Ophioliticlastic Ihungia igneous conglomerate (Early Miocene), North Island, New Zealand: evidence for an island source related to subduction initiation and deposition within a slump-generated submarine slope re-entrant
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| Description | article |
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author: Nick Mortimer Colin Mazengarb |
| Publication date | April 3, 2014 |
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| Missing/wrong data? | Edit Wikidata item |