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A heat-pipe mechanism for volcanism and tectonics on VenusA heat-pipe mechanism is proposed for the transport of heat through the lithosphere of Venus. This mechanism allows the crust and lithosphere on Venus to be greater than 150 km. thick. A thick basaltic crust on Venus is expected to transform eclogite at a depth of 60 to 80 km; the dense eclogite would contribute to lithospheric delamination that returns the crust to the interior of the planet completing the heat-pipe cycle. Topography and the associated gravity anomalies can be explained by Airy compensation of the thick crust. The principal observation that is contrary to this hypothesis is the mean age of the surface that is inferred from crater statistics; the minimum mean age is about 130 Myr and this implies an upper limit of 2 cubic kilometers per year for the surface volcanic flux. If the heat-pipe mechanism was applicable on the Earth in the Archean it would provide the thick lithosphere implied by isotopic data from diamonds.
Document ID
19890009853
Acquisition Source
Legacy CDMS
Document Type
Preprint (Draft being sent to journal)
Authors
Turcotte, D. L. (Cornell Univ. Ithaca, NY, United States)
Date Acquired
September 5, 2013
Publication Date
February 20, 1989
Subject Category
Lunar And Planetary Exploration
Report/Patent Number
NASA-CR-184791
NAS 1.26:184791
Accession Number
89N19224
Funding Number(s)
CONTRACT_GRANT: NAG2-524
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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