The formation of tonalitic and granodioritic melt from Venusian basalt

The crust of Venus is composed of the low lying volcanic planitiae and the elevated, deformed tesserae. It is thought that the tesserae may be composed of silicic igneous rocks and that it may resemble proto-continental crust. The initial development of terrestrial continental crust is likely due to...

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Bibliographic Details
Published inScientific reports Vol. 12; no. 1; pp. 1652 - 7
Main Authors Wang, Yao Jui, Shellnutt, J. Gregory, Kung, Jennifer, Iizuka, Yoshiyuki, Lai, Yu-Ming
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 31.01.2022
Nature Publishing Group
Nature Portfolio
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