Geology of Jamaica: Difference between revisions
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==Restraining bend== |
==Restraining bend== |
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[[File:Gonâve microplate.png|thumb|350px|The position of Jamaica relative to major strike-slip fault zones]] |
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During the [[Late Miocene]], the northeastern margin of the Caribbean Plate began to collide with the Bahamas Platform. This caused the formation of a two new strike-slip fault zones between the island of [[Hispaniola]] and the Mid-Cayman [[spreading center]] west of Jamaica, the [[Enriquillo-Plantain Garden fault zone]] and the [[Walton fault zone]].<ref name="Mann"> |
During the [[Late Miocene]], the northeastern margin of the Caribbean Plate began to collide with the Bahamas Platform. This caused the formation of a two new strike-slip fault zones between the island of [[Hispaniola]] and the Mid-Cayman [[spreading center]] west of Jamaica, the [[Enriquillo-Plantain Garden fault zone]] and the [[Walton fault zone]].<ref name="Mann"> |
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{{cite journal |year=1995 |
{{cite journal |year=1995 |
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Revision as of 11:34, 16 January 2018
The Geology of Jamaica is formed of rocks of Cretaceous to Neogene age. The basement consists of Cretaceous island arc and back-arc basin sequences that formed above a subduction zone. The cover is of mainly Eocene to Miocene shallow water limestones, that have been uplifted due to the presence of a restraining bend along the major strike-slip faults that bound the southern edge of the Gonâve Microplate to the north of the island.
Cretaceous
Rocks of this age occur as a series of inliers within the younger limestones.[1]
Rift basins
Rifting during the Paleogene led to the formation of rift basins in which thick sequences of clastic rocks were deposited that are exposed at the eastern end of the island in the John Crow and Wagwater belts.[1]
Limestones
During the Eocene, limestone deposition started across the whole of the Nicaraguan Rise. In Jamaica the main limestone unit is the White Limestone Group, which dominates the surface exposure of the island, particularly its central parts and consists of pure limestones and dolostones. Locally the lowermost limestone is the Yellow Limestone Group, which consists of interbedded limestones and other clastic rocks.[1]
Restraining bend
During the Late Miocene, the northeastern margin of the Caribbean Plate began to collide with the Bahamas Platform. This caused the formation of a two new strike-slip fault zones between the island of Hispaniola and the Mid-Cayman spreading center west of Jamaica, the Enriquillo-Plantain Garden fault zone and the Walton fault zone.[2] These fault zones now form part of the southern boundary of the Gonâve Microplate. The major right-stepping offset between the fault zones formed a restraining bend and led to transpression and uplift which is still active today and is the reason that the island of Jamaica is now well above sea level.[3]
References
- ^ a b c Mitchell S.F. (2016). "The Geology of Jamaica".
- ^ Mann, P.; Taylor, F.W.; Edwards, R. Lawrence; Ku, Teh Lung (1995). "Actively evolving microplate formation by oblique collision and sideways motion along strike-slip faults: An example from the northeastern Caribbean plate margin". Tectonophysics. 246 (1–3): 1–69. Bibcode:1995Tectp.246....1M. doi:10.1016/0040-1951(94)00268-E. Retrieved 8 February 2010.
- ^ Mann P.; Demets C.; Wiggins-Grandison M. (2007). "Toward a better understanding of the Late Neogene strike-slip restraining bend in Jamaica: geodetic, geological, and seismic constraints". In Cunningham W.D. & Mann P. (ed.). Tectonics of Strike-slip Restraining and Releasing Bends. Geological Society, London, Special Publications. Vol. 290. p. 239–253. ISBN 9781862392380.