Re-Os behaviour during subduction of oceanic crust

Re-Os behaviour during subduction of oceanic crust

Podrobná bibliografie
Hlavní autoři:	Dale, C, Gannoun, A, Argles, T, Burton, K, Parkinson, I, Boyle, A
Médium:	Conference item
Vydáno:	2004

Podobné jednotky

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The Miocene ocean Os-187/Os-188 curve: Driven by continental weathering
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Open-system behaviour in mid-ocean ridge basalts
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A revised petrological model for subducted oceanic crust: insights from phase equilibrium modelling
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Undulations in Subducted Oceanic Crust Correlate With Shallow Tremor Distribution in the Kuril Trench Off Hokkaido
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Miocene Os and Tl isotopes in the Indian Ocean: Implications for Antarctic water export and the residence time of Os
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The scale and origin of the osmium isotope variations in mid-ocean ridge basalts
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Ocean-continent subduction cannot be initiated without preceding intra-oceanic subduction!
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Osmium isotope constraints on chemical heterogeneities in Indian mid-ocean ridge basalts
Autor: Burton, K, a další
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Osmium isotope heterogeneity in the constituent phases of mid-ocean ridge basalts.
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Investigating Ultra‐Low Velocity Zones as Sources of PKP Scattering Beneath North America and the Western Pacific Ocean: Potential Links to Subducted Oceanic Crust
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Barium content of Archaean continental crust reveals the onset of subduction was not global
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Barium content of Archaean continental crust reveals the onset of subduction was not global
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Tectonics of Part of the Vinodol Valley Within the Model of the Continental Crust Subduction
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A rapid transition from subduction to Barrovian metamorphism: geochronology of mafic–ultramafic relicts of oceanic crust in the Central Alps, Switzerland
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Light oxygen isotopic composition in deep mantle reveals oceanic crust subduction before 3.3 billion years ago
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Osmium isotope variations in the oceans: past and present
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Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust
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