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Keith Klepeis on How Plutons Form

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Keith Klepeis explains how magma travels from deep crustal sources into the upper crust and crystallizes into plutons. Observations from southern Fiordland in New Zealand reveal the resulting structures and constrain their origin and evolution. The discussion links magma transport with the three-dimensional organization of intrusive rocks.

Topics

MAGMAdeep crustal sourcesupper crustplutonsmagma transportintrusive rockssouthern Fiordlandthree-dimensional organization

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