Print this pageHigh-Frequency Evolution of Cap Lopez Canyon (Gabon) from Annual Bathymetric Data
Biscara, Laurie 1; Mulder, Thierry 1; Hanquiez,
Vincent 1; Marieu, Vincent 1; Gallissaires, Jean-Marie 2;
Crespin, Jean-Pierre 3; Garlan, Thierry 4
(1)UMR-CNRS
5805 EPOC, Université Bordeaux 1, Talence, France. (2) IOTA SURVEY, Mauguio,
France. (3) Centre Scientifique et Technique Jean Feger, Total, Pau, France.
(4) Service Hydrographique et Océanographique de la Marine (SHOM), Brest,
France.
Sandbodies located on inner bends of meanders within deep-sea
channels can form important hydrocarbon reservoirs and are of significant
interest to the hydrocarbon industry. However, little is known about their
forming processes and their conditions of preservation. This poor understanding
is in part due to the lack of high 
resolution
geo-acoustic data. The study of
the Cap Lopez canyon, located on the Gabonese margin (West Africa) is a key
example to understand the morphological evolution of submarine channels and
their associated deposits. This paper focuses on the high resolution evolution
of this canyon on annual and multi-decennial scales, using time serial
bathymetric data acquired from 1959 to 2009.
Our results show similar rate (2-16 m/year) and way of migration
to those observed in rivers, suggesting that the Cap Lopez canyon may be
subject to very quick morphological evolutions. The lateral migration of the
thalweg at an annual scale is characterized by predominant progressive lateral
migration and catastrophic chute cutoffs related to gravity flows generated
during intense meteorologic events. It suggests that lateral migration through
time follows a linear evolution toward the development of a meandering system
(multi-decennial scale) which is the result of high frequency fluctuations
(annual scale). The lateral migration of the thalweg is performed continuously
through the erosion on the outer bank and depositional processes on the
opposite bank. This study reveals that the progressive erosion by gravity flows
is predominant compared to the establishment of large events such as mass
wasting. The erosion of the outer bends probably results in the combined action
of the erosive behaviour of gravity flows with reversal helical flow dynamic.
Finally, the comparison of the bathymetric data allowed to define several types
of terraces corresponding to the different degrees of maturity of the canyon
and to evaluate their life span.
Based on a detailed analysis of time serial bathymetric data, our
study evaluates for the first time the frequency and the degree of importance
of short term sedimentary processes responsible for the lateral migration and
meander development. This innovative approach may be of significant interest in
order to understand and eventually predict the geometry of lateral
accretion
packages.
AAPG Search and Discovery Article #90135©2011 AAPG International Conference and Exhibition, Milan, Italy, 23-26 October 2011.