Geol Engn, Beijing 100040, Peoples R China
5.Shaanxi Ctr Geol Survey, Xian 710068, Peoples R China
6.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Guo-Dong,Wang, Hao Y. C.,Chen, Hong-Xu,et al. Metamorphic P-T-t paths of pelitic granulites of the Taihua metamorphic complex in the Mts. Huashan area and tectonothermal implications for the Palaeoproterozoic Trans-North China Orogen[J]. PRECAMBRIAN RESEARCH,2017,290:147-162.
APA Wang, Guo-Dong.,Wang, Hao Y. C..,Chen, Hong-Xu.,Lu, Jun-Sheng.,Zhang, Bo.,...&Wu, Chun-Ming.(2017).Metamorphic P-T-t paths of pelitic granulites of the Taihua metamorphic complex in the Mts. Huashan area and tectonothermal implications for the Palaeoproterozoic Trans-North China Orogen.PRECAMBRIAN RESEARCH,290,147-162.
MLA Wang, Guo-Dong,et al."Metamorphic P-T-t paths of pelitic granulites of the Taihua metamorphic complex in the Mts. Huashan area and tectonothermal implications for the Palaeoproterozoic Trans-North China Orogen".PRECAMBRIAN RESEARCH 290(2017):147-162.

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来源：地质与地球物理研究所

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