The application of trishear algorithm, in which deformation occurs in a triangle zone in front of a propagating fault tip, is often used to understand fault related folding. In comparison to kink-band methods, a key characteristic of trishear algorithm is that non-uniform deformation within the triangle zone allows the layer thickness and horizon length to change during deformation, which is commonly observed in natural structures. An example from the Lenghu5 fold-and-thrust belt (Qaidam Basin, northern Tibetan Plateau) is interpreted to help understand how to employ trishear forward modelling to improve the accuracy of seismic interpretation. High resolution fieldwork data, including high-angle dips, ‘dragging structures’, thinning hanging...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
The application of trishear algorithm, in which deformation occurs in a triangle zone in front of a ...
The investigation of complex geological setting is still dominated by traditional geo-data collectio...
Basement structures, to which trichear fault-propagation models have most successfully been applied,...
Understanding the detailed fault architecture of reverse faulting is critical for understanding the ...
Master's thesis in Petroleum Geosciences EngineeringTeapot Dome is a Laramide fault-propagation fold...
This paper focuses on the strain modelling of extensional fault-propagation folds to reveal the effe...
The investigation of complex geological setting is still dominated by traditional geo-data collectio...
Situated near the northeastern edge of the Tibetan Plateau, the Sha Gou fault area (SGFA) represents...
The Qaidam Basin, especially its western part, is characterized by numerous northwest-trending folds...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
The application of trishear algorithm, in which deformation occurs in a triangle zone in front of a ...
The investigation of complex geological setting is still dominated by traditional geo-data collectio...
Basement structures, to which trichear fault-propagation models have most successfully been applied,...
Understanding the detailed fault architecture of reverse faulting is critical for understanding the ...
Master's thesis in Petroleum Geosciences EngineeringTeapot Dome is a Laramide fault-propagation fold...
This paper focuses on the strain modelling of extensional fault-propagation folds to reveal the effe...
The investigation of complex geological setting is still dominated by traditional geo-data collectio...
Situated near the northeastern edge of the Tibetan Plateau, the Sha Gou fault area (SGFA) represents...
The Qaidam Basin, especially its western part, is characterized by numerous northwest-trending folds...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...
International audienceThe morphological boundary between the Himalayas and the foreland plain is wel...