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

SYSTEMATIC heat-flow variations are commonly observed on sedimented flanks of mid-ocean ridges. These variations have been attributed to the convective circulation of pore fluids within the oceanic crust, and have been used to estimate the scale and pattern of this circulation. Here we report simila...

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Veröffentlicht in:	Nature (London) 1989-11, Vol.342 (6249), p.533-537
Hauptverfasser:	Davis, Earl E., Chapman, David S., Forster, Craig B., Villinger, Heiner
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology Geology Heat flow Humanities and Social Sciences letter Marine Marine geology multidisciplinary Ocean floor Oceans Science Science (multidisciplinary)
Online-Zugang:	Volltext
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