Orogenic Gold Deposit in Metamorphic Rocks: Minerals and Structural Control at Rarowatu Area, Southeastern Arm of Sulawesi, Indonesia

نویسندگان

چکیده

This research aims to examine the relationship between hydrothermal alteration and mineralization (ore mineralogy) in study area geological structures deformation mechanism. The was determined based on petrographic analysis, ore mineralogy which microscopic analysis. mechanism is by paleo stress analysis using win-tensor, direction of principal joints/veins faults calculated right-dihedron method. Hydrothermal includes silicification, argillic, propylitic, phyllic alterations; consists stibnite, cinnabar, pyrite, chalcopyrite, sphalerite, covellite, hematite, arsenopyrite at metamorphic rocks. structure developed shear fractures Wumbubangka right Normal-slip Fault, accompanied right-slip lag fault reverse-slip formed a simple Crenulation, micro-folds, porphyroblastic are also recognized thin sections. normal-slip fault, considered syn-mineralization structure, transpressional transtensional geologic structures, forming quartz vein parallel crosscutting foliation. correlation surface microstructures indicates that tectonic regimes have controlled gold area.

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ژورنال

عنوان ژورنال: Iraqi geological journal

سال: 2023

ISSN: ['2414-6064', '2663-8754']

DOI: https://doi.org/10.46717/igj.56.1b.2ms-2023-2-10