Rift-Related Structures and Their Seismic Expression: ABSTRACT

Abstract

Normal faults and associated secondary structures are common features in continental rifts. Fault dip and displacement, stratal dip, and fold position and size vary considerably. Synthetic seismic-reflection profiles show that each of these structural variables, as well as rock velocity, influences the seismic expression of rift-related structures. The observed dip and curvature of any fault on an unmigrated seismic section depend, not only on the dip and curvature of the actual fault surface, but also on the velocity and dip of the overlying strata. The observed dip of a fault decreases as the velocity of the strata directly overlying the fault increases. Thus, planar normal faults in rocks whose velocities increase with depth may appear to flatten with depth on seismic sections. The observed dip of a fault decreases as the acute angle between the fault surface and the overlying strata decreases. Consequently, on unmigrated seismic sections, normal faults dipping in the opposite direction as the strata may appear to have steeper dips than identical normal faults dipping in the same direction as the strata; planar normal faults ctive during deposition may appear to steepen with depth. The appearance of secondary structures associated with normal faulting on unmigrated seismic sections depends on the position and size of the secondary structures. A greater thickness of low-velocity rocks on the downthrown side of a normal fault may disrupt and bend the reflections on the upthrown side. Depth, rock-velocity distribution, and fault displacement affect the severity of the distortion. This distortion may obscure secondary structures on the upthrown side of faults, and can be interpreted erroneously as secondary faulting and folding. Synclines produced by drag on the downthrown sides of normal faults generally have small radii of curvature relative to their burial depths. This relationship makes them difficult to identify on unmigrated seismic sections. In contrast, forc d folds in rifts are gentle, shallow structures overlying normal faults. These folds are easier to identify because they are unaffected by the distortion beneath faults, and their synclines have large radii of curvature compared to their burial depths. End_of_Article - Last_Page 1838------------