The interface between subducting oceanic slabs and the hanging wall is a structurally and
lithologically complex region. Chemically disparate lithologies (sedimentary, mafic and …

Deep fluids are important for the evolution and properties of the lower continental and arc
crust in tectonically active settings. They comprise four components: H2O, nonpolar gases …

A comprehensive account of ore-forming processes, revised and updated The revised
second edition of Introduction to Ore-Forming Processes offers a guide to the multiplicity of …

Recycling of oceanic crust together with different types of marine sediments has become
somewhat of a paradigm for explaining the chemical and isotopic composition of ocean …

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 …

Geofluids (2010) 10, 254–269 Abstract Metamorphism and metasomatism both involve the
reequilibration of mineral assemblages due to changes in pressure, temperature and/or …

Fluids derived from the devolatilization of subducting slabs play a critical role in the melting
of the mantle wedge and global geochemical cycles. However, in spite of evidence for the …

Field evidence from the western Tianshan subduction complex in northwestern China
indicates that the high field strength elements Ti, Nb, and Ta were mobilized and thereby …

The transport of fluids through the Earth's crust controls the redistribution of elements to form
mineral and hydrocarbon deposits, the release and sequestration of greenhouse gases, and …

Intensive studies of ultrahigh-pressure (UHP) metamorphic rocks in continental collision
zones have provided petrological insights into the fluid regime during subduction and …