The oxidation state, and sulfur and Cu contents of arc magmas: implications for metallogeny
JP Richards - Lithos, 2015 - Elsevier
Global data for measured Fe 2 O 3/FeO ratios and Cu contents in unaltered volcanic and
intrusive arc rocks indicate that, on average, they are slightly more oxidized than other …
intrusive arc rocks indicate that, on average, they are slightly more oxidized than other …
Magmatic to hydrothermal metal fluxes in convergent and collided margins
JP Richards - Ore Geology Reviews, 2011 - Elsevier
Metals such as Cu, Mo, Au, Sn, and W in porphyry and related epithermal mineral deposits
are derived predominantly from the associated magmas, via magmatic–hydrothermal fluids …
are derived predominantly from the associated magmas, via magmatic–hydrothermal fluids …
Th/U ratios in metamorphic zircon
C Yakymchuk, CL Kirkland… - Journal of Metamorphic …, 2018 - Wiley Online Library
The Th/U ratios of zircon crystals are routinely used to help understand their growth
mechanism. Despite the wide application of Th/U ratios in understanding the geological …
mechanism. Despite the wide application of Th/U ratios in understanding the geological …
Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources: The Himalayan leucogranites
LE Gao, L Zeng, PD Asimow - Geology, 2017 - pubs.geoscienceworld.org
Abstract Most of the Himalayan Cenozoic leucogranites are products of partial melting of
metapelite sources. In the Malashan-Gyirong area (southern Tibet), the geochemical …
metapelite sources. In the Malashan-Gyirong area (southern Tibet), the geochemical …
Earth's heterogeneous mantle: A product of convection-driven interaction between crust and mantle
A Stracke - Chemical Geology, 2012 - Elsevier
Ubiquitous heterogeneity in the Earth's mantle has been documented by numerous
chemical and isotopic analyses of oceanic basalts. Despite the ever-increasing amount of …
chemical and isotopic analyses of oceanic basalts. Despite the ever-increasing amount of …
Rutile and its applications in earth sciences
G Meinhold - Earth-Science Reviews, 2010 - Elsevier
Rutile is the most common naturally occurring titanium dioxide polymorph and is widely
distributed as an accessory mineral in metamorphic rocks ranging from greenschist to …
distributed as an accessory mineral in metamorphic rocks ranging from greenschist to …
Geochemistry and magmatic history of eclogites and ultramafic rocks from the Chinese continental scientific drill hole: subduction and ultrahigh-pressure …
Three distinct groups of eclogites (low-Mg–Ti eclogites, high-Ti eclogites and Mg-rich
eclogites) and ultramafic rocks from the depth interval of 100–680 m of the Chinese …
eclogites) and ultramafic rocks from the depth interval of 100–680 m of the Chinese …
Partial melting, fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision
Partial melting at continental lithosphere depths plays an important role in generating
geochemical variations in igneous rocks. In particular, dehydration melting of ultrahigh …
geochemical variations in igneous rocks. In particular, dehydration melting of ultrahigh …
Trace element composition of mantle end‐members: Implications for recycling of oceanic and upper and lower continental crust
M Willbold, A Stracke - Geochemistry, Geophysics, Geosystems, 2006 - Wiley Online Library
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 …
somewhat of a paradigm for explaining the chemical and isotopic composition of ocean …
Trace element partitioning between apatite and silicate melts
S Prowatke, S Klemme - Geochimica et Cosmochimica Acta, 2006 - Elsevier
We present new experimental apatite/melt trace element partition coefficients for a large
number of trace elements (Cs, Rb, Ba, La, Ce, Pr, Sm, Gd, Lu, Y, Sr, Zr, Hf, Nb, Ta, U, Pb …
number of trace elements (Cs, Rb, Ba, La, Ce, Pr, Sm, Gd, Lu, Y, Sr, Zr, Hf, Nb, Ta, U, Pb …