Seyed Hani Motavalli Anbaran - Institute of Geophysics University of Tehran Tehran, Iran

The off-shore Makran accretionary complex is about ۱۰۰ km wide and is associated by characteristics of compressional tectonic regimes such as folding, thrusting, and intrusions. Herein, satellite potential field data are used to infer the large-scale structure of the prism.

Makran Accretionary Prism; satellite gravity data