This study examines the interplay between sediment dispersal along the Panama margin and the evolution of the North Panama deformed belt (NPDB) using SeaMARC II swath-mapping data and migrated seismic profiles. The NPDB is composed of folded and thrusted strata of the Colombian basin that rise to within 800 m of the sea surface along the San Bias ridge. The ridge extends for more than 200 km along strike, thereby acting as an important barrier to sediment dispersal in the eastern region of the NPDB and the Colombian basin. Sediments derived from eastern Panama are trapped in the San Bias basin, located along the landward margin of the ridge, and deflected westward before traversing the lower slope along the San Bias canyon in the central region of the NPDB. Sediment entrapment within the San Bias basin and the westward deflection of transport paths by the San Bias ridge have contributed to a recent decrease in sediment thickness along the thrust front in the eastern region of the NPDB. Sediment thickness on the underthrusting basement of the Colombian basin also decreases in the region as a result of the blockage of Magdalena fan deposits by a basement ridge located less than 20 km from the thrust front. The decrease in sediment thickness is accompanied by a decrease in the width of the NPDB in this region, suggesting a concomitant decrease in the rate of frontal accretion as compared to other regions of the NPDB. A marked decrease in the thickness and fold wavelength of accreted strata from the interior of the belt to the thrust front may result from the diversion of terrigenous sediments away from the eastern region of the belt. Convergence rates along the frontal thrust are also significantly less in this region than elsewhere in the belt. Decreased frontal accretion along the eastern region has, however, been partially offset by the incorporation of thick deposits of the San Bias basin into the rear of the belt along backthrusts. Recent accretionary growth is therefore two-sided but may have varied considerably in the past in response to shifting patterns of sediment dispersal.

The western part of the North Panama deformed belt (NPDB) undergoes a number of changes in the orientation of the frontal thrusts, in marked contrast to the eastern part of the NPDB, which shows very little change over distances of 150 km. In the western part of the belt, vergence and structural style of the frontal thrusts vary rapidly along the belt, again in contrast to the eastern part of the belt. The northeast-trending part of the western NPDB appears to be constrained in orientation by the slope of the Panama arc, which lies parallel to the thrust front. Farther west the belt trends northwest, and the thrust front migrates across the slope to the shelf area, where it has been identified by studies of the April 22, 1991, earthquake. Seismic data offshore from the surface location of this earthquake show no signs of crustal deformation, further constraining the location of the thrust front. The northwest orientation of the thrust belt on- and offshore of Costa Rica is consistent with a kinematic mechanism related to collision of Costa Rica by the Cocos Ridge. A proposal to explain the fact that the thrust front is located on the shelf, rather than at the base of the slope in its westernmost position, is impedance of thrusting as a result of the heavy load of sediment deposited by the Costa Rica fan. Thus several kinematic mechanisms are operating around the NPDB, producing very different directions of thrust belt orientation. In addition, several more mechanisms, such as slope stress, sediment loading, and possibly the structure of the lower plate, are operating to modify the orientation of the frontal thrusts.

The continental margin off the Western United States changes abruptly from the subduction type north of lat 40°38’N to the translational type south of that latitude. Along the Cascadia subduction zone in the northern area a change in structural geometry at about the Columbia River separates the Oregon structural type of fore-arc basin-ridge-slope accretionary prism from the Washington type of low accretionary plateau. This change in gross morphology results from the dominantly landward-dipping thrust faults off Oregon to seaward-dipping thrusts off Washington. Gravity anomalies along the Oregon slope have steep gradients and relatively high amplitudes, whereas off Washington the gradients and amplitudes are low. Magnetic anomalies from the down-going Juan de Fuca plate can be traced inland 100 km from the base of the Washington slope but only 20 km off Oregon. The central California translational margin is cut by several long fault zones and has five large sedimentary basins and four marginal ridges. The basins all formed in late middle Miocene, probably as a result of a change in direction of Pacific-America plate motion. Basins resting on Franciscan assemblage basement rocks show a greater structural variability than those on granitic basement. Offset of granitic rocks of the Salinian block that underlie the Farallon ridge can be restored by assuming 80 km of right lateral strike-slip along the San Gregorio fault and 600 km along the San Andreas. The San Gregorio fault may join the Hosgri-San Simeon fault zone south of Point Sur, and this fault also shows evidence for 80 to 100 km of right-lateral strike-slip. The San Gregorio-Hosgri fault system may thus be one of the longest in California. The nongranitic offshore ridges are underlain by deformed sedimentary and volcanic rocks, some of which are dated as early to middle Tertiary. A sharp change in structural style between these rocks, which were probably deformed by lower to middle Tertiary subduction, and the gently folded or undisturbed overlying strata of Miocene and younger age may represent the transition from compression associated with subduction to translational shear off central California.