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pro vyhledávání: '"Alexandre Diragitch"'
Publikováno v:
Ore and Energy Resource Geology, Vol 1, Iss, Pp-(2019)
The lower stratigraphy of Agnew-Wiluna greenstone belt is composed of two main elements; a mafic/komatiite domain and a felsic/komatiite/basalt domain. Previous stratigraphic models show the mafic domain overlying the felsic domain. Komatiites in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d504f7fa48911096ccb3fbb7f63cba78
http://www.sciencedirect.com/science/article/pii/S266626121930001X
http://www.sciencedirect.com/science/article/pii/S266626121930001X
