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Investigation of geochemical characteristics and hydrothermal alteration zone mapping supported by remote sensing of a porphyry copper prospect, southeastern Iran: integrated applications to exploration.

Authors :
Khammar, Fereshteh
Alborzian Joonaghani, Shahab
Abadi, Leila Jan
Boomeri, Mohammad
Lentz, David R.
Source :
Geochemistry: Exploration, Environment, Analysis; Nov2022, Vol. 22 Issue 4, p1-23, 23p
Publication Year :
2022

Abstract

The area discussed in this exploration methodology case study is situated along the Sistan Suture Zone where the granitoid suite is a mantle-derived multiphase intrusive complex. One of the characteristics of this region is the presence of large areas of sulfide-bearing, quartz-rich stockwork and pyritic veins. Geochemical findings show that it is limited to the calc-alkaline to shoshonitic series intrusions and is associated with a volcanic arc (I-type) formed within an active continental margin subduction setting. The associated intrusive complex has characteristics consistent with Cu productive porphyries, supported by high K-adakitic Sr/Y, La/Yb, Y and Al<subscript>2</subscript>O<subscript>3</subscript>/TiO<subscript>2</subscript> geochemical signatures. The stockwork mineralization includes the hypogene (chalcopyrite and bornite), with locally superimposed supergene (covellite, malachite, goethite and hematite) zones. The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) images (visible-near infrared (VNIR), and shortwave infrared (SWIR) bands) and mixture tuned matched filtering (MTMF) algorithm enable identification of each hydrothermal alteration type, especially where pictures were innovatively classified using a concentration–number (C–N) fractal method. Four alteration types are evident (i.e. phyllic, argillic and propylitic), as well as secondary (supergene) jarosite, that are associated with gossans, which are an indicator of the hypogene pyritic shell. The propylitic alteration envelopes the phyllic and argillic varieties, forming a belt around the pyritic shell; alteration assemblages were confirmed by X-ray powder diffraction (XRD) analysis. Finally, all results show a mineralization alteration pattern within the case study region that is similar to those of known porphyry copper and associated molybdenum- and gold-bearing systems in this region of Iran and worldwide. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
14677873
Volume :
22
Issue :
4
Database :
Complementary Index
Journal :
Geochemistry: Exploration, Environment, Analysis
Publication Type :
Academic Journal
Accession number :
160904615
Full Text :
https://doi.org/10.1144/geochem2022-014