Veins are common features in rocks and extremely useful structures to determine stress,
strain, pressure, temperature, fluid composition and fluid origin during their formation. Here …

The French Massif Central constitutes an exceptional study area due to the diversity of its
metallic deposits, its internal position in the Variscan belt, and the abundance of available …

Much of the world's known gold has been derived from arrays of quartz veins. The veins
formed during periods of mountain building that occurred as long as 3 billion years ago …

Current models of the formation and distribution of gold deposits on Earth are based on the
long-standing paradigm that hydrogen sulfide and chloride are the ligands responsible for …

Although carbon dioxide is one of the major components of crustal fluids responsible for ore
deposit formation, its effect on transport and precipitation of metals remains unknown, due to …

Orogenic gold deposits formed in various terranes of most ages since the Paleoarchean and
generally consist of quartz veins hosted in shear zones formed at the ductile brittle transition …

Scheelite and rutile from several metaturbidite-hosted gold-bearing quartz vein deposits of
the Meguma Terrane of Nova Scotia were analyzed for trace elements including rare earth …

This paper describes a methodology of translating mineral deposit models into flexible
probabilistic structures based on (1) extraction of ore components (fluids, metals, and …

The significance of magnesium isotope (δ 26 Mg) fractionation in the continental
hydrothermal domain is poorly explored. Here, a detailed Mg isotope dataset from various …

The Jbel Saghro is interpreted as part of a long-lived silicic large igneous province. The area
comprises two lithostructural complexes. The Lower Complex consists of folded …