In:
Elements, Mineralogical Society of America, Vol. 18, No. 6 ( 2022-12-1), p. 393-398
Abstract:
Io is famous for its active volcanoes, but its vigorous tectonics, which are unlike Earth’s plate tectonics, are no less remarkable. The nature of Io’s thick, cold, brittle lithosphere has been revealed through decades of investigations. The dynamics of this system is most easily explained by considering three cycles: magmatic, tectonic, and sulfurous. The magmatic cycle transports heat by a “heat pipe” process that may have operated during the earliest histories of many of the rocky bodies in the Solar System. The subsidence of the erupted lavas drives mountain uplift in the tectonic cycle. Sulfurous fluids could have a significant impact on the movement of both heat and rock.
Type of Medium:
Online Resource
ISSN:
1811-5217
,
1811-5209
DOI:
10.2138/gselements.18.6.393
Language:
English
Publisher:
Mineralogical Society of America
Publication Date:
2022
detail.hit.zdb_id:
2177991-0
detail.hit.zdb_id:
2170756-X
SSG:
13
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