The construction mechanism of the Neoproterozoic S-type Sanfang-Yuanbaoshan granitic plutons in the Jiangnan Orogenic Belt, South China: Insights from geological observation, geochronology, AMS and Bouguer gravity modeling

被引:10
作者
Yan, Chaolei [1 ,2 ,3 ]
Shu, Liangshu [1 ]
Chen, Yan [2 ]
Faure, Michel [2 ]
Feng, Zuohai [4 ,5 ]
Zhai, Mingguo [3 ,6 ]
机构
[1] Nanjing Univ, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China
[2] Univ Orleans, ISTO, BRGM, CNRS,UMR 7327, F-45071 Orleans, France
[3] Univ Chinese Acad Sci, Key Lab Computat Geodynam, Beijing 100049, Peoples R China
[4] Guilin Univ Technol, Coll Earth Sci, Guilin 541004, Guangxi, Peoples R China
[5] Guilin Univ Technol, Guangxi Key Lab Hidden Metall Ore Deposits Explor, Guilin 541004, Guangxi, Peoples R China
[6] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
基金
中国国家自然科学基金; 国家重点研发计划; 国家自然科学基金重大项目;
关键词
South China; Jiangnan Orogenic Belt; Neoproterozoic S-type granite; Anisotropy of magnetic susceptibility; Bouguer gravity modeling;
D O I
10.1016/j.precamres.2020.106054
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Neoproterozoic S-type granitic plutons, distributed along the suture zone of the Yangtze and Cathaysia blocks, play an important role in the tectonic evolution of the Jiangnan Orogeny. However, few studies had focused on the scientific issues on the physical construction process of these plutons, therefore, we carried out multidisciplinary approaches on the Sanfang and Yuanbaoshan plutons in the western Jiangan Orogenic Belt to figure out the construction mechanism of these plutons. Zircon Hf and U-Pb dating indicates that the magma, originated from the crustal partial melting, was crystallized at ca. 830 Ma. Field investigation shows that the plutons are dome shaped, and the inclinations of bedding/foliation of the country rocks, the Sibao group, gradually decreases away from the contact zone with pluton boundaries. A top-to-the-E kinematic sense was observed in the eastern margin of the Yuanbaoshan pluton. Both the textural analysis and AMS measurement reveal primary magmatic and secondary general top-to-the-W/NW post-solidus fabrics. The Bouguer gravity modeling reveals that the feeder zone probably locates in the southern part of each pluton and these two plutons are connected at depth. According to the primary magmatic fabric patterns, deep geometric shape as well as structural features of the country rocks, we propose that crustal partial melting magma probably initially intruded into the pre-existing mechanically weak (fold/fault) zone of the Sibao group, and meanwhile laterally and upward accreted to progressively construct the dome-shape plutons. The intrusion of ca. 850-820 Ma S-type granites in the Jiangnan region possibly marked the latest stage of the Jiangnan Orogeny. However, the timing and mechanism of the post-solidus deformation are not well constrained, the proposed interpretations remain hypothetical yet.
引用
收藏
页数:20
相关论文
共 89 条
[1]  
[Anonymous], 2014, QUAL STAND YAO MED M
[2]  
Bgmrh, 1982, REGIONAL GEOLOGY HEB, P1
[3]  
BGMRHN (Bureau of Geology and Mineral Resources of Hunan Province), 1988, REGIONAL GEOLOGY HUN, P6
[4]  
BGMRJX (Bureau of Geology and mineral Resources Jiangxi Province), 1984, REG GEOL JIANGX PROV, P2
[5]  
BGMRZJ (Bureau of Geology and mineral Resources Zhejiang Province), 1989, REG GEOL JIANGX PROV, P5
[6]   The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system [J].
BlichertToft, J ;
Albarede, F .
EARTH AND PLANETARY SCIENCE LETTERS, 1997, 148 (1-2) :243-258
[7]   Tectonic applications of magnetic susceptibility and its anisotropy [J].
Borradaile, GJ ;
Henry, B .
EARTH-SCIENCE REVIEWS, 1997, 42 (1-2) :49-93
[8]   Internal fabrics of the Idaho batholith, USA [J].
Byerly, A. ;
Tikoff, B. ;
Kahn, M. ;
Jicha, B. ;
Gaschnig, R. ;
Fayon, A. K. .
LITHOSPHERE, 2017, 9 (02) :283-298
[9]   Non-Newtonian rheology of crystal-bearing magmas and implications for magma ascent dynamics [J].
Caricchi, Luca ;
Burlini, Luigi ;
Ulmer, Peter ;
Gerya, Taras ;
Vassalli, Melissa ;
Papale, Paolo .
EARTH AND PLANETARY SCIENCE LETTERS, 2007, 264 (3-4) :402-419
[10]   AN EXSOLUTION SILICA-PUMP MODEL FOR THE ORIGIN OF MYRMEKITE [J].
CASTLE, RO ;
LINDSLEY, DH .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1993, 115 (01) :58-65