Noble gases and volatile recycling at subduction zones

DR Hilton, TP Fischer, B Marty - Reviews in mineralogy …, 2002 - pubs.geoscienceworld.org
Volatiles are lost from the Earth's mantle to the atmosphere, hydrosphere and crust through
a combination of subaerial and submarine volcanic and magmatic activity. These volatiles …

[HTML][HTML] Depósitos epitermales en México: actualización de su conocimiento y reclasificación empírica

A Camprubí, T Albinson - Boletín de la Sociedad Geológica Mexicana, 2006 - scielo.org.mx
Depósitos epitermales en México: actualización de su conocimiento y reclasificación empírica
SciELO - Scientific Electronic Library Online vol.58 número1 Características metalogenéticas …

Hafnium isotope evidence for 'conservative'element mobility during subduction zone processes

JD Woodhead, JM Hergt, JP Davidson… - Earth and Planetary …, 2001 - Elsevier
The high field strength elements (HFSE) play a critical role in the interpretation of chemical
variation within subduction-related magmas by providing an assumed mantle-dominated …

Australian crust in Indonesia

R Hall, I Sevastjanova - Australian Journal of Earth Sciences, 2012 - Taylor & Francis
It is now generally accepted that the core of Southeast (SE) Asia was assembled from
continental blocks that separated from Gondwana in the Paleozoic and amalgamated with …

Trace element and Sr, Nd, Pb and O isotope variations in medium-K and high-K volcanic rocks from Merapi Volcano, Central Java, Indonesia: evidence for the …

R Gertisser, J Keller - Journal of Petrology, 2003 - academic.oup.com
Abstract Merapi volcano (Central Java), located within the Quaternary volcanic front of the
Sunda arc, is one of the most active volcanoes of the Indonesian archipelago. During the …

Magma–Carbonate Interaction Processes and Associated CO2 Release at Merapi Volcano, Indonesia: Insights from Experimental Petrology

FM Deegan, VR Troll, C Freda, V Misiti… - Journal of …, 2010 - academic.oup.com
There is considerable evidence for continuing, late-stage interaction between the magmatic
system at Merapi volcano, Indonesia, and local crustal carbonate (limestone). Calc-silicate …

U, Th and Ra disequilibria, Sr, Nd and Pb isotope and trace element variations in Sunda arc lavas: predominance of a subducted sediment component

S Turner, J Foden - Contributions to Mineralogy and Petrology, 2001 - Springer
The time scales of magma formation, transfer and storage beneath island arc volcanoes are
important because of the insights they provide into the physical processes of magma …

Subduction and recycling of nitrogen along the Central American margin

TP Fischer, DR Hilton, MM Zimmer, AM Shaw… - Science, 2002 - science.org
We report N and He isotopic and relative abundance characteristics of volatiles emitted from
two segments of the Central American volcanic arc. In Guatemala, δ15N values are positive …

The helium and carbon isotope systematics of a continental geothermal system: results from monitoring studies at Long Valley caldera (California, USA)

DR Hilton - Chemical Geology, 1996 - Elsevier
This study reports fumarole and hot spring gas chemistry of a 3-year monitoring programme
(1986–1988) at the seismically-active Long Valley caldera (LVC) in the Sierra Nevada …

Carbonate assimilation at Merapi Volcano, Java, Indonesia: insights from crystal isotope stratigraphy

JP Chadwick, VR Troll, C Ginibre, D Morgan… - Journal of …, 2007 - academic.oup.com
Recent basaltic andesite lavas from Merapi volcano contain abundant, complexly zoned,
plagioclase phenocrysts, analysed here for their petrographic textures, major element …