Publication:
Anatomy of an exhumed debrite and impact on stratal architecture

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dc.creatorMartanez Donate, Ander
dc.creatorPrivat, Aurelia
dc.creatorSpychala, Yvonne
dc.creatorHodgson, David
dc.creatorJackson, Christopher A. L.
dc.creatorKane, Ian
dc.creatorSchwarz, Ernesto
dc.creatorFlint, Stephen S.
dc.date.issued2020
dc.description.abstractSubmarine debrites generate complicated patterns of seabed relief which in uence subsequent ow behaviour and depositional patterns. However, recognizing this interaction in subsurface data is challenging in seismic and well data. To bridge this resolution gap, large-scale outcrop analogues can be used. The early post-rift Middle Jurassic succession of the Los Molles Formation is well-exposed along a 10 km long and downdip-orientated W-E outcrop belt located the western Central Neuquen Basin, Argentina.
dc.identifierAnatomy of an exhumed debrite and impact on stratal architecture; 59th British Sedimentological Research Group Annual General Meeting; Liverpool; Reino Unido; 2020; 68-69
dc.identifierhttp://hdl.handle.net/11336/172216
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://naturalis.fcnym.unlp.edu.ar/handle/628872547/57277
dc.languageeng
dc.publisherBritish Sedimentological Reseach Group
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.liverpool.ac.uk/earth-ocean-and-ecological-sciences/events/bsrg/
dc.sourceBSRG 2020 abtract volume
dc.subjectEXHUMED DEBRITE
dc.subjectDEEP WATER SYSTEMS
dc.subjectLOS MOLLES FM
dc.subjectNEUQUÉN BASIN
dc.titleAnatomy of an exhumed debrite and impact on stratal architecture
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeinfo:eu-repo/semantics/conferenceObject
dc.typeinfo:ar-repo/semantics/documento de conferencia
dspace.entity.typePublication

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