Please use this identifier to cite or link to this item: https://www.um.edu.mt/library/oar/handle/123456789/45635
Title: Holocene canyon activity under a combination of tidal and tectonic forcing
Authors: Mountjoy, Joshu
Micallef, Aaron
Stevens, Craig
Stirling, Mark
Keywords: Faults (Geology)
Sediments (Geology) -- Analysis
Canyons -- New Zealand
Morphology -- Statistical methods
Issue Date: 2013
Publisher: Copernicus GmbH
Citation: Mountjoy, J., Micallef, A., Stevens, C., & Stirling, M. (2013). Holocene canyon activity under a combination of tidal and tectonic forcing. Geophysical Research Abstracts, 15
Abstract: The majority of submarine canyon systems that are active during sea level highstands are coupled to terrestrial or littoral sediment transport systems (e.g. high sediment-yield rivers, wave-base sediment disturbance). However, non-coupled canyon systems can also exhibit sedimentary activity. Characterising the nature, origin, and spatial and temporal influence of the processes responsible for this sedimentary activity is important to understand the extent of sediment and carbon transfer to the deep sea, the impact of sedimentary flows on biological colonisation and diversity, and the control of recent seafloor processes on canyon morphology.
URI: https://www.um.edu.mt/library/oar/handle/123456789/45635
ISSN: 16077962
Appears in Collections:Scholarly Works - FacSciGeo

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