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000089582 005__ 20210902121624.0
000089582 0247_ $$2doi$$a10.1130/G47008.1
000089582 0248_ $$2sideral$$a117603
000089582 037__ $$aART-2020-117603
000089582 041__ $$aeng
000089582 100__ $$aSutherland, R.
000089582 245__ $$aContinental-scale geographic change across zealandia during paleogene subduction initiation
000089582 260__ $$c2020
000089582 5060_ $$aAccess copy available to the general public$$fUnrestricted
000089582 5203_ $$aData from International Ocean Discovery Program (IODP) Expedition 371 reveal vertical movements of 1-3 km in northern Zealandia during early Cenozoic subduction initiation in the western Pacific Ocean. Lord Howe Rise rose from deep (~1 km) water to sea level and subsided back, with peak uplift at 50 Ma in the north and between 41 and 32 Ma in the south. The New Caledonia Trough subsided 2-3 km between 55 and 45 Ma. We suggest these elevation changes resulted from crust delamination and mantle flow that led to slab formation. We propose a "subduction resurrection" model in which (1) a subduction rupture event activated lithospheric-scale faults across a broad region during less than ~5 m.y., and (2) tectonic forces evolved over a further 4-8 m.y. as subducted slabs grew in size and drove plate-motion change. Such a subduction rupture event may have involved nucleation and lateral propagation of slip-weakening rupture along an interconnected set of preexisting weaknesses adjacent to density anomalies.
000089582 536__ $$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2017-84693-R
000089582 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000089582 590__ $$a5.399$$b2020
000089582 591__ $$aGEOLOGY$$b1 / 48 = 0.021$$c2020$$dQ1$$eT1
000089582 592__ $$a2.609$$b2020
000089582 593__ $$aGeology$$c2020$$dQ1
000089582 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000089582 700__ $$aDickens, G.R.
000089582 700__ $$aBlum, P.
000089582 700__ $$aAgnini, C.
000089582 700__ $$0(orcid)0000-0002-8801-9544$$aAlegret, L.$$uUniversidad de Zaragoza
000089582 700__ $$aAsatryan, G.
000089582 700__ $$aBhattacharya, J.
000089582 700__ $$aBordenave, A.
000089582 700__ $$aChang, L.
000089582 700__ $$aCollot, J.
000089582 700__ $$aCramwinckel, M.J.
000089582 700__ $$aDallanave, E.
000089582 700__ $$aDrake, M.K.
000089582 700__ $$aEtienne, S.J.G.
000089582 700__ $$aGiorgioni, M.
000089582 700__ $$aGurnis, M.
000089582 700__ $$aHarper, D.T.
000089582 700__ $$aHuang, H.H.M.
000089582 700__ $$aKeller, A.L.
000089582 700__ $$aLam, A.R.
000089582 700__ $$aLi, H.
000089582 700__ $$aMatsui, H.
000089582 700__ $$aMorgans, H.E.G.
000089582 700__ $$aNewsam, C.
000089582 700__ $$aPark, Y.H.
000089582 700__ $$aPascher, K.M.
000089582 700__ $$aPekar, S.F.
000089582 700__ $$aPenman, D.E.
000089582 700__ $$aSaito, S.
000089582 700__ $$aStratford, W.R.
000089582 700__ $$aWesterhold, T.
000089582 700__ $$aZhou, X.
000089582 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000089582 773__ $$g48, 5 (2020), 419-424$$pGeology$$tGeology$$x0091-7613
000089582 8564_ $$s815738$$uhttps://zaguan.unizar.es/record/89582/files/texto_completo.pdf$$yVersión publicada
000089582 8564_ $$s48936$$uhttps://zaguan.unizar.es/record/89582/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
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000089582 951__ $$a2021-09-02-08:49:03
000089582 980__ $$aARTICLE