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Open AccessJournal ArticleDOI

Constraints on the uptake of REE by scheelite in the Baoshan tungsten skarn deposit, South China

TLDR
In this article, the scheelite was classified into three types: prograde, retrograde, and semi-retrograde skarns, and the lattice strain model was used to estimate the relative distribution of rare earth element (REE) in scheelites and to predict the relative distributions of REE in the ore-forming fluids.
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This article is published in Chemical Geology.The article was published on 2018-01-20 and is currently open access. It has received 66 citations till now. The article focuses on the topics: Scheelite & Tungsten.

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In-situ LA-ICP-MS trace element analyses of scheelite and wolframite: Constraints on the genesis of veinlet-disseminated and vein-type tungsten deposits, South China

TL;DR: Wang et al. as discussed by the authors conducted in-situ laser ablation-inductively coupled plasma-mass spectrometry trace element analyses to understand the origin and processes of tungsten mineralization.
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Trace element composition of scheelite in orogenic gold deposits

TL;DR: Scheelite from 25 representative orogenic gold deposits from various geological settings was investigated by EPMA (electron probe micro-analyzer) and LA-ICP-MS (laser ablation-inductively coupled plasma mass spectrometer) to establish discriminant geochemical features to constrain indicator mineral surveys for gold exploration as discussed by the authors.
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Origin of the Muguayuan veinlet-disseminated tungsten deposit, South China: Constraints from in-situ trace element analyses of scheelite

TL;DR: The late Triassic Muguayuan W deposit is located in the middle of the Jiangnan Orogen, South China as mentioned in this paper, which is characterized by veinlet-disseminated W mineralization that developed in the Sanxianba granitic porphyry stock.
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Comparative geochemical study of scheelite from the Shizhuyuan and Xianglushan tungsten skarn deposits, South China: Implications for scheelite mineralization

TL;DR: The Shizhuyuan and the Xianglushan world-class W deposits from the Nanling W-Sn region and Jiangnan W belt, respectively, were analyzed in this article.
References
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Journal ArticleDOI

Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides

TL;DR: The effective ionic radii of Shannon & Prewitt [Acta Cryst. (1969), B25, 925-945] are revised to include more unusual oxidation states and coordinations as mentioned in this paper.
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The composition of the Earth

TL;DR: In this paper, the authors compared the relative abundances of the refractory elements in carbonaceous, ordinary, and enstatite chondritic meteorites and found that the most consistent composition of the Earth's core is derived from the seismic profile and its interpretation, compared with primitive meteorites, and chemical and petrological models of peridotite-basalt melting relationships.
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In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard

TL;DR: In this paper, an internal standard-independent calibration strategy for LA-ICP-MS analysis of anhydrous minerals and glasses was described, where the ablation yield correction factor (AYCF) was used to correct the matrix-dependent absolute amount of materials ablated during each run.
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Continental and Oceanic Crust Recycling-induced Melt^Peridotite Interactions in the Trans-North China Orogen: U^Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths

TL;DR: In this article, the first finding of continental crust-derived Precambrian zircons in garnet/spinel pyroxenite veins within mantle xenoliths carried by the Neogene Hannuoba basalt in the central zone of the North China Craton (NCC).
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Petrogenesis of Mesozoic granitoids and volcanic rocks in south China : a response to tectonic evolution.

TL;DR: In this paper, the authors proposed that these rocks were formed in time and space as a response to regional tectonic regime change from the continent-continent collision of the Indosinian orogeny within the broad Tethyan orogenic domain in the Early Mesozoic (T1-T3) (Period I) to the largely extensional setting as a result of the Yanshanian Orogeny genetically associated with the NW-WNW-ward subduction of the paleo-Pacific oceanic lithosphere in the Late Mesozooric (J
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