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dc.contributor.authorCanales, J. Pablo  Concept link
dc.contributor.authorCarton, Helene  Concept link
dc.contributor.authorMutter, John C.  Concept link
dc.contributor.authorHarding, Alistair J.  Concept link
dc.contributor.authorCarbotte, Suzanne M.  Concept link
dc.contributor.authorNedimovic, Mladen R.  Concept link
dc.date.accessioned2012-05-08T16:05:19Z
dc.date.available2012-05-08T16:05:19Z
dc.date.issued2012-03
dc.identifier.citationOceanography 25, no. 1 (2012): 113–115en_US
dc.identifier.urihttps://hdl.handle.net/1912/5163
dc.descriptionAuthor Posting. © The Oceanography Society, 2012. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 25, no. 1 (2012): 113–115, doi:10.5670/oceanog.2012.09.en_US
dc.description.abstractAcademic research using marine multichannel seismic (MCS) methods to investigate processes related to Earth's oceanic crust has made substantial advances in the last decade. These advances were made possible by access to state-of-the-art MCS acquisition systems, and by development of data processing and modeling techniques that specifically deal with the particularities of oceanic crustal structure and the challenges of subseafloor imaging in the deep ocean. Among these methods, we highlight multistreamer three-dimensional (3D) imaging, streamer refraction tomography, synthetic ocean bottom experiments (SOBE), and time-lapse (4D) studies.en_US
dc.description.sponsorshipThe studies highlighted here were supported by NSF OCE grants 0327885, 0327872, 0621660, and 0826481.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherThe Oceanography Societyen_US
dc.relation.urihttps://doi.org/10.5670/oceanog.2012.09
dc.titleRecent advances in multichannel seismic imaging for academic research in deep oceanic environmentsen_US
dc.typeArticleen_US
dc.identifier.doi10.5670/oceanog.2012.09


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