SEA-FLOOR STRUCTURAL OBSERVATIONS, COSTA-RICA ACCRETIONARY PRISM

By studying seafloor morphology we can make associations between near surface deformation, fluid flow and the overall structural framework o f accretionary prisms. In February, 1994 a DS/RV ALVIN program to the Costa Rica accretionary prism investigated the relationship of fluid s eepage and sediment deformation by using the distribution of chemosynt hetic communities End heat flow anomalies as indicators of fluid flow. The active normal faults that cut the hemipelagic section on the Coco s plate may provide conduits for fluids that cause the regional heat f low to be extremely low. These normal faults intersect the toe of the prism at an oblique angle, creating localized regions of increased def ormation. Positive heat flow anomalies observed at the deformation fro nt indicate diffuse fluid flow, however, we discovered no seep communi ties indicative of focused flow. The seaward-most seep communities dis covered are in a region of active out-of-sequence thrusts that cut a s ediment apron which covers the complex to within 3 km of the prism toe . Vents occur consistently at the base of the fault scarps. Dives on a mud diapir show extensive seep communities, pock marks, and authigeni c carbonates. Evidence of fluid release is on the crest which implies a low viscosity fluid migrating upward in the center of the structure. Normal faults on the upper slope can be seen in cross-section in the walls of a submarine canyon. The faults cut the slope apron and displa ce the seafloor, actively maintaining the critical taper of the prism.