The formation of SiO2-rich melts within the deep oceanic crust by hydrous partial melting of gabbros
The formation of SiO2-rich melts within the deep oceanic crust by hydrous partial melting of gabbros
About this item
Full title
Author / Creator
Publisher
Heidelberg: Springer Nature B.V
Journal title
Language
English
Formats
Publication information
Publisher
Heidelberg: Springer Nature B.V
Subjects
More information
Scope and Contents
Contents
Small amounts of felsic, evolved plutonic rocks, often called oceanic plagiogranites, always occur as veins or small stocks within the gabbroic section of the oceanic crust. Four major models are under debate to explain the formation of these rocks: (1) late-stage differentiation of a parental MORB melt, (2) partial melting of gabbroic rocks, (3) i...
Alternative Titles
Full title
The formation of SiO2-rich melts within the deep oceanic crust by hydrous partial melting of gabbros
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_proquest_journals_208178343
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_208178343
Other Identifiers
ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-006-0135-y
