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–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.
</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 |
| recordtype |
dc |
| _version_ |
1686587542279815168 |
| score |
17.204819 |