Adakite petrogenesis

PR Castillo - Lithos, 2012‏ - Elsevier
Adakite was originally proposed as a genetic term to define intermediate to high-silica, high
Sr/Y and La/Yb volcanic and plutonic rocks derived from melting of the basaltic portion of …

Making continental crust

RL Rudnick - Nature, 1995‏ - nature.com
The continental crust has an andesitic bulk composition, which cannot have been produced
by the basaltic magmatism that dominates sites of present-day crustal growth—at both …

Element transport from slab to volcanic front at the Mariana arc

T Elliott, T Plank, A Zindler, W White… - Journal of Geophysical …, 1997‏ - Wiley Online Library
We present a comprehensive geochemical data set for the most recent volcanics from the
Mariana Islands, which provides new constraints on the timing and nature of fluxes from the …

Adakites without slab melting: high pressure differentiation of island arc magma, Mindanao, the Philippines

CG Macpherson, ST Dreher, MF Thirlwall - Earth and Planetary Science …, 2006‏ - Elsevier
New geochemical data for Pleistocene magmatic rocks from the Surigao peninsula, eastern
Mindanao, the Philippines, demonstrate typical adakitic traits, including elevation of Sr/Y and …

Geochemical evidence for mélange melting in global arcs

SG Nielsen, HR Marschall - Science advances, 2017‏ - science.org
In subduction zones, sediments and hydrothermally altered oceanic crust, which together
form part of the subducting slab, contribute to the chemical composition of lavas erupted at …

Sampling mantle heterogeneity through oceanic basalts: isotopes and trace elements

AW Hofmann, RW Carlson - 2003‏ - books.google.com
Thus, Hurley and his collaborators were able to distinguish crustal magma sources from
those located in the mantle on the basis of their initial strontium-isotopic compositions …

Oxygen isotope variations of basaltic lavas and upper mantle rocks

JM Eiler - Reviews in mineralogy and geochemistry, 2001‏ - pubs.geoscienceworld.org
This chapter summarizes the oxygen isotope geochemistry of terrestrial basalts and their
mantle sources, including the conceptual framework for interpreting such data and the …

FOZO, HIMU, and the rest of the mantle zoo

A Stracke, AW Hofmann, SR Hart - Geochemistry, geophysics …, 2005‏ - Wiley Online Library
The parameter μ describes the 238U/204Pb ratio of an Earth reservoir. Mantle domains
labeled HIMU (high μ) originally defined reservoirs with highly radiogenic Pb isotope ratios …

Uranium isotope fractionation

MB Andersen, CH Stirling… - Reviews in Mineralogy …, 2017‏ - pubs.geoscienceworld.org
This review focuses on the rapidly growing field of natural 238U/235U variability, largely
driven by the technical advances in the measurement of U isotope ratios by mass …

Trace element transport during dehydration processes in the subducted oceanic crust: 1. Experiments and implications for the origin of ocean island basalts

T Kogiso, Y Tatsumi, S Nakano - Earth and Planetary Science Letters, 1997‏ - Elsevier
Dehydration experiments on natural amphibolite have been carried out under upper mantle
P/T conditions, in order to examine transportation of trace elements during dehydration …