A fold and thrust belt (FTB) 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.
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A foldandthrustbelt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Foldand thrust...
The Zagros foldandthrustbelt (Zagros FTB) is an approximately 1,800-kilometre (1,100 mi) long zone of deformed crustal rocks, formed in the foreland...
Sevier FoldandThrustBelt extends from southern California near the Mexican border to Canada. Basin and Range faults cut the older Sevier thrust faults...
The Maria foldandthrustbelt (MFTB) is a portion of the North American Cordillera orogen in which geological structures accommodate roughly north–south...
The Cape FoldBelt is a foldandthrustbelt of late Paleozoic age, which affected the sequence of sedimentary rock layers of the Cape Supergroup in the...
eastern continuation of the Central Cordillera as a foldandthrustbelt. Between the Occidental and Central Cordillera the approximately 3,750-meter-high...
salt is mined from the Salt Range mountains, the southern edge of a fold-and-thrustbelt that underlies the Pothohar Plateau south of the Himalayas in Pakistan...
only involves the sedimentary cover. This style is typical of many foldandthrustbelts developed in the foreland of a collisional zone. This is particularly...
Ouachita orogeny was a mountain-building event that resulted in the foldingand faulting of strata currently exposed in the Ouachita Mountains. The more...
Verkhoyansk fold-and-thrustbelt, the Chersky collisional zone, and the Kolyma-Omolon microcontinent. The Verkhoyansk fold-and-thrustbelt consists of...
Mesoproterozoic, Paleozoic, and Mesozoic strata. The Lewis thrust sheet is one of the major structures of the foreland thrustandfoldbelt extending over 280 mi...
The nappes of the Flysch Belt were thrusted due to subduction of their basement and later formed andfoldandthrustbelt. The character of the lithosphere...
as seen in salt domes in the Zagros Mountains and in El Gordo diapir (Coahuila fold-and-thrustbelt, NE Mexico). If the pressure within the salt body...
located inside and parallel to the Fuegian foldandthrustbelt, and marks the boundary between a southern belt of Paleozoic meta sediments and a northern...
plate tectonics and before the internal architecture of thrustbelts became well understood, the term was used to describe most mountain belts but has otherwise...
The Moine ThrustBelt or Moine Thrust Zone is a linear tectonic feature in the Scottish Highlands which runs from Loch Eriboll on the north coast 190...
in the formation of the Marañón foldandthrustbelt. An unconformity cutting across the Marañón foldandthrustbelt show the Incaic Phase ended no later...
Complex is exposed in a set of anticlinoriums within the foreland foldandthrustbelt of the Paleoproterozoic Wopmay Orogen. The gneisses of the Acasta...
Basin is rimmed to the northwest by the Jura mountains, an external fold-and-thrustbelt, which can be seen as part of the Alps geologically. The western...
the form of emergent salt diapirs within anticlines of the Zagros foldandthrustbelt. As a result of their involvement in post-depositional salt tectonics...
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