ABSTRACT: The objective of the present study was to interpret the direction of gravitational sedimentary flows in the turbidite deposits of the Maracangalha Formation (Recôncavo Basin), indicating the
Summary of reconstructed rigidity (Te) and topography of the northern Tian Shan along the section zones A to H, and sensitivity analysis of topography reconstruction.
The Marivan granitoid body of the northern Sanandaj–Sirjan Zone (N-SaSZ) of northwest Iran was emplaced into Cretaceous sediments, and is associated with minor amounts of iron skarn-type mineralizatio
