Orogenic gold deposits of all ages, from Paleoarchean to Tertiary, show consistency in
chemical composition. They are the products of aqueous-carbonic fluids, with typically 5–20 …

Although the term orogenic gold has become widely accepted over the past 20 years for
disseminated-to lode-style gold deposits that formed in a variety of tectonic environments …

The term orogenic gold deposits has been widely accepted, but there has been continuing
debate on their genesis. Early syn-sedimentary or syn-volcanic models and hydrothermal …

A metamorphic devolatilization model can explain the enrichment, segregation, timing,
distribution and character of many goldfields such as those found in Archean greenstone …

Although the term orogenic gold deposit has been widely accepted for all gold-only lode-
gold deposits, with the exception of Carlin-type deposits and rare intrusion-related gold …

The hydration and complexation of metals in hydrothermal fluids are key processes
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …

Understanding the source of metamorphic sulfur is critical to clarifying the complete cycle of
ore genesis, from source to sink, for several mineral deposit types. In this study, a mass …

Both gold-rich sulphides and ultra-high grade native gold oreshoots are common but poorly
understood phenomenon in orogenic-type mineral systems, partly because fluids in these …

This review offers an update on arsenic-bearing minerals and pigments with the aim of
serving as a guide for the study of Cultural Heritage materials in which these materials can …

Recognizing if and how Au is remobilized, in solid, melt, or fluid state, is critical for
understanding the origin of high-grade ore zones in Au deposits. When evidence for Au …