The massive accumulation of available multi-modal mineral exploration data for most
metallogenic belts worldwide provides abundant information for the discovery of mineral …

Submarine hydrothermal sulfide ores occur at mid-ocean ridges, intra-oceanic arcs and in
back-arc basins associated with host rocks of highly variable composition. Pyrite is the …

Due to the combined influences such as ore-forming temperature, fluid and metal sources,
sphalerite tends to incorporate diverse contents of trace elements during the formation of …

The key for understanding the trace metal inventory of currently explored VHMS deposits
lies in the understanding of trace element distribution during the formation of these deposits …

In the Urals, a wide range of well-preserved chimneys are found in VMS deposits, which are
associated with ultramafic (Atlantic type: Dergamysh), mafic (Cyprus type: Buribay), bimodal …

The Troodos ophiolite represents one of the best-preserved fossil analogs of modern
oceanic crust and includes numerous volcanic-hosted massive sulfide deposits. The …

Trace element compositions of sphalerite and chalcopyrite have been investigated for four
arc-hosted Cretaceous VMS deposits (María Teresa, Perubar, and Palma in Peru, and Cerro …

Abstract Shallow (< 1500 mbsl) submarine arc-related hydrothermal systems can host base
(Cu), precious (Au) and volatile elements (As, Se, Sb, Te, Tl) in significant quantities. Their …

Abstract The basalt-hosted Wocan Hydrothermal Field (WHF), located on the NW slope of an
axial volcanic ridge at a depth of∼ 3000 m at 6° 22′ N on the slow-spreading Carlsberg …

Many hydrothermal vein-type Pb–Zn deposits were discovered in the Qinhang Ore Belt
(South China), but their origin remains enigmatic due to the lack of constraints on the ore …