![Hier klicken, um den Treffer aus der Auswahl zu entfernen](images/unchecked.gif) |
Titel |
Searching palaeoearthquakes in fault bedrock scarps based on reflectivity, erosion features and surface ruptures with terrestrial laser scanning |
VerfasserIn |
Thomas Wiatr, Klaus Reicherter, Ioannis Papanikolaou, Tomás Fernández-Steeger |
Konferenz |
EGU General Assembly 2010
|
Medientyp |
Artikel
|
Sprache |
Englisch
|
Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 12 (2010) |
Datensatznummer |
250040735
|
|
|
|
Zusammenfassung |
The terrestrial laser scanner (TLS) has been used for the investigation of escarpments
(bedrock fault scarps) at different sites in Greece in order to identify the palaeo-slip events
and rates. Our approach is based on differential weathering, karstification and bioerosion of
the subsequentially exposed limestone free face from repeated earthquake surface
faulting events. Data acquisition with the TLS method and the high-resolution spatial
surface analysis can help to improve data quality and to provide a more accurate
prediction for a plane analysis of the fault bedrock scarps. Scientific objectives are the
analysis of rock surface roughness in different scales, orientations and methods, which
may help us to determine the relative age of slip. Furthermore, the intensity of the
backscattered reflection of the scarp surface can offer us the possibility to identify different
weathering stages semi-automatically. The degradation and erosion features of
the fault plane can help to reconstruct the plane geomorphology. We applied the
LiDAR at limestone fault scarps with clear free faces that have experienced large
surface faulting events in the past, such as the Kaparelli Fault or the Sparta Fault in
mainland Greece. Some of these scarps have been dated with cosmogenic isotopes.
The results of the cosmogenic nuclide dating on scarps give an absolute age of the
individual palaeoseismological slip events. This ensures the cross validation of the TLS
data. Additionally, geodetic measurements with compass and GPS were carried
out to cross-validate the quality of the TLS point cloud data and to georeference. |
|
|
|
|
|