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- W103635366 startingPage "27" @default.
- W103635366 abstract "Macquarie Island, in the Southern Ocean, was formed by oceanic crust uplift due to transpressivc forcesbetween the Indian / Australian and Pacific oceanic plates, in a transpressional regime which has persisted over the last10 Ma. The amount of uplift is affected by regional isostatic compensation for crustal thickening; accompanying effectsare tilting of rocks and rotation of the southern segment of the island. Gabbro and serpentinite, in the north, and basalts,in the south, all of which were formed in the primary oceanic crust, are now exposed. Consequently, magnetic propertiesof igneous rocks on the island correlate with similar features on the Indian plate which is on both sides of it.In conflict with evidence from younger palaeontological and potassium-argon (K-Ar) dating, which may reflect laterepisodes, this suggests that the original oceanic crust composing the island was formed at the I ndian-Antarctic accretingmid-oceanic ridge around the time of anomaly 7 (27 Ma BY.)." @default.
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- W103635366 date "1988-01-01" @default.
- W103635366 modified "2023-10-16" @default.
- W103635366 title "Origin, structural and tectonic history of the Macquarie Island region" @default.
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- W103635366 doi "https://doi.org/10.26749/rstpp.122.1.27" @default.
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