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Late Jurassic Sn metallogeny in eastern Guangdong, SE China coast: Evidence from geochronology, geochemistry and Sr–Nd–Hf–S isotopes of the Dadaoshan Sn deposit
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TLDR
The Dadaoshan Sn deposit is located in the eastern Guangdong Sn-W province, coastal SE China as mentioned in this paper, and the porphyritic granite was LA-ICP-MS zircon U-Pb dated to be 153.2±1.2About:
This article is published in Ore Geology Reviews.The article was published on 2017-04-01. It has received 29 citations till now. The article focuses on the topics: Porphyritic & Zircon.read more
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The great Yanshanian metallogenic event of eastern Asia: Consequences from one hundred million years of plate margin geodynamics
TL;DR: Yanshanian metallogeny of eastern Asia was dominantly controlled by oblique subduction and rollback of the Izanagi plate, and also, more locally in the north, by closure of the Mudanjiang Ocean basin and accretion of the Bureya-Jiamusi-Khanka block and the Sikhote-Alin terranes as discussed by the authors.
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Formation and geodynamic implication of the Early Yanshanian granites associated with W–Sn mineralization in the Nanling range, South China: an overview
Jingya Cao,Xiaoyong Yang,Jianguo Du,Qian-Hong Wu,Hua Kong,Huan Li,Qiu Wan,Xiao-Shuang Xi,Yushuang Gong,Huarong Zhao +9 more
TL;DR: The Nanling range (Nanling) is characterized by intense and widespread Mesozoic magmatism related large-scale W-Sn mineralization as discussed by the authors, which is a summary of geochemistry, geochronology, and petrogenesis for the...
Journal Article
Granites of southeast Asian tin belt
TL;DR: In this paper, the essential granite geology of the southeast Asian tin belt, distinguishing plutons within batholiths and characterizing them by their component units, field relationships, lithology, texture, petrology, geochemistry, geochronology, and mineral potential are established.
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Geochronology, Petrology, and Genesis of Two Granitic Plutons of the Xianghualing Ore Field in South Hunan Province: Constraints from Zircon U–Pb Dating, Geochemistry, and Lu–Hf Isotopic Compositions
TL;DR: The Laiziling and Jianfengling plutons are composed of medium-to coarse-grained two-mica and coarsegrained biotite granites, respectively, and have zircon U-Pb ages of 156.4 ± 1.4 Ma and 165.2 ± 1 4 Ma, respectively as discussed by the authors.
Journal ArticleDOI
Origin of Early Cretaceous A-type granite and related Sn mineralization in the Sanjiaowo deposit, eastern Guangdong, SE China and its tectonic implication
Qing-He Yan,Qing-He Yan,He Wang,Zeng-Wang Qiu,Xiao-Peng Wei,Pei Li,Rui Dong,Xiao-Yu Zhang,Kailin Zhou +8 more
TL;DR: Zhang et al. as discussed by the authors suggested that the Sanjiaowo Granite porphyry belongs to the A2-subtype and were formed by partial melting of a crustal source of Mesoproterozoic overall residence age with minor input of mantle materials.
References
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Chemical and isotopic systematics of oceanic basalt : implications for mantle composition and processes
TL;DR: In this article, trace-element data for mid-ocean ridge basalts and ocean island basalts are used to formulate chemical systematics for oceanic basalts, interpreted in terms of partial-melting conditions, variations in residual mineralogy, involvement of subducted sediment, recycling of oceanic lithosphere and processes within the low velocity zone.
Journal ArticleDOI
Chemical and isotopic systematics of oceanic basalts. Implications for Mantle Composition and Processes
The continental crust: Its composition and evolution
TL;DR: In this paper, the authors describe the composition of the present upper crust and deal with possible compositions for the total crust and the inferred composition of lower crust, and the question of the uniformity of crustal composition throughout geological time is discussed.
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Trace element discrimination diagrams for the tectonic interpretation of granitic rocks
TL;DR: In this article, a data bank containing over 600 high quality trace element analyses of granites from known settings was used to demonstrate using ORG-normalized geochemical patterns and element-SiO2 plots that most of these granite groups exhibit distinctive trace element characteristics.
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