Fold-and-thrust (FAT) belts occur worldwide and have long been the focus of research of structural geologists who have devised a variety of techniques to image, characterize and model their main structural features. This introductory chapter reviews the principal geological features of FAT belts formed in different settings, emphasizing aspects related to their kinematic evolution and structural styles. Despite great advances, challenges remain, particularly in the understanding of the spatial and temporal evolution (4D) of FAT belts and their controlling factors. These research efforts are being assisted by the growing availability to researchers of relatively new tools to collect field data, high quality 3D seismic data, and computer and ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Fold-and-thrust (FAT) belts occur worldwide and have long been the focus of research of structural g...
Fold-and-thrust (FAT) belts occur worldwide and have long been the focus of research of structural g...
The deformation front of an orogen is defined as a zone or surface separating regions of different d...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Deformation in fold-and-thrust belts such as the Himalayas can be represented by the displacement ve...
Deformation in fold-and-thrust belts such as the Himalayas can be represented by the displacement ve...
Concepts are a critical element in our ability to understand and categorise natural phenomena. Indee...
The repeated opening and closure of oceans along the same trends, and the consequent fragmentation a...
The repeated opening and closure of oceans along the same trends, and the consequent fragmentation a...
The repeated opening and closure of oceans along the same trends, and the consequent fragmentation a...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Fold-and-thrust (FAT) belts occur worldwide and have long been the focus of research of structural g...
Fold-and-thrust (FAT) belts occur worldwide and have long been the focus of research of structural g...
The deformation front of an orogen is defined as a zone or surface separating regions of different d...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Deformation in fold-and-thrust belts such as the Himalayas can be represented by the displacement ve...
Deformation in fold-and-thrust belts such as the Himalayas can be represented by the displacement ve...
Concepts are a critical element in our ability to understand and categorise natural phenomena. Indee...
The repeated opening and closure of oceans along the same trends, and the consequent fragmentation a...
The repeated opening and closure of oceans along the same trends, and the consequent fragmentation a...
The repeated opening and closure of oceans along the same trends, and the consequent fragmentation a...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...
Collisional mountain belts are the product of deformation of former continental margins. During the ...