Mega structural system Cajamarca, structural construction suggested in relation to the mineralization of porphyries and epithermals in northern Peru

• Autores: Torres Guerra, Jesús A., Tumi Pacheco, José, Samanez Trigoso, Mariel, Caycho Vilca, Yordy
• Formato: artículo
• Fecha de Publicación: 2020
• Institución: Universidad Nacional Mayor de San Marcos
• Repositorio: Revistas - Universidad Nacional Mayor de San Marcos
• Lenguaje: español
• OAI Identifier: oai:ojs.csi.unmsm:article/19187
• Enlace del recurso: https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/19187
• Nivel de acceso: acceso abierto
• Materia: Mega structural systems; dextral; sinestral; deposits; inca and quechua phases; Mega sistemas estructurales; depósitos; fases inca y quechua

The north of Peru is characterized by the presence of world-class porphyry (Cu-Au and Cu-Mo) and epithermal (Au) deposits, located on the west of central Andes, northern Peru. These mines and mineralized deposits are present in a temporal-structural associated with Neogene magmatism with ages from 24 Ma to 7 Ma, intruding silica-clastic rocks from the upper Cretaceous, which, due to the effects of tectonic deformations, particularly in the Cenozoic (Incaica and Quechua phases), led to the occurrence of mega controls Structural problems such as the one proposed in the following publication and hopes to open a window of debate in its environment. Structurally, the deposits in the north of Peru are controlled by mega structural systems that contain the Punre - Canchis fault (Rivera et al., 2008) in the eastern sector as the main structural accident, as well as the system of folds and faults of the Marañón, and in the Western sector include faults to the East of Chongoyape that limit the eastern edge of the Batolito of the Coast, as well as the silicoclastics of the Mesozoic, putting them in contact with volcanos of the Cenozoic. The basin in its western sector would have undergone changes in the status of regional efforts, producing epirogenic movements, since the Upper Cretaceous, with large regional faults playing an important role, controlling the extensive basin through normal faults. (Pardo-Casas & Molnar, 1987). The subduction occurred obliquely and with a low angle, thus generating permeable zones, of kilometer dimensions generating mega parallel and conjugate structures that gave rise to structural jogs. The analysis and evaluation of the compiled information allows us to suggest a new concept to define the structural behavior of this sector in the Peruvian Andes, proposing a new denomination Mega Cajamarca Structural System for a sinextral system with compressive behavior and with Andean direction in the Miocene. It is also considered that in this north sector, an oblique convergence plaque area has been developed in the subduction zone, as well as the subduction angle variation (15 degrees), as main characteristic for the mineral deposit generation. In this way, this concept has the principal objective to involve a general mechanism of an ensemble understanding and interpretation, including previously developed structural studies.