ISSN:
1476-4687
Source:
Nature Archives 1869 - 2009
Topics:
Biology
,
Chemistry and Pharmacology
,
Medicine
,
Natural Sciences in General
,
Physics
Notes:
[Auszug] Earth loses internal heat in two main ways: in cooling of the ocean lithosphere, originally generated at mid-ocean ridges, and in conduction across the boundary between the mantle and the continental and oceanic lithospheres. Heat exchange between the lithosphere and the oceans then occurs through ...
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1038/421590a