Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie–Sulu orogen in China: implications for geodynamics and fluid regime
Discovery of coesite, diamond, and extreme 18O-depletion in eclogites from the Dabie–Sulu
orogen in central-east China has contributed much to our understanding of subduction of …
orogen in central-east China has contributed much to our understanding of subduction of …
A review of the isotopic and trace element evidence for mantle and crustal processes in the Hadean and Archean: Implications for the onset of plate tectonic …
Considerable geochemical evidence supports initiation of plate tectonics on Earth shortly
after the end of the Hadean. Nb/Th and Th/U of mafic-ultramafic rocks from the depleted …
after the end of the Hadean. Nb/Th and Th/U of mafic-ultramafic rocks from the depleted …
[HTML][HTML] Stagnant lids and mantle overturns: Implications for Archaean tectonics, magmagenesis, crustal growth, mantle evolution, and the start of plate tectonics
JH Bédard - Geoscience Frontiers, 2018 - Elsevier
The lower plate is the dominant agent in modern convergent margins characterized by
active subduction, as negatively buoyant oceanic lithosphere sinks into the asthenosphere …
active subduction, as negatively buoyant oceanic lithosphere sinks into the asthenosphere …
Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts
The oxygen isotope ratios of Phanerozoic zircons from kimberlite pipes in the Kaapvaal
Craton of southern Africa and the Siberian Platform vary from 4.7 to 5.9‰ VSMOW. High …
Craton of southern Africa and the Siberian Platform vary from 4.7 to 5.9‰ VSMOW. High …
A catalytic delamination-driven model for coupled genesis of Archaean crust and sub-continental lithospheric mantle
JH Bédard - Geochimica et cosmochimica acta, 2006 - Elsevier
There is no consensus on the processes responsible for near-coeval formation of Archaean
continental crust (dominantly tonalite–trondhjemite–granodiorite: TTG), greenstone belts …
continental crust (dominantly tonalite–trondhjemite–granodiorite: TTG), greenstone belts …
Post-collisional potassic and ultrapotassic magmatism in SW Tibet: geochemical and Sr–Nd–Pb–O isotopic constraints for mantle source characteristics and …
CH Miller, R Schuster, U Klötzli, W Frank… - Journal of …, 1999 - academic.oup.com
Major and trace element, Sr–Nd–Pb–O isotope and mineral chemical data are presented for
post-collisional ultrapotassic, silicic potassic and high-K calc-alkaline volcanic rocks from …
post-collisional ultrapotassic, silicic potassic and high-K calc-alkaline volcanic rocks from …
Mantle samples included in volcanic rocks: xenoliths and diamonds
Occurrence and ClassificationFragments of the Earth's mantle are frequently transported to
the surface via volcanic rocks that are dominantly alkaline in nature. These fragments range …
the surface via volcanic rocks that are dominantly alkaline in nature. These fragments range …
Anhydrous partial melting experiments on MORB-like eclogite: phase relations, phase compositions and mineral–melt partitioning of major elements at 2–3 GPa
M Pertermann, MM Hirschmann - Journal of Petrology, 2003 - academic.oup.com
We present melt and mineral compositions from nominally anhydrous partial melting
experiments at 2–3 GPa on a quartz eclogite composition (G2) similar to average oceanic …
experiments at 2–3 GPa on a quartz eclogite composition (G2) similar to average oceanic …
Two terrestrial lead isotope paradoxes, forward transport modelling, core formation and the history of the continental crust
JD Kramers, IN Tolstikhin - Chemical geology, 1997 - Elsevier
A combined solution for the two major terrestrial lead paradoxes has been sought. These
are the 'future'paradox (upper crustal and upper mantle Pb isotope compositions plot in the …
are the 'future'paradox (upper crustal and upper mantle Pb isotope compositions plot in the …
Concentration and transport of nitrate by the mat-forming sulphur bacterium Thioploca
MARINE species of Thioploca occur over 3,000 km along the continental shelf off Southern
Peru and North and Central Chile1–4. These filamentous bacteria live in bundles …
Peru and North and Central Chile1–4. These filamentous bacteria live in bundles …