Adakitic magmas: modern analogues of Archaean granitoids
Both geochemical and experimental petrological research indicate that Archaean continental crust was generated by partial melting of an Archaean tholeiite transformed into a garnet-bearing amphibolite or eclogite. The geodynamic context of tholeiite melting is the subject of controversy. It is assum...
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Published in | Lithos Vol. 46; no. 3; pp. 411 - 429 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.03.1999
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Subjects | |
Online Access | Get full text |
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