Magnetic susceptibilities of rocks of the Antarctic Peninsula: Implications for the redox state of the batholith and the extent of metamorphic zones
A combination of 1555 magnetic susceptibility measurements from the Antarctic Peninsula between 65°S to 72°S (for which the raw data are made available), and petrological, structural and metamorphic data, has been used to improve understanding of: (1) magma sources for the Antarctic Peninsula bathol...
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Veröffentlicht in: | Tectonophysics 2013-02, Vol.585, p.48-67 |
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Sprache: | eng |
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