georefid:2001-021661SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2001-021661<gco:CharacterString>Cretaceous demise of the Moa Plate and strike-slip motion at the Gondwana margin</gco:CharacterString>2001-01-01publicationgeorefid:2001-021661Sutherland, RupertInstitute of Geological & Nuclear Sciences, Lower Hutt, New ZealandauthorHollis, ChrisauthorGeological Society of America (GSA), Boulder, CO, United StatespublisherdocumentHardcopyGeology (Boulder)29 (3)279-282Radiolaria and paleomagnetic data from Deep Sea Drilling Project Sites 595 and 596 indicate that Early Cretaceous seafloor was formed at moderate to high latitudes in the Pacific. This inference requires a Cretaceous spreading ridge south of the Pacific-Phoenix Ridge and substantial dextral strike-slip motion at the Gondwana margin. The previously unrecognized southern oceanic plate, called here the Moa plate, was obliquely subducted beneath the Gondwana margin, and material accreted from it is now part of the Eastern province of New Zealand.completedSolid-earth geophysicsStratigraphyassemblagesAustralasiabiostratigraphycontinental marginCretaceouscrustDeep Sea Drilling ProjectDSDP Site 595DSDP Site 596East PacificfaultsGondwanagravity anomaliesInvertebrataIPODLeg 91Lower CretaceousMesozoicmicrofossilsMoa PlateNew Zealandoceanic crustPacific Oceanpaleomagnetismplate tectonicsProtistaRadiolariareconstructionsea-floor spreadingSouth PacificSoutheast Pacificspreading centersstrike-slip faultssubductionurn:org.iodp:exp:91urnlargerWorkCitationcampaignurn:org.iodp:exp:91:site:595urnlargerWorkCitationstudyurn:org.iodp:exp:91urnlargerWorkCitationcampaignurn:org.iodp:exp:91:site:596urnlargerWorkCitationstudyurn:org.iodp:exp:91urnlargerWorkCitationcampaignEnglishgeoscientificInformation-165.3917-165.3151-23.5113-23.4921Inst. Geol. and Nucl. Sci., Contrib. No. 2064