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100 years of seismic research on the Moho

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dc.contributor.authorProdehl, Claus
dc.contributor.authorKennett, Brian
dc.contributor.authorArtemieva, Irina M
dc.contributor.authorThybo, Hans
dc.date.accessioned2015-12-13T23:02:10Z
dc.date.issued2013
dc.date.updated2015-12-12T07:45:25Z
dc.description.abstractThe detection of a seismic boundary, the "Moho", between the outermost shell of the Earth, the Earth's crust, and the Earth's mantle by A. Mohorovičić was the consequence of increased insight into the propagation of seismic waves caused by earthquakes.
dc.identifier.issn0040-1951
dc.identifier.urihttp://hdl.handle.net/1885/84768
dc.publisherElsevier
dc.sourceTectonophysics
dc.title100 years of seismic research on the Moho
dc.typeJournal article
local.bibliographicCitation.lastpage44
local.bibliographicCitation.startpage9
local.contributor.affiliationProdehl, Claus, University of Karlsruhe
local.contributor.affiliationKennett, Brian, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationArtemieva, Irina M, University of Copenhagen, Denmark
local.contributor.affiliationThybo, Hans, University of Copenhagen
local.contributor.authoruidKennett, Brian, u8413736
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040407 - Seismology and Seismic Exploration
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf5625xPUB13017
local.identifier.citationvolume609
local.identifier.doi10.1016/j.tecto.2013.05.036
local.identifier.scopusID2-s2.0-84889090407
local.identifier.thomsonID000330201000002
local.type.statusPublished Version

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