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Tectonics of the Tectonics of the Caribbean Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad www.uwiseismic.com
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Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Mar 28, 2015

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Page 1: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Tectonics of the CaribbeanTectonics of the CaribbeanTectonics of the CaribbeanTectonics of the Caribbean

Richard RobertsonSeismic Research Unit, U.W.I.

St. Augustine, Trinidadwww.uwiseismic.com

Page 2: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

OutlineOutlineOutlineOutline

• Definitions: Tectonics, Caribbean Plate• Plate Tectonics• Evolution of the Caribbean• Physiographic/Tectonic Provinces• Tectonics of the Caribbean• Summary

Page 3: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

TectonicsTectonicsTectonicsTectonics

• The processes responsible for tectonic activity

• Field of study concerned with structures within the cruststructures within the crust and with forces and movementsforces and movements that operate to create these

• Concerned with mountain buildingmountain building & with the development of cratons and tectonic terranes => earthquakes, volcanoes & tsunamis

Page 4: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Melting of the more fusible constituents of the upper mantle produces magma

The Earth’s layered The Earth’s layered structurestructureThe Earth’s layered The Earth’s layered structurestructure

• Inner core: 1216 km thick and consists of solid rock at very high temperature and pressure

• Outer core: extends up to 2270 km from the centre of the earth and consists mainly of molten iron with about 10% nickel and traces of other materials

• Mantle: extends to ~ 2900 km and consists of silicate rocks; due to high temperature and pressure the rocks are able to flow extremely slowly like a thick & stick liquid

• The Mantle accounts for 83 % of the Earth’s volume & 67% of its mass

• The Upper and lower mantle separated by the 670 km seismic discontinuity

Page 5: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Lithospheric PlatesLithospheric PlatesLithospheric PlatesLithospheric Plates

Page 6: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Plate boundary settingsPlate boundary settingsPlate boundary settingsPlate boundary settings

Page 7: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

The Caribbean PlateThe Caribbean PlateThe Caribbean PlateThe Caribbean Plate

• A lithospheric platelithospheric plate consisting mainly of a unusually thick, oceanic plateau situated between two major continental regions

• A geologically complex regiongeologically complex region that displays a variety of displays a variety of plate boundary interactionsplate boundary interactions including subduction (Lesser Antilles), transcurrent/strike-slip (north & south) and sea-floor spreading (Cayman Trough)

Page 8: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

The CaribbeanThe CaribbeanThe CaribbeanThe Caribbean

Page 9: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Evolution of CaribbeanEvolution of CaribbeanEvolution of CaribbeanEvolution of Caribbean

• Allochthonous/Mobilist vs. In Situ/Fixist models for origin of Caribbean

• In-situ evolution• Gulf of Mexico & Caribbean region existed in the past i.e.

during Triassic, Jurassic & early Cretaceous• Allocthonous evolution:

• All accept significant amounts of eastward Caribbean migration relative to the Americas

• A Great Arc vs Multi-arc evolution of the region • Interpretation of the facts => A single geology and too many

points of view

Page 10: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Evolution of the Caribbean Evolution of the Caribbean PlatePlateEvolution of the Caribbean Evolution of the Caribbean PlatePlate

Page 11: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

The Caribbean IGCP The Caribbean IGCP Project 433Project 433The Caribbean IGCP The Caribbean IGCP Project 433Project 433

• Is the Caribbean Plate allochthonous or developed in situ?

• There is a single Great Arc or the compressive margins evolved as multiarcs?

• Why can not be reconcile local geology with the general models?

Page 12: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Physiographic regionsPhysiographic regionsPhysiographic regionsPhysiographic regions

Page 13: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Geologic ProvincesGeologic ProvincesGeologic ProvincesGeologic Provinces

Page 14: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Tectonics of the Caribbean Tectonics of the Caribbean - I- ITectonics of the Caribbean Tectonics of the Caribbean - I- I

• Result primarily from the interaction of one relatively small plate of lithosphere with surrounding plates

• The Caribbean – geologically complex region; variety of plate boundary interactions including: • Subduction (Lesser Antilles &

Central America)• Transcurrent (strike-slip) on

northern and southern boundaries

• Sea floor spreading in Cayman Trough

Page 15: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Tectonics of the Caribbean Tectonics of the Caribbean - II- IITectonics of the Caribbean Tectonics of the Caribbean - II- II

• Caribbean – a lithospheric plate that consists mainly of anomalously thick, oceanic plateau located between 2 major continental regions => tectonic interactions between thick oceanic crust and continental crust

Page 16: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Caribbean SeismicityCaribbean SeismicityCaribbean SeismicityCaribbean Seismicity

• First motion studies indicate left-lateral strike slip at northern & right-lateral strike slip at southern boundary => left lateral and right lateral transform boundaries

• Thrust fault solutions, typical of upper parts of convergent plate boundaries occur at western and eastern margins of plate

• Depth of hypocentres and their positions relative to island arc volcanoes indicates Wadati-Benioff Zones dipping eastward beneath Central American & westward beneath Lesser Antilles

-8 5 W -8 0 W -7 5 W -7 0 W -6 5 W -6 0 W

-8 5 W -8 0 W -7 5 W -7 0 W -6 5 W -6 0 W

Longitude

1 0 N

1 5 N

2 0 N

2 5 N

Latitude

1 0 N

1 5 N

2 0 N

2 5 N

Caribbean Earthquakes: 1964 to Caribbean Earthquakes: 1964 to 20022002Caribbean Earthquakes: 1964 to Caribbean Earthquakes: 1964 to 20022002

Page 17: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

SummarySummarySummarySummary

• The Caribbean is a geologically complex region which exhibits a variety of plate boundary interactions and by extension tectonic features

• It is a lithospheric plate that consists mainly of anomalously thick, oceanic plateau located between 2 major continental regions

• Despite recent advances in knowledge there is still disagreement over its evolution

Page 18: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

ReferencesReferencesReferencesReferences

• Mattson, Peter, H. ed. (1977): West Indies island arcs. Benchmark Papers in Geology V. 33. Dowden, Hutchinson & Ross, Inc., p. 361. (see Chapters 2, 32-35b)

• Jackson, Trevor, A. ed. (2002): Caribbean Geology into the Third Millennium – transactions of the Fifteenth Caribbean Geological Conference. University of the West Indies Press, 279p.

• Donovan, Stephen K. and Jackson, Trevor, A. (1994): Caribbean Geology – An Introduction. The University of the West Indies Publishers Association, Jamaica, 289p.

• http://www.ig.utexas.edu/CaribPlate/CaribPlate.html

Page 19: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Seismic Research UnitSeismic Research UnitSeismic Research UnitSeismic Research Unit

Earthquake & Volcano MonitoringResearch & Public Education

www.uwiseismic.com

Page 20: Tectonics of the Caribbean Richard Robertson Seismic Research Unit, U.W.I. St. Augustine, Trinidad .

Thank you for Thank you for listening!listening!

Thank you for Thank you for listening!listening!

For more information on the work of the Seismic Research Unit logon to our website at:

www.uwiseismic.com

Earthquake & Volcano MonitoringResearch & Public Education