A SOURCE TO SINK MEASUREMENT METHOD IN ANOROGENIC SETTINGS.
Abstract
We developed a double method for measuring both deposited sediment volumes (sink) based
on basins stratigraphy and eroded rock volumes in upstream catchments (source) based on
geomorphology. This method was drafted in Africa - characterized by large plateaus and plains
surrounded by passive margins and interior basins (sags and rifts) - in the frame of the TopoAfrica
project funded by the French Research Agency ANR.
Measurement of deposited sediment volumes: This measurement is based on subsurface
data (seismic lines and wells) in passive margin or rifts/sags.
• Biostratigraphic dating of reference wells and definition of a regional sequence stratigraphic
framework based on key seismic lines,
• Isochore maps from the regional propagation of key time-lines,
• Depth conversion of the isochore to isopach maps,
• Compaction of the sediments (knowledge of the lithology and the porosity),
• Measurement of the compacted volumes and quantification of the uncertainties based
on the software Volume Estimator developed by J. Braun.
Measurement of the eroded volumes: This study is based on the mapping of the characteristic
landforms of the anorogenic reliefs: the planation surfaces.
• Analysis and relative chronology of the different stepped planation surfaces: etchplains
and pediments/pediplains, and their associated incised valleys,
• Dating of the planation surfaces based on the dating (when they exist) of (1) the thin
sediment covers, (2) the contemporaneous magmatism and/or (3) the weathering profiles
(magnetostratigraphy, geochronology, chemostratigraphy..),
• Mapping of the relevant planation surfaces,
• Reconstruction of the successive topographies by restoring the initial shape of the eroded
planation surfaces by younger landforms,
• Measurement of the eroded volumes.