The Volcanology of Venera and VEGA Landing Sites and the Geochemistry of Venus

J. S. Kargel, G. Komatsu, Victor Baker, R. G. Strom

Research output: Contribution to journalArticle

59 Citations (Scopus)

Abstract

Magellan images confirm volcanic interpretations of television panoramas and geochemical data obtained by Venera and VEGA landers. Magellan and Venera/VEGA data are consistent with mafic volcanic compositions at all seven landing sites, although such compositions were proven at only three sites. Rock analyses show an unexpectedly high fraction of potassium-rich lavas. If the seven Venera and VEGA samples are approximately representative of the upper crust, just 10 km of the average material distributed globally would contain as much potassium as contained in Earth's continental and oceanic crust. Despite the likelihood that Venus' crust is overwhelmingly mafic, in terms of highly incompatible elements it may represent the differentiated magmatic equivalent of Earth's granitoid continents and of the Moon's anorthositic highlands. Although associated tectonic and petrogenetic aspects of lunar and Venusian crustal genesis were different, crust-forming processes on both objects (and possibly early terrestrial continent formation) may have involved cataclysmic partial melting of large fractions of these planets' mantles. A fairly mafic alkaline character of Venus' crust is attributed to a generally anhydrous, carbonated composition of Venus' mantle, which contrasts with a generally uncarbonated and variably hydrated composition of Earth's mantle. Aside from this important difference, Venus' mantle is geochemically almost identical to Earth's and is distinct from all other planetary objects for which compositional data exist. The compositional similarity of the mantles of Venus and Earth implies that the combined geochemical effects of nebular condensation, planetary accretion, and core formation were not substantially different for these planets.

Original languageEnglish (US)
Pages (from-to)253-275
Number of pages23
JournalIcarus
Volume103
Issue number2
DOIs
StatePublished - Jun 1993

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landing sites
volcanology
Venus (planet)
geochemistry
Venus
crusts
Earth mantle
mantle
continents
crust
planets
potassium
planet
highlands
television
moon
granitoid
upper crust
oceanic crust
continental crust

ASJC Scopus subject areas

  • Astronomy and Astrophysics
  • Space and Planetary Science

Cite this

The Volcanology of Venera and VEGA Landing Sites and the Geochemistry of Venus. / Kargel, J. S.; Komatsu, G.; Baker, Victor; Strom, R. G.

In: Icarus, Vol. 103, No. 2, 06.1993, p. 253-275.

Research output: Contribution to journalArticle

Kargel, J. S. ; Komatsu, G. ; Baker, Victor ; Strom, R. G. / The Volcanology of Venera and VEGA Landing Sites and the Geochemistry of Venus. In: Icarus. 1993 ; Vol. 103, No. 2. pp. 253-275.
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