The origin of hypogene alteration and mineralization features in the Escondida porphyry Cu deposit resulted from intense overprinting related to three main hydrothermal stages. beginning each stage is recorded by deposition bright quartz crystals on vein walls that precipitated high-temperature fluids. In deepest zones deposit, earliest started with exsolution intermediate-density fluids, which...

Abstract –– Tambang Sawah Area, Lebong Regency, Bengkulu Province, is geologically located in the Barisan mountains and Sumatra fault zone. The prospect of area lies physiography central Sumatran ranges composed by igneous rocks Sunda – Banda magmatic arc. This study aimed to understand deposit geology ore characteristics gold at area. Quartz vein mineralization occurred granite rock intruded i...

The Tareek Darreh gold deposit is located 40km north of Torbat-e Jaam in the Khorassan-Razavi province, NE-Iran. The study area mainly comprises slightly metamorphosed, sedimentary rocks of Jurassic age including alternation of shale, siltstone, and sandstone. These rocks have been intruded by plutonic rocks such as gabbro-norite, diorite, quartz-diorite, and rhyodacite. The ore bodes are expos...

This work describes the structural and lithological controls that affect distribution, orientation, precipitation mechanism of mineralization in Martinetas district, from context analysis role played by geological units host mineralization. is a low sulfidation epithermal gold silver mining district located northeastern sector Deseado Massif, Argentina. The characterized numerous quartz veins, ...

Oxygen, carbon, and strontium isotope variations in vein-filling calcite and quartz cements and their host rocks are used to elucidate the origin, spatial and temporal evolution, and migration pathways of fluids in the detachment Nuncios fold complex, northeastern Mexico. The folded Mesozoic sedimentary sequence contains two regional paleohydrostratigraphic units separated by a unit of low perm...

The Mesozoic Xuefengshan Orogen (XFSO) in South China hosts abundant gold ore deposits. XFSO records a history of polyphase tectonic deformation and the structural controls on mineralization are poorly understood. recently discovered quartz-vein type Huanggou deposit southern is characterized by multiple stages represents an excellent natural laboratory for deciphering complex orogenic belt. A ...