The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
The mafic dyke is metamorphosed to amphibolite-facies and is calc-alkaline with intermediate SiO 2 (∼56%) and high Al 2O 3 and TiO 2 and is transitional between basaltic to andesitic compositions. The dyke has high Sr, Zr and Ba contents. The steep chon
Bibliographic Details
Main Authors: |
Grantham, Geoff H,
Armstrong, Richard,
Moyes, A.B. |
Other Authors: |
Hanski, E.,
Mertanen, S.,
Ramo, T.,
Vuollo,
J. |
Format: | Book Part
|
Language: | unknown |
Published: |
Taylor & Francis Group
2015
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Subjects: |
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Online Access: | http://hdl.handle.net/1885/26203
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