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- The Cordilleran orogenic system, comprised of an interrelated forearc accretionary complex, magmatic arc, retroarc hinterland, Sevier fold-thrust belt, and foreland basin locally deformed by Laramide arches, developed during Jurassic to Paleogene Andean-style subduction and terrane accretion.
Author: W. Adolph Yonkee, Arlo Brandon WeilPublish Year: 2015www.sciencedirect.com/science/article/pii/S0012825215300258 - People also ask
Cordilleran orogenic belt - SpringerLink
These additional elements form the central and southern Rocky Mountains and the Colorado Plateau. The edge of the miogeosynclinal area of Paleozoic and Mesozoic time was west of these ranges and plateaus, in central Utah The area to the east was part of the North American craton until late in Paleozoic time, … See more
The structures of the Northern Cordillera terminate southward along the Lewis and Clark lineament, a zone of west-northwest-trending faults in western Montana and northern Idaho, south of which the … See more
Wide areas of the deformed geosynclinal rocks in the southern part of the Great Basin were covered in early to mid-Tertiary time by silicic volcanic rocks, including widely spread sheets of ignimbrites. Even … See more
Along the Pacific coast of California are various mountains: the Coast ranges in the north that are separated from the Sierra Nevada by the Great Valley and the Transverse ranges and Peninsular ranges farther south. They include rocks and structures that are younger than those to the east and that are still in the process of deformation. In … See more
Fold-thrust belt - Idaho State University
- Studies of cordilleran belt structure
The broad mountainous region of western North America is known as the "Cordillera"1, an orogenic belt that extends from South America (the Andean Cordillera) through Canada …
Fold and thrust belts: structural style, evolution and …
Jul 31, 2020 · The outer parts of collision mountain belts are commonly represented by fold and thrust belts. Many of the key concepts in the structural geology of fold and thrust belts have origins in ancient orogens such as the …
Regional structure and kinematic history of the …
The geometry, structure, and stratigraphic architecture of the Belt-Purcell basin controlled the architecture of the Cordilleran thrust belt of north-central …
- Author: Facundo Fuentes, Peter G. DeCelles, Kurt N. Constenius
- Publish Year: 2012
Tectonic evolution of the Sevier and Laramide belts within the …
Generalized map of the North American Cordilleran system shows current distribution of major tectonic elements, including Jurassic–Eocene accretionary complexes, forearc basins, …
Cyclicity in Cordilleran orogenic systems | Nature Geoscience
Mar 15, 2009 · Cordilleran orogenic systems, such as the modern Andes, are long belts of deformation and magmatism that are associated with the subduction of oceanic plates …
- Author: Peter G. DeCelles, Mihai N. Ducea, Paul Kapp, George Zandt
- Publish Year: 2009
Structure of orogenic belts controlled by lithosphere age
Aug 18, 2013 · Figure 1 shows that shortening estimates vary significantly between the world’s orogenic belts. Shortening is strongest in the Himalayan and the North-America Cordilleran …
(PDF) Cyclicity in Cordilleran orogenic systems
Mar 15, 2009 · Cordilleran orogenic systems, such as the modern Andes, are long belts of deformation and magmatism that are associated with the subduction of oceanic plates beneath continental ones.
Fold and Thrust Belts: Structural Style, Evolution and Exploration
Apr 14, 2020 · The outer parts of collision mountain belts are commonly represented by fold and thrust belts. Major advances in understanding these tectonic settings have arisen from regional studies that integrate diverse geological information in quests to find and produce hydrocarbons.
The North American Cordilleran Anatectic Belt
Apr 1, 2021 · The North American Cordilleran Anatectic Belt (CAB) is a ~3,000 km long region in the hinterland of the Cordillera that comprises numerous exposures of Late Cretaceous to …
The Role of Shortening in the Sevier Hinterland Within …
Apr 30, 2021 · We then use this compilation to interpret shortening in the Sevier hinterland in the broader space-time context of shortening in adjacent components of the Cordilleran retroarc thrust system, including the LFTB to …
(PDF) Regional structure and kinematic history of the Cordilleran …
Oct 1, 2012 · The Cordilleran thrust belt of northwestern Montana (United States) has received much less attention than its counterparts in the western interior of USA and Canada.
Intra-oceanic subduction shaped the assembly of Cordilleran
Apr 3, 2013 · The widely accepted explanation posits that the oceanic Farallon plate acted as a conveyor belt, sweeping terranes into the continental margin while subducting under it.
The Cordilleran Foreland Thrust Belt in Northwestern Montana …
Jun 1, 1991 · COCORP and petroleum industry seismic reflection profiles in northwestern Montana reveal the structure of the Cordilleran foreland thrust belt. The Front Ranges consist …
The geometry, structure, and stratigraphic architecture of the Belt-Purcell basin controlled the architecture of the Cordilleran thrust belt of north-central Montana and southern Canada (Price …
The Cordilleran orogenic belt between Nevada and Chihuahua
The Cordilleran orogenic belt of North America was formed during an orogeny which occurred mainly in Cretaceous and Paleocene time. The belt is marked by a zone of strong folding and …
Structure of the central Canadian Cordilleran thrust-and-fold belt ...
Jun 1, 1996 · The Canadian Cordilleran foreland thrust-and-fold belt, as a classic example of thin-skinned tectonics, was described. Three types of first order decollements were identified within …
Hot Cordilleran hinterland promoted lower crust mobility ...
May 4, 2024 · Protracted subduction of the Farallon plate generated two phases of deformation that partially overlap in space and time: (i) the Early to Late Cretaceous Sevier fold-and-thrust …
Chapter 3 - Structure and Architecture - Alberta Geological Survey
The Middle Jurassic to Eocene compressive deformation of the western edge of the WCSB formed the Cordilleran structural elements - the Foreland Fold and Thrust Belt and the …
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