Data for: Redox reactions control Cu and Fe isotope fractionation in a magmatic Ni-Cu mineralization system

Main Author: Xue, Chunji
Format: Dataset
Terbitan: Mendeley , 2020
Subjects:
Online Access: https:/data.mendeley.com/datasets/z464c5nfty
ctrlnum 0.17632-z464c5nfty.1
fullrecord <?xml version="1.0"?> <dc><creator>Xue, Chunji</creator><title>Data for: Redox reactions control Cu and Fe isotope fractionation in a magmatic Ni-Cu mineralization system</title><publisher>Mendeley</publisher><description>Copper and Fe are redox-sensitive metals, and their isotopic compositions may potentially record changes of oxidation conditions in high-temperature magmatic Ni&#x2013;Cu mineralization systems. High-precision Cu and Fe isotope data for sulfides (chalcopyrite) and whole-rock samples of the Tulaergen magmatic Ni&#x2013;Cu system (NW China) were analyzed to evaluate redox-induced fractionation during segregation of sulfide melt from silicate melt and internal fractionation within segregated sulfide melt. Table 1 Chalcophile elements (PGE, Cu, and Ni) and S contents of whole-rock samples from the Tulaergen deposit. Table 2 Copper and Fe isotopic compositions and Cu/Fe ratios of chalcopyrite separates, and whole-rock Fe isotopic compositions from the Tulaergen magmatic Ni&#x2013;Cu mineralization system. </description><subject>Isotope</subject><type>Other:Dataset</type><identifier>10.17632/z464c5nfty.1</identifier><rights>Attribution-NonCommercial 3.0 Unported</rights><rights>https://creativecommons.org/licenses/by-nc/3.0</rights><relation>https:/data.mendeley.com/datasets/z464c5nfty</relation><date>2020-03-24T01:52:19Z</date><recordID>0.17632-z464c5nfty.1</recordID></dc>
format Other:Dataset
Other
author Xue, Chunji
title Data for: Redox reactions control Cu and Fe isotope fractionation in a magmatic Ni-Cu mineralization system
publisher Mendeley
publishDate 2020
topic Isotope
url https:/data.mendeley.com/datasets/z464c5nfty
contents Copper and Fe are redox-sensitive metals, and their isotopic compositions may potentially record changes of oxidation conditions in high-temperature magmatic Ni–Cu mineralization systems. High-precision Cu and Fe isotope data for sulfides (chalcopyrite) and whole-rock samples of the Tulaergen magmatic Ni–Cu system (NW China) were analyzed to evaluate redox-induced fractionation during segregation of sulfide melt from silicate melt and internal fractionation within segregated sulfide melt. Table 1 Chalcophile elements (PGE, Cu, and Ni) and S contents of whole-rock samples from the Tulaergen deposit. Table 2 Copper and Fe isotopic compositions and Cu/Fe ratios of chalcopyrite separates, and whole-rock Fe isotopic compositions from the Tulaergen magmatic Ni–Cu mineralization system.
id IOS7969.0.17632-z464c5nfty.1
institution Universitas Islam Indragiri
affiliation onesearch.perpusnas.go.id
institution_id 804
institution_type library:university
library
library Teknologi Pangan UNISI
library_id 2816
collection Artikel mulono
repository_id 7969
city INDRAGIRI HILIR
province RIAU
shared_to_ipusnas_str 1
repoId IOS7969
first_indexed 2020-04-08T08:19:07Z
last_indexed 2020-04-08T08:19:07Z
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