Differences between Archean and Proterozoic lithospheres: Assessment of the possible major role of thermal conductivity

Differences between Archean and Proterozoic lithospheres: Assessment of the possible major role of thermal conductivity is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2006GGG.....7.3021P
P356DOI10.1029/2005GC001053

P2093author name stringM. Grégoire
M. Rabinowicz
S. Chevrot
S. Petitjean
P2860cites workHeat flow from the Earth's interior: Analysis of the global data setQ22122451
Rheology of the upper mantle: a synthesisQ28243293
The composition of the EarthQ29396953
Global anisotropy and the thickness of continentsQ46743947
Early formation and long-term stability of continents resulting from decompression melting in a convecting mantleQ53933381
Mantle convection and the thermal structure of the platesQ56136737
Composition and development of the continental tectosphereQ56136740
Structure and Formation of the Continental TectosphereQ56136780
Nature and composition of the continental crust: A lower crustal perspectiveQ56212018
The geochemical evolution of the continental crustQ56388610
Cratonization and thermal evolution of the mantleQ56656991
Olivine-wadsleyite transition in the system (Mg,Fe)2SiO4Q56680244
CRUST 5.1: A global crustal model at 5° × 5°Q57308373
Mantle solidus: Experimental constraints and the effects of peridotite compositionQ57857385
Models of seismic anisotropy in the deep continental lithosphereQ57866533
The density structure of subcontinental lithosphere through timeQ57888866
Is the continental Moho the crust-mantle boundary?Q57889050
Comparison of continental and oceanic mantle electrical conductivity: Is the Archean lithosphere dry?Q58156604
Thermal structure, thickness and composition of continental lithosphereQ58761020
K, U and Th in mid-ocean ridge basalt glasses and heat production, K/U and K/Rb in the mantleQ59057033
Evidence for a 150–200-km thick Archaean lithosphere from diamond inclusion thermobarometryQ59092650
The thermal structure of stable continental lithosphere within a dynamic mantleQ59712947
Heat flow scaling for mantle convection below a conducting lid: Resolving seemingly inconsistent modeling results regarding continental heat flowQ59712963
Thermal thickness and evolution of Precambrian lithosphere: A global studyQ59852440
Heat transfer and horizontally averaged temperature of convection with large viscosity variationsQ60709342
On the emergence of plate tectonicsQ61660922
The Seismic anisotropy of the Earth's mantle: From single crystal to polycrystalQ64029103
Age-dependent Large-scale Fabric of the Mantle Lithosphere as Derived from Surface-wave Velocity AnisotropyQ69670297
A global analysis of heat flow from Precambrian terrains: Implications for the thermal structure of Archean and Proterozoic lithosphereQ69671707
Heat flow and structure of the lithosphere in the Eastern Canadian ShieldQ70598129
Anisotropy of thermal diffusivity in the upper mantleQ74220108
Mantle values of thermal conductivity and the geotherm from phonon lifetimesQ95288260
Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphereQ97322608
Initiation of Subduction Zones as a Consequence of Lateral Compositional Buoyancy Contrast within the Lithosphere: a Petrological PerspectiveQ97455728
Diversion of heat by Archean cratons: a model for southern AfricaQ97999045
Three-dimensional modeling of plume-lithosphere interactionQ98962718
P433issue3
P921main subjectlithosphereQ83296
P577publication date2006-03-01
P1433published inG3: Geochemistry, Geophysics, GeosystemsQ15759647
P1476titleDifferences between Archean and Proterozoic lithospheres: Assessment of the possible major role of thermal conductivity
P478volume7

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Q33419293Temperature-dependent thermal diffusivity of the Earth's crust and implications for magmatismcites workP2860

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