The Trans-Mexican Volcanic Belt (TMVB) is a 1000km long Neogene continental arc
showing a large variation in composition and volcanic style, and an intra-arc extensional …

The transport of water from subducting crust into the mantle is mainly dictated by the stability
of hydrous minerals in subduction zones. The thermal structure of subduction zones is a key …

The last 15yr have seen an explosion of data on the volatile contents of magmas parental to
arc volcanoes. This has occurred due to the intense study of melt inclusions trapped in …

The partitioning of 15 major to trace metals between monosulfide solid solution (MSS),
sulfide liquid (SL) and mafic silicate melt (SM) was determined in piston-cylinder …

The origin of tholeiitic (TH) versus calc-alkaline (CA) magmatic trends has long been
debated. Part of the problem stems from the lack of a quantitative measure for the way in …

Continental basalts generally display enrichment of fluid-mobile elements and depletion of
high-field-strength elements, similar to those that evolved in the subduction environment, but …

Subduction zone magmas are characterized by high concentrations of pre-eruptive H2O,
presumably as a result of an H2O flux originating from the dehydrating, subducting slab. The …

The Yamansu skarn iron deposit is hosted in Early Carboniferous submarine lava flow and
volcaniclastic rocks of the Yamansu Formation in Eastern Tianshan Mountains, NW China …

Inclusions of basaltic melt trapped inside of olivine phenocrysts during igneous
crystallization provide a rich, crystal-scale record of magmatic processes ranging from …

This paper deals with the earliest stages of formation of porphyry Cu deposits, starting with
the production of partial melts in the mantle and ending where upper crustal magmas reach …