You are here: Home » Past Issues » Volume 11, 2016 - Number 1 » GOLD POSITION AND DISTRIBUTION IN LOWER CRETACEOUS IOCG DEPOSITS OF THE COPIAPO BASIN, ATACAMA REGION, CHILE
Ioan FILIP1 & Eugen ORLANDEA2
1Carmen Bajo Mining Company, P-je Hochschild 113-A, Copiapo, Atacama, Chile, e-mail: firstname.lastname@example.org
2Carmen Bajo Mining Company, P-je Hochschild 113-A, Copiapo, Atacama, Chile,e-mail: email@example.com
GOLD POSITION AND DISTRIBUTION IN LOWER CRETACEOUS IOCG DEPOSITS OF THE COPIAPO BASIN, ATACAMA REGION, CHILE
Detailed geological, petrographic and metallogenic data, including stable isotopes and fluid inclusions have been derived for vein-stockwork mineralization, stratabound to Manto type and replacement-lens shaped to skarn/contact ore bodies of the Lower Cretaceous IOCG Copper Belt near Copiapo, Atacama (Ojancos Viejo-Ojancos Nuevo tectonic alignments). At least three types of gold association can be distinguished in this IOCG environment, as follows:
1. Early iron oxide (magnetite) related gold (M type) is included in early mesothermal magnetite and mushketovite associated with fine grained biotite with/without potassic feldspar. The fluids of the M type gold bearing stage were hypersaline (41-59%wt.NaCl eq.) with temperatures ranging from 3500 to >5000C. The source of fluids was mainly magmatic (δ34S from -5.3 to 4.7) with possible crustal rock (e.g. evaporite) assimilation during the magma ascent.
2. Later copper sulfides (chalcopyrite) related gold (C type) is genetically linked with, the mostly mesothermal, main copper event and associated with proximal Na-rich (albite) alteration. C type gold was deposited from magmatic or near magmatic fluids (δ34S from -6.9 to 4.1) which, also were highly saline (32-59%wt.NaCleq.) at temperatures varying between 2500 and 4000C.The evolution of the mineralized system may have included the introduction of an external saline brine and the possible mixing of two different types of fluid.
3. Late pyrite or hematite (specularite) related gold (P/H type). This gold type is recorded either as a subsequent epithermal overprint or a still preserved epithermal suite in the upper part of the structures. The key proximal alteration is a sericite bearing intermediate argillic halo or carbonate – hematite dominant assemblage. The fluid temperatures were between 1800-2900C, with moderate salinities (15-20%wt. NaCleq.).The mixing of magmatic (δ13C from -3 to -9; δ34S between 0-2) and meteoric fluids (δ18O between 9-11; δ34S extreme values of 7.6 and 8.3), including boiling phenomena characterize this gold bearing stage.
Keyword: Au typology, Lower Cretaceous, IOCG deposits, Ojancos Viejo/Nuevo, Copiapo, Chile.
(c) 2006 - 2021 , Earth and Environmental Team
Design by Adrian Dorin