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Mantle dynamics and the heat flow into the Earth's continents (1995)

Lenardic, A. ; Kaula, W. M.

[s.l.] : Nature Publishing Group

Nature 378 (1995), S. 709-711

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ISSN: 1476-4687

Quelle: Nature Archives 1869 - 2009

Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik

Notizen: [Auszug] The behaviour shown in Fig. 1 has previously been interpreted as evidence of additional heat input into the base of old continental lithosphere due to a secondary scale of convection-that is, one of a smaller scale than that associated directly with the formation of tectonic plates at mid-ocean ...

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1038/378709a0

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Digitale Medien

Dynamically Plausible Hypotheses of Lunar Origin (1973)

KAULA, W. M. ; HARRIS, A. W.

[s.l.] : Nature Publishing Group

Nature 245 (1973), S. 367-369

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ISSN: 1476-4687

Quelle: Nature Archives 1869 - 2009

Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik

Notizen: [Auszug] All those who hypothesise Capture acknowledge that it is an improbable event. So mostf~7 suggest that the Moon was made somewhere near the Eajrth, which seems contrary to the thermochemically inspired v^ish to make the Moon in a different part of the Solar System. All but one4-7, however, ...

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1038/245367a0

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Earth science: The changing shape of the Earth (1983)

Kaula, W. M.

[s.l.] : Nature Publishing Group

Nature 303 (1983), S. 756-756

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ISSN: 1476-4687

Quelle: Nature Archives 1869 - 2009

Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik

Notizen: [Auszug] THE tracking of Earth satellites continues to produce new findings about Earth pro perties. The most recent finding, reported in this issue of Nature (p.757), uses 5.5 years' laser ranging to Lageos, a 60-centimetre ball of brass covered by retro-reflectors whose retrograde orbit lies at 6,000 km ...

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1038/303756a0

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