About: Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus

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scholarly article by C. C. Reese et al published 1 June 1998 in Journal of Geophysical Research

Attributes	Values
rdf:type	Item
description	wetenschappelijk artikel (nl) наукова стаття, опублікована в червні 1998 (uk) article scientifique publié en 1998 (fr) im Juni 1998 veröffentlichter wissenschaftlicher Artikel (de) scholarly article by C. C. Reese et al published 1 June 1998 in Journal of Geophysical Research (en)
publication date	wds:Q59712971-55EABE5C-70B1-4B6E-93B7-266F244969AC
publication date	1998-06-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q59712971-E0376BA6-99A1-4F6B-AFE3-638206DD697B
language of work or name	English
cites work	wds:Q59712971-09E5CBE8-C499-4CBE-95D1-C191137A1C3E wds:Q59712971-1A62116A-FF44-49B4-8EFD-B773ABBAE9AA wds:Q59712971-26ABBE6F-F273-4FBC-A9D7-299AB8E948ED wds:Q59712971-50578338-7E0E-44D0-A13D-4712FA4D58F8 wds:Q59712971-60C3A8E1-954C-4CC9-AEE2-323BEBE9DC97 wds:Q59712971-63E550A0-636C-4158-B105-9AE8BCD958F0 wds:Q59712971-7F7B88FA-13EA-488E-8CDC-010ABB7D1199 wds:Q59712971-9810C028-6706-43A4-BFDF-A2442862E0E6 wds:Q59712971-A937746C-5F08-49F6-93B2-76E4FF2D7446
cites work	Magnetism and thermal evolution of the terrestrial planets Rheology of the upper mantle: a synthesis Tectonics and evolution of Venus. Venus: a contrast in evolution to Earth Speculations on the Thermal and Tectonic History of the Earth Melting of garnet peridotite to 13 GPa and the early history of the upper mantle Melting of peridotite at uppermost lower-mantle conditions Heat transfer and horizontally averaged temperature of convection with large viscosity variations Convection experiments in fluids with highly temperature-dependent viscosity and the thermal evolution of the planets
author name string	wds:Q59712971-13159231-A5FC-4874-8408-68BE0C87DCFE wds:Q59712971-9A576710-BEF5-48CA-9169-3DD28FB0875F wds:Q59712971-F02A6B40-A519-4163-B18B-F7607FD5EA17
author name string	V. S. Solomatov C. C. Reese L.-N. Moresi
rdfs:label	Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (en) Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (nl)
skos:prefLabel	Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (en) Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (nl)
name	Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (en) Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (nl)
title	wds:Q59712971-5E62D370-23A9-45F4-A1DB-6DDE411F7F14
title	Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus (en)
page(s)	wds:Q59712971-D149CA27-31C3-4ACF-8E93-8441620FF489
page(s)	13643-13657
instance of	wds:Q59712971-5D4066BB-2772-422F-9BE5-19F8436BDC0E
instance of	scholarly article
main subject	wds:Q59712971-0DAE8D04-6133-4A9B-B9CD-3A3CDE96CDEB
main subject	Mars
published in	wds:Q59712971-1DE20ABC-4449-4469-95A5-4BF965DBEDDA
published in	Journal of Geophysical Research
issue	wds:Q59712971-AB02FB67-0C49-4C15-ACD7-FADBB4DCE53D
volume	wds:Q59712971-FDC10C08-B072-4E05-998B-30DF9185734B
issue	E6
volume	103
DOI	wds:Q59712971-BC30AA87-D776-48AB-9E3F-F845559F84F8
DOI	http://dx.doi.org/10.1029/98JE01047
DOI	10.1029/98JE01047
ADS bibcode	wds:Q59712971-1F8B1E21-C3DB-43C2-8080-E3419BAC31BF
ADS bibcode	1998JGR...10313643R
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q59712971
is cites work of	3D thermal convection with variable viscosity: can transient cooling be described by a quasi-static scaling law? Clues to the lithospheric structure of Mars from wrinkle ridge sets and localization instability Scaling of time-dependent stagnant lid convection: Application to small-scale convection on Earth and other terrestrial planets Heat transport in stagnant lid convection with temperature- and pressure-dependent Newtonian or non-Newtonian rheology Tidal heating and convection in Io Survival of Archean cratonal lithosphere Magma oceans and enhanced volcanism on TRAPPIST-1 planets due to induction heating 142Nd evidence for early Earth differentiation Simulating the thermochemical magmatic and tectonic evolution of Venus's mantle and lithosphere: Two-dimensional models Grain size variations in the Earth's mantle and the evolution of primordial chemical heterogeneities
is cites work of	wds:Q64385621-DB31A88C-73F0-4948-B9AD-DEC86A17C58D wds:Q59712966-9B862797-CB14-4569-B873-42A940DBC1E4 wds:Q60146339-730EC398-1C79-4BA5-99CA-3BC71C5D2DF1 wds:Q107269107-1B067610-C138-4AF1-BD7E-A6371371DE6B wds:Q107271028-3F3D5767-CA0E-4AA4-B5AB-5AFC4CD680C7 wds:Q69202132-285723EF-3963-4F56-A86F-EB689122581F wds:Q69661255-FA9D16F7-02D9-4190-97F8-52E06E02FDA2 wds:Q55923290-9A44253D-7263-4D5E-A8C9-FADB34B891D0 wds:Q59737887-FD9958B1-8ED7-4E77-8CA8-9EBE69A87083 wds:Q56031775-974D314B-A807-433D-8376-6FE77CC635E0

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