The Miduk porphyry Cu deposit,Kerman, Iran: A geochemical analysis of the potassic zone including halogen element systematics related to Cu mineralization processes |
| |
| Authors: | Mohammad Boomeri Kazuo Nakashima David Richard Lentz |
| |
| Affiliation: | 1. Geology Department, University of Sistan and Baluchestan, Zahedan, Iran;2. Department of Earth and Environmental Sciences, Faculty of Science, Yamagata University, Yamagata, Japan;3. Department of Geology, University of New Brunswick, PO Box 4400, Fredericton, NB Canada E3B5A3 |
| |
| Abstract: | ![]()
Miduk hypogene and supergene porphyry Cu–Mo mineralization occurs within the Miocene porphyritic quartz–diorite and host Eocene plagioclase–hornblende phyric andesitic pyroclastic and flow sequence. Both the host rocks were extensively altered by hydrothermal fluids to dominantly potassic, phyllic, and argillic with interstitial to distal propylitic types. |
| |
| Keywords: | Miduk porphyry Cu deposit Potassic alteration Biotite Halogen fugacity Iran |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
