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Sevier orogeny information


Geography of Sevier Orogeny
An example of thin-skinned thrusting in Montana where the white Madison Limestone is repeated, with one occurrence in the foreground (that pinches out with distance) and another to the upper right corner and top of the photo.
ContinentNorth America
BordersUnited States and Canada

The Sevier orogeny was a mountain-building event that affected western North America from northern Canada to the north to Mexico to the south.

Location of the Sevier Fold and Thrust Belt (highlighted in red). After Yonkee and Weil (2015).[1]

The Sevier orogeny was the result of convergent boundary tectonic activity, and deformation occurred from approximately 160 million years (Ma) ago[2] to around 50 Ma.[3] This orogeny was caused by the subduction of the oceanic Farallon Plate underneath the continental North American Plate. Crustal thickening that led to mountain building was caused by a combination of compressive forces and conductive heating initiated by subduction, which led to deformation.[4] The Sevier River area of central Utah is the namesake of this event.

  1. ^ Yonkee, W. Adolph; Weil, Arlo Brandon (2015-11-01). "Tectonic evolution of the Sevier and Laramide belts within the North American Cordillera orogenic system". Earth-Science Reviews. 150: 531–593. doi:10.1016/j.earscirev.2015.08.001. ISSN 0012-8252.
  2. ^ Giallorenzo, M.A.; Wells, M.L.; Yonkee, W.A.; Stockli, D.F.; Wernicke, B.P. (2018-03-01). "Timing of exhumation, Wheeler Pass thrust sheet, southern Nevada and California: Late Jurassic to middle Cretaceous evolution of the southern Sevier fold-and-thrust belt". GSA Bulletin. 130 (3–4): 558–579. doi:10.1130/B31777.1. ISSN 0016-7606.
  3. ^ Decelles, Peter G. (1994-01-01). "Late Cretaceous-Paleocene synorogenic sedimentation and kinematic history of the Sevier thrust belt, northeast Utah and southwest Wyoming". GSA Bulletin. 106 (1): 32–56. doi:10.1130/0016-7606(1994)106<0032:LCPSSA>2.3.CO;2. ISSN 0016-7606.
  4. ^ Cite error: The named reference Utah was invoked but never defined (see the help page).

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80 million years ago, the Sevier Orogeny created mountains much higher than those found in western Utah today. The Sevier Desert was formed starting...

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include gypsum and other evaporites, mined from the Arapien Shale. The Sevier orogeny to the west shed gravel and other sediments into the Morrison Formation...

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Belt Supergroup, with folds from compression that dates back to the Sevier Orogeny 50 to 100 million years ago. The rock was deposited 1.5 billion years...

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rate of subduction off the west coast increased in the Middle Jurassic Sevier Orogeny. At the same time, an inland sea began to encroach on the continent...

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and uplift of the Rocky Mountains (late Cretaceous Sevier orogeny and the Paleogene Laramide orogeny). Tectonic highlands supplied the Eocene sedimentary...

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were thrust faulted over the Precambrian craton during the Cretaceous Sevier orogeny. These rocks were later intruded and altered in the Tertiary by granitoid...

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composed primarily of the still growing Sevier Mountains; formed from shallow thrust faulting caused by the Sevier orogeny. As the shoreline moved back and forth...

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heavily deformed by faulting, folding, and overthrusting. During the Sevier orogeny mountain-building event about 115 and 55 million years ago, what is...

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over much younger Madison Limestone; this faulting was part of the Sevier orogeny. Within the canyon, caves and folded layers of Madison Limestone are...

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to 80 million years ago during the Cretaceous. This was part of the Sevier orogeny. All told there have been more than 50 plutons found in the park. A...

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Greenhorn Limestone

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limestones in the Greenhorn are associated with volcanic events in the Sevier orogeny. The oceanic iron (Fe) and volcanic sulfur (S) that precipitated with...

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accretions occurred, crustal shortening accompanied them during the Sevier orogeny and during the Mesozoic into the early Cenozoic, and was accompanied...

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about at times when very high sea levels coincided with the nearby Sevier orogeny that affected Laramidia to the west and Caribbean large igneous province...

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forming the undulating Nevadaplano. As the Farallon Plate subducted, the Sevier Orogeny generated large mountain ranges in the east. In the Mesozoic, the subducting...

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vast foreland basin east of the coastal mountains thrown up by the Sevier orogeny. The increasing weight of the Sonoma mountains to the west drove subsidence...

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