WESTERN-CARIBBEAN Phanerozoic Tectonic

Deformations as Recorded in the Cuban Foldbelt

ITURRALDE-VINENT, Manuel A.Museo Nacional de Historia Natural, Obispo no. 61,

Plaza de Armas, La Habana 10100 Cuba, iturralde@mnhnc.inf.cu

Many tectonic elements which today built-up the Cuban foldbelt, originally where part of the Mesozoic North American passive margins and the Proto-Caribbean and Caribbean crusts.

They are represented by the Bahamian-North Cuban foldbelt, the Cuban Southwestern Terranes and the Northern Ophiolites.

Nueva Gerona

La Habana

Pinar del Rio

Matanzas

Cienfuegos

Santa Clara

Trinidad

Camaguey

Holguin

Santiago de Cuba

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

20°N 20°N

21°N 21°N

22°N 22°N

23°N 23°N

0 100 200 KM

Bahamian margin

Yucatán margin

Guaniguanicoterrane

Pinosterrane Escambray

terrane

Asunciónterrane

Gibara

Cubitas

Camaján

The North American continental margin units crops out along the northern half of the island (Bahamian borderland) and as the Cuban Southwestern terranes (Mayan borderland).

Bahamian borderland

Mayan (Yucatan) borderland

Nueva Gerona

La Habana

Pinar del Rio

Matanzas

Cienfuegos

Santa Clara

Trinidad

Camaguey

Holguin

Santiago de Cuba

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

20°N 20°N

21°N 21°N

22°N 22°N

23°N 23°N

0 100 200 KM

Bahamian margin

Yucatán margin

Guaniguanicoterrane

Pinosterrane Escambray

terrane

Asunciónterrane

Gibara

Cubitas

Camaján

In the sections of the Bahamian borderland there is no record of Mesozoic tectonic deformation or regional metamorphism.

Deformation and very low degree of metamorphism took place only during the Early Tertiary (Paleocene-Eocene).

The Mesozoic stratigraphy of both the Guaniguanico and Escambray terranes are very similar, but the Pinos terrane differ in representing a more continental-ward set of siliciclastic and carbonate rocks.

An important distinction in the Mesozoic geological history of these terranes is the age of their tectonic deformations and metamorphism.

Nueva Gerona

La Habana

Pinar del Rio

Matanzas

Cienfuegos

Santa Clara

Trinidad

Camaguey

Holguin

Santiago de Cuba

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

20°N 20°N

21°N 21°N

22°N 22°N

23°N 23°N

0 100 200 KM

Bahamian margin

Yucatán margin

Guaniguanicoterrane

Pinosterrane Escambray

terrane

Asunciónterrane

Gibara

Cubitas

Camaján

Nueva Gerona

La Habana

Pinar del Rio

Matanzas

Cienfuegos

Santa Clara

Trinidad

Camaguey

Holguin

Santiago de Cuba

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

20°N 20°N

21°N 21°N

22°N 22°N

23°N 23°N

0 100 200 KM

Bahamian margin

Yucatán margin

Guaniguanicoterrane

Pinosterrane Escambray

terrane

Asunciónterrane

Gibara

Cubitas

Camaján

In the Guaniguanico terrane there is no record of Mesozoic tectonic deformation or regional metamorphism. Deformation took place during Paleocene and early Middle Eocene.

The Escambray and Pinos terranes suffered deformation and metamorphism during the Cretaceous. K-Ar datings in these terranes record thermal events at the end of the Cretaceous (Pinos 78 - 65 Ma; Escambray 85 - 65 Ma). Ar-Ar and U-Pb dating record ages around 100 Ma.

The deformations of the North American continental margin took place in progression from Cretaceous to Late Eocene.

Nueva Gerona

La Habana

Pinar del Rio

Matanzas

Cienfuegos

Santa Clara

Trinidad

Camaguey

Holguin

Santiago de Cuba

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

85°W 84°W 83°W 82°W 81°W 80°W 79°W 78°W 77°W 76°W 75°W 74°W

20°N 20°N

21°N 21°N

22°N 22°N

23°N 23°N

0 100 200 KM

Cretaceous

Paleocene-Middle Eocene

Guaniguanicoterrane

Pinosterrane Escambray

terrane

Asunciónterrane

Gibara

Cubitas

Middle to Upper Eocene

Age of the deformations in the continental margin areas

Bahamas

Yucatán

Caribbean

Gulf of Mexico

South America

Guaniguanico

PinosEscambray

ORIGINAL POSITION OF THE CUBAN TERRAINS

BAHAMAS

The deformations along the continental margins of North America have some important implications:

1. Is quite probably that these deformations record the interaction between the North American Plate (NOAM) and the Caribbean Plate (CARIB).

2. The oldest deformations are recorded in the Pinos and Escambray terranes, suggesting that they were the first to interact with CARIB.

3. The youngest deformations are identified along the Guaniguanico terrane and the Bahamian borderland, recording the so called CARIB “collision” with the Bahamas.

