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pro vyhledávání: '"Denis M. Schlatter"'
Autor:
George L. Guice, Iain McDonald, Hannah S. R. Hughes, Denis M. Schlatter, Kathryn M. Goodenough, John M. MacDonald, John W. Faithfull
Publikováno v:
Geosciences, Vol 8, Iss 9, p 338 (2018)
The relative depletion of high field strength elements (HFSE), such as Nb, Ta and Ti, on normalised trace-element plots is a geochemical proxy routinely used to fingerprint magmatic processes linked to Phanerozoic subduction. This proxy has increasin
Externí odkaz:
https://doaj.org/article/9fdaf19bfb2f4e9ca70dcfc2a44f16a7
