Re-Os behaviour during subduction of oceanic crust

Re-Os behaviour during subduction of oceanic crust

Bibliografiske detaljer
Main Authors:	Dale, C, Gannoun, A, Argles, T, Burton, K, Parkinson, I, Boyle, A
Format:	Conference item
Udgivet:	2004

Lignende værker

Rhenium-osmium isotope and elemental behaviour during subduction of oceanic crust and the implications for mantle recycling
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Highly siderophile element behaviour accompanying subduction of oceanic crust: Whole rock and mineral-scale insights from a high-pressure terrain
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Ancient melt extraction from the oceanic upper mantle revealed by Re-Os isotopes in abyssal peridotites from the Mid-Atlantic ridge
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Seismic visibility of carbonated subducted oceanic crust in the lower mantle
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Calcium isotope evidence for early Archaean carbonates and subduction of oceanic crust
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Interplay between oceanic subduction and continental collision in building continental crust
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Subducted oceanic crust as the origin of seismically slow lower-mantle structures
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Strain and Stress Accumulation in Viscoelastic Splay Fault and Subducting Oceanic Crust
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A Role for Subducted Oceanic Crust in Generating the Depleted Mid‐Ocean Ridge Basalt Mantle
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Velocity and density characteristics of subducted oceanic crust and the origin of lower-mantle heterogeneities
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Carbon Dioxide Released From Subducted Oceanic Crust by Hydrous Carbonatitic Liquids
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Alteration and dehydration of subducting oceanic crust within subduction zones: implications for décollement step-down and plate-boundary seismogenesis
af: Jun Kameda, et al.
Udgivet: (2017-04-01)

Pressure-driven processes explain the decreasing magnetization of the subducting oceanic crust in the Japan Trench
af: Dongwoo Han, et al.
Udgivet: (2023-07-01)

New age for ferromanganese crust 109D-C and implications for isotopic records of lead, neodymium, hafnium, and thallium in the Pliocene Indian Ocean
af: Nielsen, S, et al.
Udgivet: (2011)

Fe<sup>3+</sup>∕ΣFe variation in lawsonite and epidote in subducted oceanic crust
af: D. L. Whitney, et al.
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The Miocene ocean Os-187/Os-188 curve: Driven by continental weathering
af: Georg, R, et al.
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Open-system behaviour in mid-ocean ridge basalts
af: Gannoun, A, et al.
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A revised petrological model for subducted oceanic crust: insights from phase equilibrium modelling
af: Hernández‐Uribe, D, et al.
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Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogite
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Author Correction: Velocity and density characteristics of subducted oceanic crust and the origin of lower-mantle heterogeneities
af: Wenzhong Wang, et al.
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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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Factors on the Mesozoic Transition From Flat to Steep Subduction of the Paleo‐Pacific Plate Beneath South China: Thickened Oceanic Crust and Subduction Rate
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Pervasive detachment faults within the slow spreading oceanic crust at the poorly coupled Antilles subduction zone
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Assessing the scale of osmium isotope heterogeneity in Mid-Ocean Ridge Basalts
af: Gannoun, A, et al.
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Spatial Heterogeneity of Pore Structure in the Crustal Section of the Samail Ophiolite: Implications for High VP/VS Anomalies in Subducting Oceanic Crust
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Extrusion of subducted crust explains the emplacement of far-travelled ophiolites
af: Kristóf Porkoláb, et al.
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The scale and origin of the osmium isotope variations in mid-ocean ridge basalts
af: Gannoun, A, et al.
Udgivet: (2007)

The scale and origin of the osmium isotope variations in mid-ocean ridge basalts
af: Gannoun, A, et al.
Udgivet: (2007)

Ocean-continent subduction cannot be initiated without preceding intra-oceanic subduction!
af: Alexander Koptev, et al.
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Osmium isotope constraints on chemical heterogeneities in Indian mid-ocean ridge basalts
af: Burton, K, et al.
Udgivet: (2009)

Osmium isotope heterogeneity in the constituent phases of mid-ocean ridge basalts.
af: Gannoun, A, et al.
Udgivet: (2004)

Investigating Ultra‐Low Velocity Zones as Sources of PKP Scattering Beneath North America and the Western Pacific Ocean: Potential Links to Subducted Oceanic Crust
af: Michael S. Thorne, et al.
Udgivet: (2024-08-01)

Barium content of Archaean continental crust reveals the onset of subduction was not global
af: Huang, G, et al.
Udgivet: (2022)

Barium content of Archaean continental crust reveals the onset of subduction was not global
af: Guangyu Huang, et al.
Udgivet: (2022-11-01)

Tectonics of Part of the Vinodol Valley Within the Model of the Continental Crust Subduction
af: Ivan Blašković
Udgivet: (2010-11-01)

A rapid transition from subduction to Barrovian metamorphism: geochronology of mafic–ultramafic relicts of oceanic crust in the Central Alps, Switzerland
af: Kim Lemke, et al.
Udgivet: (2024-08-01)

Light oxygen isotopic composition in deep mantle reveals oceanic crust subduction before 3.3 billion years ago
af: Dongjian Ouyang, et al.
Udgivet: (2024-01-01)

Osmium isotope variations in the oceans: past and present
af: Burton, K, et al.
Udgivet: (2002)

Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust
af: Sonja Aulbach, et al.
Udgivet: (2019-12-01)