GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2010-2014  (4)
Document type
Publisher
Years
Year
  • 1
    Publication Date: 2017-10-04
    Description: This study highlights the potential of using a low frequency multibeam echosounder for detection and visualization of shallow gas occurring several meters beneath the seafloor. The presence of shallow gas was verified in the Bornholm Basin, Baltic Sea, at 80 m water depth with standard geochemical core analysis and hydroacoustic subbottom profiling. Successively, this area was surveyed with a 95 kHz and a 12 kHz multibeam echosounder (MBES). The bathymetric measurements with 12 kHz provided depth values systematically deeper by several meters compared to 95 kHz data. This observation was attributed to enhanced penetration of the low frequency signal energy into soft sediments. Consequently, the subbottom geoacoustic properties contributed highly to the measured backscattered signals. Those appeared up to 17 dB higher inside the shallow gas area compared to reference measurements outside and could be clearly linked to the shallow gas front depth down to 5 meter below seafloor. No elevated backscatter was visible in 95 kHz MBES data, which in turn highlights the superior potential of low frequency MBES to image shallow sub-seafloor features. Small gas pockets could be resolved even on the outer swath (up to 65°). Strongly elevated backscattering from gassy areas occurred at large incidence angles and a high gas sensitivity of the MBES is further supported by an angular response analysis presented in this study. We conclude that the MBES together with subbottom profiling can be used as an efficient tool for spatial subbottom mapping in soft sediment environments.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    In:  [Talk] In: Konferenz Schall und Schwingungen, Wellen und Turbulenz in sensibler Umgebung, 17.-20.09.2012, Kiel .
    Publication Date: 2012-10-23
    Type: Conference or Workshop Item , NonPeerReviewed
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    In:  [Talk] In: The Lübeck Retreat, Collaborative Research SFB 574 Volatiles and Fluids in Subduction Zones: Climate Feedback and Trigger Mechanisms for Natural Disasters, 23.-25.05.2012, Lübeck . The Lübeck Retreat: final colloquium of SFB 574; May 23-25, 2012: program & abstracts ; pp. 35-36 .
    Publication Date: 2012-09-21
    Description: Submarine landslides are an important but underestimated geological hazard. They can destroy offshore installations like cables and oil platforms, and generate destructive tsunamis that can devastate populated shorelines regionally. Off Central and Southern Chile more than 60 submarine landslides were identified based on a unique bathymetric dataset that was continuously extended and refined over 16 years and 16 scientific cruises and that now covers ~ 90% of the continental margin. Despite of the good documentation, still little is known about the mechanisms that caused the individual slope failure events, about the frequency of such events and their relation to the powerful earthquakes that happen here each 50-100 years.To investigate the preconditioning and triggering mechanisms for the landslides we combine the highresolution swath bathymetric data set with reflection seismic profiles and sediment-echosounder data.In particular we focus on how the tectonic regime, that significantly varies along-strike, impacts on thetype, shape and frequency of slope failures. Furthermore, we investigate how the direct and instantaneous seismic loading generated by the magnitude 8.8 Maule Earthquake that ruptured partsof the study area on the 27 February of 2010 impacted on the slope stability. Such a comparison is possible as we mapped the rupture area bathymetrically before and shortly after the earthquake. Our results indicate that the spatial occurrence of two groups of landslides - lower slope collapses and failures that affect the entire slope - are closely related to the tectonic segmentation of the forearc, and that the long-time tectonic stress regime is a major factor preconditioning slope failure. The seismic loading by the Maule earthquake, on the other hand had surprisingly little effect in triggering km-size submarine landslides, albeit steep slopes, ubiquiteous mass wasting of the past and extreme vertical acceleration in the rupture area.
    Type: Conference or Workshop Item , NonPeerReviewed
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    In:  [Talk] In: 6. Scientific Work Group Meeting &COST Action ES0902 PERGAMON 7th Management Committee Meeting, 5.-7.11.2012, Gent, Belgium .
    Publication Date: 2012-10-25
    Type: Conference or Workshop Item , NonPeerReviewed
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...