(Q57855280)

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Hydrothermal heat flux through aged oceanic crust: where does the heat escape?

article by Heinrich Villinger et al published August 2002 in Earth and Planetary Science Letters

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Hydrothermal heat flux through aged oceanic crust: where does the heat escape? (English)

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Ingo Grevemeyer

2

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author name string

Heinrich Villinger

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1

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Norbert Kaul

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3

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Jan Hauschild

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4

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Marion Pfender

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5

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language of work or name

English

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publication date

August 2002

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published in

Earth and Planetary Science Letters

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volume

202

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issue

1

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page(s)

159-170

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Fundamentals of ridge crest topography

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7 January 2021

An analysis of the variation of ocean floor bathymetry and heat flow with age

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7 January 2021

A model for the global variation in oceanic depth and heat flow with lithospheric age

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7 January 2021

Submarine thermal sprirngs on the galapagos rift

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7 January 2021

Hydrothermal activity and the evolution of the seismic properties of upper oceanic crust

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Channelized fluid flow in oceanic crust reconciles heat-flow and permeability data

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Heat-flow variations correlated with buried basement topography on the Juan de Fuca Ridge flank

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Warm springs discovered on 3.5 Ma oceanic crust, eastern flank of the Juan de Fuca Ridge

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A multibeam-sonar, magnetic and geochemical flowline survey at 14°14′S on the southern East Pacific Rise: insights into the fourth dimension of ridge crest segmentation

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Segmentation of the Pacific-Nazca Spreading Center, 1°N–20°S

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7 January 2021

A map series of the Southern East Pacific Rise and its flanks, 15° S to 19° S

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reference URL

https://api.crossref.org/works/10.1016%2FS0012-821X%2802%2900759-8

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7 January 2021

Seamount abundances and Abyssal Hill Morphology on the eastern flank of the East Pacific Rise at 14°S

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reference URL

https://api.crossref.org/works/10.1016%2FS0012-821X%2802%2900759-8

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7 January 2021

Heat flow from the Earth's interior: Analysis of the global data set

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7 January 2021

Identifiers

DOI

10.1016/S0012-821X(02)00759-8

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ADS bibcode

2002E&PSL.202..159V

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(Q57855280)

Hydrothermal heat flux through aged oceanic crust: where does the heat escape?

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