Trace element fractionation in magnetite as a function of Fe depletion from ore fluids at the Baijian Fe-(Co) skarn deposit, eastern China: Implications for Co …

G Wen, JW Li, AH Hofstra, DE Harlov, XF Zhao… - American …, 2024 - degruyter.com
Magnetite is common in various magmatic and hydrothermal ore deposit types, and its trace
element geochemistry has become increasingly used in ore genesis studies and mineral …

[HTML][HTML] Tectonic setting, mineralization, and ore geochemistry of the Paleozoic IOCG deposits in Xinjiang, NW China

S Zhang, L Zhao, P Liang, H Jiang, W Zhang - Ore Geology Reviews, 2024 - Elsevier
The Paleozoic iron oxide copper–gold (IOCG) deposits in Xinjiang correspond to magmatic
arc formations (Andean type) within the Central Asian Orogenic Belt (CAOB). These deposits …

[HTML][HTML] 柴北缘青山造山型金-铅矿床成矿机制: 矿石和黄铁矿组成约束

张志超, 龙灵利, 杨立强, 王玉往, 祝新友, 童海奎… - 岩石学报, 2024 - dzkx.org
青山金铅矿床位于柴北缘滩间山矿集区内, 是全球罕见的金-铅共/伴生的造山型矿床.
矿体主要赋存于古元古代达肯大坂群片岩中, 受到北西西向断裂控制, 发育蚀变岩和石英脉两种 …

Magnetite Texture and Geochemistry in the Takab Ore Deposit (NW Iran): Implications for a Complex Hydrothermal Evolution

C Wagner, O Boudouma, N Rividi, B Orberger… - Minerals, 2025 - mdpi.com
The massive magnetite deposit from Takab (NW Iran) is hosted in amphibolite layers
intercalated with the chemical and terrigenous sediments of the Takab BIF. A …