Kinematics of late Paleozoic continental collision between Laurentia and Gondwana
Science
By: P. E. Sacks and D.T. Secor Jr.
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Abstract
In the Appalachians, late Paleozoic Alleghanian orogenesis is widely regarded as resulting from dextral oblique collision between irregular margins of Gondwana and Laurentia. However, this relative plate motion cannot account for coeval convergence in the Ouachitas and Variscides and is incompatible with some tectonic transport indicators in the Appalachians. An alternative kinematic model is proposed in which early sinistral transpression in the Appalachians is followed by counterclockwise rotation of Gondwana and the development of a system of dextral strike-slip faults extending from southern Europe to Alabama.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Kinematics of late Paleozoic continental collision between Laurentia and Gondwana |
| Series title | Science |
| Volume | 250 |
| Issue | 4988 |
| Year Published | 1990 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 1702 |
| Last page | 1705 |
| Google Analytic Metrics | Metrics page |