Fold and thrust belt
A fold and thrust belt is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to major orogens as deformation propagates outwards. Fold and thrust belts usually comprise both folds and thrust faults, commonly interrelated. They are commonly also known as thrust-and-fold belts, or simply thrust-fold belts.
Thrust belts
- The Zagros fold and thrust belt, located in Iran and Iraq, a young and active deforming belt.
Europe
Thrustbelt Name | Age | Structural Style |
---|---|---|
Alps | Cenozoic | |
Scandinavian Caledonides | Ordovician - Devonian | |
Carpathians | Mesozoic - Tertiary |
North America
Thrustbelt Name | Age | Structural Style |
---|---|---|
Alaska Range | Late Cretaceous - Cenozoic | Thick-skin |
Anadyr Range | Late Paleocene - Eocene | Unknown |
Antler Thrustbelt | Carboniferous | Thin-skin |
Appalachians | Late Paleozoic | Thin-skin |
Arctic Cordillera | Middle Devonian - Early Carboniferous | Unknown |
Brooks Range | Jurassic - Early Cretaceous, Early Cenozoic | Thin-skin |
California Coast Ranges | Late Miocene - Quaternary | Transpressional |
Chihuahua Belt | Paleocene | Unknown |
Chugach Mountains | Cenozoic | Thin-skin |
Sierra Madre Oriental | Early Cenozoic | Unknown |
Innuitian Fold-Thrust Belt | Late Cretaceous - Early Cenozoic | Thin-skin |
Kuskokwim Mountains | Late Cretaceous - Eocene | Unknown |
Mackenzie Mountains | Late Cretaceous - Middle Eocene | Thin-skin |
Maria Fold and Thrust Belt | Cretaceous | Thick-skin |
North Greenland Fold Belt | Middle Devonian - Early Carboniferous | Unknown |
Northern Ellesmere Fold Belt | Middle Devonian - Early Carboniferous | Thin-skin |
Ogilvie Mountains | Late Cretaceous - Eocene | Thin-skin |
Oregon Accretionary Prism | Late Miocene - Quaternary | Thin-skin |
Ouachitas | Late Carboniferous - Early Permian | Thick- and thin-skin |
Richardson Mountains | Late Cretaceous - Middle Eocene | Thin-skin |
Rocky Mountains | Paleocene to Middle Eocene | Thick-skin |
Selwyn Fold Belt, Yukon[1] | Late Cretaceous | Unknown |
South Canadian Rockies | Late Jurassic - Eocene | Thin-skin |
Sierra Madre Occidental | Cretaceous - Eocene | Unknown |
Wyoming-Utah Thrustbelt (North Sevier) | Late Jurassic - Eocene | Thin-skin |
Much of this table is adapted from Nemcok et al., 2005[2]
South America
Thrustbelt Name | Age | Structural Style |
---|---|---|
Magallanes (Fuegian) fold and thrust belt | Late Cretaceous - Cenozoic | Thin skin |
Central Andean fold and thrust belt | Mesozoic - Cenozoic | Thin skin[3] |
References
- ↑ Selwyn Basin Metallogeny Yukon Geological Survey
- ↑ Nemcok, M., Schamel, S. & Gayer, R. 2005. Thrustbelts - Structural Architecture, Thermal Regimes and Petroleum Systems. Cambridge University Press ISBN 978-0-521-82294-7
- ↑ THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES. 1997.