Intracontinental rift-related deposits: A review of key models

RUBINSTEIN, NORA; CROSTA, SABRINA; SEGAL, SUSANA J.; ZAPPETTINI, EDUARDO O.

ORE GEOLOGY REVIEWS

ELSEVIER SCIENCE BV

Año: 2017 vol. 89 p. 594 - 608

0169-1368

Mineral systems associated with extensional fault systems in continental environments and not relatedto magmatic activity involve various deposit models that can be grouped into a single system whichwould plausibly explain the source and chemical composition of fluids, the formation depth, the sourceof heat and the structural history within a common geologic setting.Mineral deposits related to this tectonic setting are those described within the detachment-relatedmodel, including massive replacements, stockworks and veins of Cu and Fe oxides (with or withoutAu), polymetallic sulfide veins, barite and/or fluorite veins and stratabound and vein Mn deposits. Thispaper reviews the abovementioned deposits as well as others related to this tectonic setting, such asSe-rich polymetallic deposits, Almadén type Hg deposits, U-Ni-Co-As-Ag polymetallic deposits with subordinatedBi-Cu-Pb-Zn (five element deposits), simple polymetallic Pb-Ag-Zn deposits, and the membersof the IOCG clan (including the Au-Ag detachment-related deposits) involved in the Cu-Fe (-Au) modeldeposits.All these mineral deposits are the result of fluid motion unrelated to magmatism in areas of thermalanomalies. These fluids collect certain elements producing a district mineralogical specialization withinhomogeneities in the distribution of mineralization types along the region affected by rifting. Fluidhomogenization temperatures and salinities range between 60 and 430 C, and 0 and 27 equivalentwt% NaCl, respectively. The O, S and D isotope composition is consistent with basinal poral fluids derivedfrom meteoric waters under different P-T conditions in an active faults environment. Pb isotopes suggestthat Pb derives from a mixture of rocks with a long period of residence in the upper crust and rocksdeformed along repeated orogenic cycles with a contribution of Pb from the lower crust and even themantle. Fluid flow along fault planes leads to different types of hydrothermal alterations depending onP-T conditions, particularly propylitization and low temperature potassium metasomatism.All such deposits can be found in two different geotectonic environments of metallogenic interestinvolving extensional faults associated with detachment zones in depth; i.e., 1) continental extension in a back-arc environment and 2) extension with rift development and generation of oceanic crust in a passive continental margin. Although the economic importance of this group of deposits is mainly relatedto industrial minerals, non-magmatic IOCG deposits could significantly augment the economic potential of this setting. The rift setting itself, without relation to detachments, is favorable for concentrating metals in stratabound deposits such as SEDEX ores. Additionally, the development of deposits directly related to magmatic activity contributes to the economic interest of this environment.