3-D Visualization and Interpretation of Branching Unconformities
Wirth, Bastian,
Stefan Back, Peter Kukla,
This study concerns the detailed analysis of the
three-dimensional morphology of laterally amalgamated unconformities on 3D
seismic data. The study area covers a block of 10 x 15 km in a Jurassic to
Cretaceous rift system in the
The approach presented
comprises 1) the mapping of unconformities by picking seismic boundary
surfaces that are defined by reflection discontinuities, and 2) an integrated
analysis of lap surface geometry, subsidence development and hiatus maps. Our
interpretation results show a distinct contrast in unconformity character
between structural highs and basinal areas: discontinuity surfaces on
structural highs are generally represented by angular contacts, reflecting
major material removal during a multistage erosional history. Unconformity
surfaces of the basin areas are predominantly lapsurfaces, often lacking erosional
truncation. Both areas are linked by a transition zone, in which discontinuity
surfaces onlap stepwise on older unconformities and converge towards structural
highs, accompanied with an increase in unconformity diachronism.