Fluid phase separation promotes mineralization of epithermal base metal sulfides: A case study from the Central Seruyan Pb-Zn-Cu deposit in Kalimantan, Indonesia


Date

2025-11

Publication Type

Journal Article

ETH Bibliography

yes

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Abstract

The Central Seruyan Pb-Zn-Cu deposit in Central Kalimantan is an epithermal deposit situated within the Central Borneo metallogenic belt. To develop a genetic model for this deposit and provide insights for future exploration, we conducted studies on petrography, fluid inclusions, trace element geochemistry of sulfide minerals, and Pb isotope compositions. The mineralization can be categorized into four hydrothermal stages, based on the characteristics of alteration and ore mineral assemblages. The primary base metal sulfide minerals in the main ore stage include galena, sphalerite, and chalcopyrite, with minor amounts of covellite and tetrahedrite-tennantite. The principal Pb-Zn-Cu mineralization occurred under temperatures ranging from 170 to 320 ℃ at an apparent depth of 0.1 to 0.4 km from the paleosurface. Petrographic analysis and fluid inclusion microthermometry suggest that fluid boiling and decompression-induced quenching were the dominant processes driving base metal mineralization. The heterogeneous trace element distribution and color zonation observed in sulfide minerals further indicate an abrupt temperature change during the main mineralization stage. Arsenic and gold zonation in pyrite, along with indium and gallium zonation in sphalerite, suggest rapid temperature fluctuations likely associated with boiling. Microanalyses of fluid inclusions in sphalerite reveal that the ore-forming fluids originated from subduction-related magmas undergoing batholith-scale fractionation. For future exploration, we recommend targeting SW-NE trending faults, which may have facilitated decompression and subsequent boiling.

Publication status

published

Editor

Book title

Volume

186

Pages / Article No.

106925

Publisher

Elsevier

Event

Edition / version

Methods

Software

Geographic location

Date collected

Date created

Subject

Magmatic-hydrothermal fluid; Pb-Zn-Cu epithermal deposit; Fluid inclusion; Trace element geochemistry; Pb isotope; Phase separation

Organisational unit

03958 - Bachmann, Olivier / Bachmann, Olivier check_circle

Notes

Funding

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