Porphyry and Skarn Systems: Critical Metal Enrichment, Fluid Evolution and Exploration Implications

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".

Deadline for manuscript submissions: 30 September 2026 | Viewed by 746

Special Issue Editors


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Guest Editor
School of Earth and Planetary Sciences, East China University of Technology, Nanchang 330013, China
Interests: porphyry deposit; geochemistry; mineral exploration; economic geology

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Guest Editor
School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
Interests: skarn deposit; fluid inclusion; economic geology

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Guest Editor
School of Earth Sciences, Lanzhou University, Lanzhou 730000, China
Interests: magmatism; economic geology; low-temperature thermochronology
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Special Issue Information

Dear Colleagues,

Porphyry and skarn deposits are among the Earth’s most important sources of copper, molybdenum, and gold, and are increasingly recognized as vital suppliers of critical metals for renewable energy technologies, such as cobalt, tungsten, lithium, indium, and rhenium. These mineral systems exemplify the dynamic interplay among magmatic–hydrothermal fluids, crustal lithologies, and structural controls. Recent advances in microanalytical geochemistry, experimental modeling, and geophysical exploration call for an integrated reappraisal of metal transport and deposition mechanisms, as well as their implications for future resource targeting.

For this Special Issue, we invite contributions that highlight recent progress in the following areas:

(1) Critical metal enrichment processes, including enrichment mechanisms of energy-related metals (e.g., Cu, Co, Li, REE) in porphyry–skarn environments, and the role of exotic ligands, magmatic redox conditions, and fluid–rock interactions in metal scavenging and ore formation.

(2) Fluid evolution pathways employing isotopic and geochemical tracers to constrain fluid origin and evolution, supported by microthermometry and LA-ICP-MS fluid inclusion analysis, and investigating transitions from magmatic to hydrothermal stages and triggers for metal precipitation.

(3) Exploration innovations, such as novel geochemical vectors, mineralogical indicators, and geophysical signatures for deep targeting, along with machine learning applications in deposit modeling and resource prediction.

(4) Global case studies and modeling based on field investigations of understudied regions and metallogenic belts, and quantitative 3D modeling of ore-forming processes.

(5) Post-mineralization exhumation and preservation conditions, integrating multiple geo-thermochronological techniques to unravel the relationships between ore formation and subsequent post-mineralization modifications, thereby guiding the identification of high-potential exploration targets.

We look forward to receiving your original research and reviews that will help advance our understanding of these complex and economically crucial systems.

Prof. Dr. Chengbiao Leng
Prof. Dr. Qihai Shu
Prof. Dr. Fan Yang
Guest Editors

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Keywords

  • porphyry deposit
  • skarn deposit
  • critical metals
  • fluid inclusions
  • geochemistry
  • metallogenesis
  • mineral explorations

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Published Papers (1 paper)

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Research

23 pages, 19492 KB  
Article
Geochemical Compositions of Zircon and Apatite from the Langdu Intrusions in the Zhongdian Arc: Implications for Porphyry–Skarn Cu Mineralization
by Lei Mo, Chengbiao Leng, Hongze Gao, Kaixuan Li, Xilian Chen, Yanjun Wang, Tao Dong, Wanquan Luo and Haijun Yu
Minerals 2026, 16(4), 413; https://doi.org/10.3390/min16040413 - 16 Apr 2026
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Abstract
The Zhongdian Arc is an important copper polymetallic ore cluster in China’s Sanjiang Tethyan Metallogenic Domain, and the Langdu deposit is a representative porphyry–skarn Cu deposit in this region. This study aims to constrain the timing of magmatic activity at the Langdu deposit. [...] Read more.
The Zhongdian Arc is an important copper polymetallic ore cluster in China’s Sanjiang Tethyan Metallogenic Domain, and the Langdu deposit is a representative porphyry–skarn Cu deposit in this region. This study aims to constrain the timing of magmatic activity at the Langdu deposit. It also seeks to reveal the magma’s physical–chemical properties and evolution, and to identify the factors controlling mineralization. To achieve these objectives, this study used LA-ICP-MS zircon U-Pb dating and elemental analysis, combined with halogen and trace element data from apatite. Zircon U–Pb dating shows that the Langdu intrusions were emplaced at ca. 216 Ma in a continental arc setting associated with the westward subduction of the Garzê–Litang oceanic crust during the Late Triassic. Geochemical and mineralogical features indicate that the Langdu intrusions are I-type granite. They originated from partial melting of the mantle wedge metasomatized by subduction fluids. During their ascent, these magmas experienced fractional crystallization dominated by amphibole, titanite, rutile, and monazite. Geochemical records from zircon and apatite further reveal that the ore-forming magma of the Langdu intrusions exhibited high oxygen fugacity (ΔFMQ = +1.53), elevated H2O content (avg. 7.63 wt.%), and enrichment in S (avg. 560 ppm) and Cl (avg. 2141 ppm). This Cl-rich magma experienced fluid exsolution during its early evolutionary stage. This provided the necessary conditions for metal extraction and transport. In summary, the key factors controlling the formation of the Langdu porphyry–skarn Cu deposit are high-oxygen-fugacity magma enriched in water and volatiles (S and Cl), coupled with efficient fluid exsolution. This understanding is important for better understanding regional metallogeny and for guiding mineral exploration. Full article
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