Porphyry Cu systems
斑岩铜矿系统How collision and post-collision processes reorganize mantle and lower-crustal materials to produce fertile magmas.
关注碰撞—后碰撞过程中地幔与下地壳物质的再活化,以及成矿岩浆的形成机制。
Geology · Ore deposits · Geochemistry
I am Yiwei Zhou (James / 周怿惟), a PhD candidate in geology studying porphyry copper systems, halogen geochemistry, and mineral-scale records of magmatic evolution.
我是周怿惟,地质学博士研究生,主要研究斑岩铜矿系统、卤素地球化学与矿物尺度的岩浆演化记录。
My work connects economic geology with analytical geochemistry. I am interested in how deep material recycling, crust–mantle interaction, and magma reservoir processes control volatile budgets and the fertility of porphyry systems.
我的研究连接矿床地质学与分析地球化学,重点关注深部物质循环、壳幔相互作用和岩浆储库过程如何控制挥发分收支及斑岩系统的成矿潜力。
CURRENTPhD Candidate, School of Earth and Space Sciences, Peking University
RESEARCH BASEInstitute of Geology, Chinese Academy of Geological Sciences
BASED INBeijing, China
From tectonic inheritance to the analytical signal, each scale helps explain why some magmas become ore-forming systems.
How collision and post-collision processes reorganize mantle and lower-crustal materials to produce fertile magmas.
关注碰撞—后碰撞过程中地幔与下地壳物质的再活化,以及成矿岩浆的形成机制。
Using F–Cl–Br–I systematics to trace volatile sources, magma evolution, degassing, and fluid transfer.
利用 F–Cl–Br–I 体系示踪挥发分来源、岩浆演化、脱气与流体迁移。
Reading apatite and other minerals as time-resolved records of magma storage and magmatic–hydrothermal transition.
以磷灰石等矿物记录解析岩浆储库演化及岩浆—热液转换过程。
Developing robust methods for low-abundance volatile elements in geological materials, including multi-halogen analysis.
开发地质样品中低丰度挥发性元素的可靠分析方法,包括多卤素联合测定。
Selected peer-reviewed studies spanning porphyry systems, critical elements, and volatile cycling.
Manuscripts under review are intentionally not listed as publications.
Contact · 联系
I welcome conversations about porphyry systems, halogen analysis, apatite geochemistry, and related collaborations.
geoyiwei@gmail.com ↗