The origin of the magnetic record in Eocene-Miocene coarse-grained sediments deposited in hyper-arid/arid conditions: Examples from the Atacama Desert

dc.creatorPizarro, H.
dc.creatorRousse, S.
dc.creatorRiquelme, R.
dc.creatorVeloso Espinosa, Eugenio Andrés
dc.creatorCampos, E.
dc.creatorGonzález, R.
dc.creatorBissigd, T.
dc.creatorCarretier , S.
dc.creatorFernández-Morta, A.
dc.creatorMuñoz, S.
dc.date.accessioned2019-10-07T16:24:13Z
dc.date.available2019-10-07T16:24:13Z
dc.date.created2019-10-07T16:24:13Z
dc.date.issued2019
dc.identifier10.1016/j.palaeo.2018.12.009
dc.identifier0031-0182
dc.identifierhttps://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=tsmetrics&SrcApp=tsm_test&DestApp=WOS_CPL&DestLinkType=FullRecord&KeyUT=ISI:000456903000026
dc.identifierhttps://repositorio.uc.cl/handle/11534/26468
dc.rightsacceso restringido
dc.subjectAtacama paleoclimate
dc.subjectMagnetic proxies
dc.subjectAtacama gravels
dc.subjectPaleoenvironmentWetland deposits
dc.subjectPaleosols
dc.titleThe origin of the magnetic record in Eocene-Miocene coarse-grained sediments deposited in hyper-arid/arid conditions: Examples from the Atacama Desert
dc.typeartículo


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