The dynamic history of the Trans-Mexican Volcanic Belt and the Mexico subduction zone
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 …
showing a large variation in composition and volcanic style, and an intra-arc extensional …
The transport of water in subduction zones
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 …
of hydrous minerals in subduction zones. The thermal structure of subduction zones is a key …
Why do mafic arc magmas contain∼ 4 wt% water on average?
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 …
arc volcanoes. This has occurred due to the intense study of melt inclusions trapped in …
Partitioning of V, Mn, Co, Ni, Cu, Zn, As, Mo, Ag, Sn, Sb, W, Au, Pb, and Bi between sulfide phases and hydrous basanite melt at upper mantle conditions
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 …
sulfide liquid (SL) and mafic silicate melt (SM) was determined in piston-cylinder …
The role of water in generating the calc-alkaline trend: new volatile data for Aleutian magmas and a new tholeiitic index
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 …
debated. Part of the problem stems from the lack of a quantitative measure for the way in …
Origin of arc-like continental basalts: Implications for deep-Earth fluid cycling and tectonic discrimination
XC Wang, SA Wilde, B Xu, CJ Pang - Lithos, 2016 - Elsevier
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 …
high-field-strength elements, similar to those that evolved in the subduction environment, but …
Mantle melting as a function of water content beneath the Mariana Arc
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 …
presumably as a result of an H2O flux originating from the dehydrating, subducting slab. The …
Geochronology and geochemistry of submarine volcanic rocks in the Yamansu iron deposit, Eastern Tianshan Mountains, NW China: constraints on 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 …
volcaniclastic rocks of the Yamansu Formation in Eastern Tianshan Mountains, NW China …
Olivine-hosted melt inclusions: a microscopic perspective on a complex magmatic world
Inclusions of basaltic melt trapped inside of olivine phenocrysts during igneous
crystallization provide a rich, crystal-scale record of magmatic processes ranging from …
crystallization provide a rich, crystal-scale record of magmatic processes ranging from …
Magmatic controls on porphyry copper genesis
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 …
the production of partial melts in the mantle and ending where upper crustal magmas reach …