Cuban ophiolites

Within the Northern Cuban Ophiolites occur inclusions of HP/LT metamorphic rocks, including metasedimentary ones,

whose K-Ar age range from 126±9.6 - 67 ±10.4 Ma.

Nueva Gerona

La Habana

Pinar del Rio

Matanzas

Cienfuegos

Santa Clara

Trinidad Ciego de Avila

Cabaiguan

FloridaCamaguey

Victoria de las TunasHolguin

GuantanamoSantiago de Cuba

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20°N 20°N

21°N 21°N

22°N 22°N

23°N 23°NNN

0 100 200 KM

Yucatán borderland

Northern Ophiolites

Bahamian borderland

Volcanic arc (K-Cretaceous, P-Paleogene)K P

Pinos terrane

Escambray terrane

Guaniguanicoterrane

P-Volcanic arc

K-Volcanic arcCretaceous arcs

Paleogene arcc

Deformations within the

Volcanic Arcs

Within the sections of the volcanic arcs can be recorded a number of regional deformational events. These deformations took place during the Aptian, Coniacian-Santonian, late Campanian, Maastrichtian-Paleocene and Middle Eocene.

Every deformation is associated with local hiata, conglomerates, changes in the geochemistry of the magmas, and with plutonite emplacement -sometimes very large as during the latest Cretaceous and the Middle-Late Eocene.

The deformations within the Northern Ophiolites and the Volcanic Arcs have additional implications:

1. Is quite probably that these deformations record intraplate tectonic events of the Caribbean (CARIB) and Proto-Caribbean Plates (P-CARIB).

2. The fact that P-CARIB elements (Northern ophiolites) suffered deformations since the Early Cretaceous, suggest that this plate had had a rather complicate history.

3. The punctuated deformations recorded within the volcanic arcs since the Aptian, imply that the Arc terranes were deformed way before the “collision” with the Bahamas.

Paleogeographic evolution of the continental margins

Latest Triassic-Early Jurassic(205-180 m.y.)

Andeanterrains

Chortis

Mexicanterrains

PACIFICOCEAN

NORTH AMERICA

SOUTH AMERICA

AFRICA

North Atlanticrift system

A

Land environments Shallow marinesiliciclastics Deep oceanRed beds and

fresh water sediments

Western Pangeanintracontinental rift system

Land environmentsShallow marinesiliciclastics Carbonate shelf Deep ocean

Late JurassicOxfordian (154-146 m.y.)

PACIFICOCEAN

NORTHATLANTIC

CaribbeanSeaway

C

Late JurassicTithonian (141-136 m.y.)

NORTHATLANTIC

PACIFICOCEAN

ProtoCaribbean

Florida-Bahamas

Gulf ofMexico

Land environmentsShallow marine siliciclastics Carbonate shelf Deep ocean

D

-90˚ -85˚ -80˚ -75˚

15˚

20˚

25˚

Bahamas Platform

Florida Platform

Yucatan Platform

?

Chixulub

Jamaica

Cuban Platform

Late Cretaceous paleogeography of the continental margin

Cretaceous deformationand metamorphism

PINOSTERRANE

ESCAMBRAYTERRANE

NORTHERNOPHIOLITES

-90˚ -85˚ -80˚ -75˚

15˚

20˚

25˚

Bahamas Platform

Florida Platform

Yucatan Platform

Chixulub

FORELAND BASINS

PIGGYBACK BASIN

ARCYucatan

Deep

Paleocene paleogeography of the continental margin

-90˚ -85˚ -80˚ -75˚

15˚

20˚

25˚

Bahamas Platform

Florida Platform

Yucatan Platform

Chixulub

w Jamaica

FORELAND BASINS

PIGGYBACK BASIN

ARC

Eocene deformation of the continental margin

Progressive deformationof the continental margin

CONCLUSIONS

1. The deformations along the borderland of the Maya block took place from SW to NE, starting in the Cretaceous (Pinos and Escambray terranes) and lasted until the Middle Eocene (Guaniguanico terrane).

3. The deformations of the Northern Ophiolites took place from South to North, and lasted since the Cretaceous and until the Late Eocene.

2. The deformations along the Bahamian borderland took place from West to East, and embrace only the Paleocene-Late Eocene.

4. These facts corroborate the Plate Tectonic models which require that the present Caribbean Plate originated West of Pangaea, to became intercalated between North and South America since the Cretaceous.

5. Nevertheless, the same results also represent a problem for the most common Caribbean models, because none of them explain why the Bahamian borderland is deformed only during the Paleogene, while the ophiolites for a long period of time since the Early Cretaceous.

This is a contribution to IGCP Project 433:

"Caribbean Plate Tectonics"

Project 433Caribbean Plate

To learn more of this project visit our web page

www.ig.utexas.edu/CaribPlate/CaribPlate.htm

Project 433Caribbean Plate