Aesthetically appealing thrust systems and related large-scale anticlines, in both active and
fossil foreland fold-and-thrust belts, and the economic potential associated with them, have …

There is considerable variability in the thickness, structure, and macroscopic deformation
style within shale-prone major thrust zones, which also impacts the structural style in the …

The evolution of the Eurekan deformation zones in the Arctic is closely related to the
development of the circum-Greenland plate boundaries in Early Cenozoic times (53–34 Ma) …

Out‐of‐sequence thrusts (OOST) are those thrusts which do not obey the foreland
propagating or in‐sequence deformation style. They include both isolated thrusts which …

The foothills of the northern segment of the Magallanes basin between 47° and 49° S
latitudes record the development of a complex fold-and-thrust belt in the Patagonian …

Abstract The Argentine Precordillera (AP) represents a high-level fold-and-thrust belt which
was formed during the Andean (Tertiary) crustal shortening. In a WE transect studied, mostly …

The EW trending Yanshan belt, an intraplate fold‐thrust belt located in the northern North
China Craton that has experienced several episodes of deformation widely separated in …

Приводится обзор современных представлений о геометрии, кинематике,
геологических методах изучения и нефегазоносности складчато-надвиговых поясов …

Analysis of synorogenic deposits preserved near the thrust front zone of the Precordillera
fold and thrust belt and in the Bermejo foreland basin in central Argentina documents the …

The Subandean Zone of Bolivia is a foreland fold and thrust belt which forms the eastern
edge of the central Andes mountains. Between 19° S and 22° S latitude, the construction of …