About 2,480,000 results
Open links in new tab
  1. Through the use of seismic reflection profiles,satellite images,and balanced kinematic models,we describe patterns that help to identify imbricate structures and define the sequence of thrusting in …

  2. Aug 25, 2009 · Deep-water toe thrust anticlines have been interpreted using traditional models derived from observations in orogenic thrust belts and accretionary prisms, such as fault-propagation folds, …

  3. These observations imply relatively small distortions of the thrust sheets along the strike to accommodate variations i n displacement along the thrust surfaces.

  4. A thrust system is an interconnected network of thrust faults that are usually also kinematically linked. Horizontal shortening forces the topography upwards, creating a mountain defined as a landform …

  5. n thrust belts is duplex structure. At its sim plest, a duplex consists of two or more dipping thrusts that are bound above nd be low by sub horizontal faults. These ar called the floor and roof thrusts. The …

  6. • Deformation mainly accommodated by slip along break–forward propagation mode • Closely space thrust ramps and folded hanging–walls • Continuous individual thrust–fault planes (up to the depth of …

  7. Here, we present 2-D crustal numerical models of a shallow steep listric thrust (as 38 inferred in the region) embedded in the high viscosity upper crust, and we show that such 39 model reproduces the …