| Mousivand, Fardin, Rastad, Ebrahim, Meffre, Sebastien, Peter, Jan M., Solomon, Mike, Zaw, Khin (2011) U–Pb geochronology and Pb isotope characteristics of the Chahgaz volcanogenic massive sulphide deposit, southern Iran. International Geology Review, 53 (10) 1239-1262 doi:10.1080/00206811003783364 | Journal (article/letter/editorial) | characteristics of the Chahgaz volcanogenic massive sulphide deposit, southern Iran a a b Fardin Mousivand , Ebrahim...characteristics of the Chahgaz volcanogenic massive sulphide deposit, southern Iran, International Geology Review, 53:10...characteristics of the Chahgaz volcanogenic massive sulphide deposit, southern Iran 1938-2839 Geology Review, 0020-6814...Chahgaz Zn–Pb–Cu volcanogenic massive sulphide (VMS) deposit occurs within a metamorphosed bimodal volcano–sedimentary...Sanandaj–Sirjan Zone (SSZ) of southern Iran. This deposit is hosted by rhyodacitic volcaniclastics and is | | | Journal (article/letter/editorial) | Allen3,4 and Carmen Conde5 Centro de Astrobiología - Consejo Superior de Investigaciones Científicas, Ctra...Ctra Ajalvir km.4.5. 28850 Torrejón de Ardoz, Spain. f.tornos@csic.es 2 Geological Survey of Canada...pumiceous volcaniclastic rocks, and in some cases limestone, favoured the development of large replacive deposits...carbonate-altered mass flow deposits) or limestone. One deposit or district may comprise two or more of these...are one of the best known and wellstudied ore deposit types (e.g., Franklin et al. 1981; 2005; Lydon | | Mousivand, Fardin, Rastad, Ebrahim, Meffre, Sebastien, Peter, Jan M., Mohajjel, Mohammad, Zaw, Khin, Emami, Mohammad Hashem (2012) Age and tectonic setting of the Bavanat Cu–Zn–Ag Besshi-type volcanogenic massive sulfide deposit, southern Iran. Mineralium Deposita, 47 (8) 911-931 doi:10.1007/s00126-012-0407-6 | Journal (article/letter/editorial) | Cu–Zn–Ag Besshi-type volcanogenic massive sulfide deposit, southern Iran Fardin Mousivand & Ebrahim Rastad...Besshi-type volcanogenic massive sulfide (VMS) deposit occurs within the Surian volcano-sedimentary complex...shale, basalt, gabbro sills, and thin-bedded limestone. Mineralization occurs as stratiform sheet-like...foraminifera, and conodonts). The Bavanat Cu–Zn–Ag VMS deposit is located in the Bavanat area, 195 km northeast...(Fig. 1) and about 170 km NW of the Chahgaz VMS deposit (Figs. 1 and 2). There are numerous semimassive |
|