From seafloor spreading to uplift: the structural and geochemical evolution of Macquarie Island on the Australian-Pacific plate boundary
text Macquarie Island (54º30’S, 158º54’E) is unique, consisting of a section of uplifted oceanic crust and upper mantle that still lies within the ocean basin where it formed. Earlier geophysical studies indicate that between ~40 and 6 Ma, this plate boundary evolved from a spreading ridge to the mo...
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Format: | Thesis |
Language: | English |
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2003
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Online Access: | http://hdl.handle.net/2152/1056 |