Relevant bibliographies by topics / Northern Caribbean plate

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  1. Journal articles

Academic literature on the topic 'Northern Caribbean plate'

Author: Grafiati
Published: 25 May 2024

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Journal articles on the topic "Northern Caribbean plate"

1

Corbeau, J., F. Rolandone, S. Leroy, et al. "How transpressive is the northern Caribbean plate boundary?" Tectonics 35, no. 4 (2016): 1032–46. http://dx.doi.org/10.1002/2015tc003996.

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2

Styron, Richard, Julio García-Pelaez, and Marco Pagani. "CCAF-DB: the Caribbean and Central American active fault database." Natural Hazards and Earth System Sciences 20, no. 3 (2020): 831–57. http://dx.doi.org/10.5194/nhess-20-831-2020.

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Abstract. A database of ∼250 active fault traces in the Caribbean and Central American regions has been assembled to characterize the seismic hazard and tectonics of the area, as part of the Global Earthquake Model (GEM) Foundation's Caribbean and Central American Risk Assessment (CCARA) project. The dataset is available in many vector GIS formats and contains fault trace locations as well as attributes describing fault geometry and kinematics, slip rates, data quality and uncertainty, and other metadata as available. The database is public and open source (available at: https://github.com/GEM
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3

Davison, I., J. N. F. Hull, and J. Pindell. "About this title - The Basins, Orogens and Evolution of the Southern Gulf of Mexico and Northern Caribbean." Geological Society, London, Special Publications 504, no. 1 (2021): NP. http://dx.doi.org/10.1144/sp504.

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This volume brings together 17 comprehensive, data-rich analyses to provide an updated perspective on the Mexican sector of the Gulf of Mexico, Florida and the northern Caribbean. The papers span a broad range of scales and disciplines from plate tectonic evolution to sub-basin-scale analysis. Papers are broadly categorized into three themes: (1) geological evolution of the basins of the southern Gulf of Mexico in Mexico, Bahamas and Florida and their hydrocarbon potential; (2) evolution of the region's Late Cretaceous to Neogene orogens and subsequent denudation history; and (3) geological ev
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4

Calais, Eric, and Bernard Mercier de Lepinay. "From transtension to transpression along the northern Caribbean plate boundary off Cuba: implications for the Recent motion of the Caribbean plate." Tectonophysics 186, no. 3-4 (1991): 329–50. http://dx.doi.org/10.1016/0040-1951(91)90367-2.

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5

Escuder-Viruete, J., A. Suárez-Rodríguez, J. Gabites, and A. Pérez-Estaún. "The Imbert Formation of northern Hispaniola: a tectono-sedimentary record of arc-continent collision and ophiolite emplacement in the northern Caribbean subduction-accretionary prism." Solid Earth Discussions 7, no. 2 (2015): 1827–76. http://dx.doi.org/10.5194/sed-7-1827-2015.

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Abstract. In northern Hispaniola, the Imbert Formation (Fm) has been interpreted as an orogenic "mélange" originally deposited as trench-fill sediments, an accretionary (subduction) complex formed above a SW-dipping subduction zone, or the sedimentary result of the early oblique collision of the Caribbean plate with the Bahama Platform in the middle Eocene. However, new stratigraphical, structural, geochemical and geochronological data from northern Hispaniola indicate that the Imbert Fm constitutes a coarsening-upward stratigraphic sequence that records the transition of the sedimentation fro
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6

Escuder-Viruete, J., Á. Suárez-Rodríguez, J. Gabites, and A. Pérez-Estaún. "The Imbert Formation of northern Hispaniola: a tectono-sedimentary record of arc–continent collision and ophiolite emplacement in the northern Caribbean subduction–accretionary prism." Solid Earth 7, no. 1 (2016): 11–36. http://dx.doi.org/10.5194/se-7-11-2016.

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Abstract. In northern Hispaniola, the Imbert Formation (Fm) has been interpreted as an orogenic “mélange” originally deposited as trench-fill sediments, an accretionary (subduction) complex formed above a SW-dipping subduction zone, or the sedimentary result of the early oblique collision of the Caribbean plate with the Bahama Platform in the middle Eocene. However, new stratigraphical, structural, geochemical and geochronological data from northern Hispaniola indicate that the Imbert Fm constitutes a coarsening-upward stratigraphic sequence that records the transition of the sedimentation fro
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7

Larue, D. K. "Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone." Marine and Petroleum Geology 17, no. 5 (2000): 656. http://dx.doi.org/10.1016/s0264-8172(99)00067-7.

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8

Corbeau, J., F. Rolandone, S. Leroy, et al. "The northern Caribbean plate boundary in the Jamaica Passage: Structure and seismic stratigraphy." Tectonophysics 675 (April 2016): 209–26. http://dx.doi.org/10.1016/j.tecto.2016.03.022.

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9

Rodríguez-Zurrunero, A., J. L. Granja-Bruña, A. Muñoz-Martín, et al. "Along-strike segmentation in the northern Caribbean plate boundary zone (Hispaniola sector): Tectonic implications." Tectonophysics 776 (February 2020): 228322. http://dx.doi.org/10.1016/j.tecto.2020.228322.

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10

Cerón, John F., James N. Kellogg, and Germán Y. Ojeda. "BASEMENT CONFIGURATION OF THE NORTHWESTERN SOUTH AMERICA - CARIBBEAN MARGIN FROM RECENT GEOPHYSICAL DATA." CT&F - Ciencia, Tecnología y Futuro 3, no. 3 (2007): 25–49. http://dx.doi.org/10.29047/01225383.474.

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The oceanic nature of the crust in northern Colombia (underlying the Lower Magdalena Basins) has been postulated by different authors as a northern extension of the Cretaceous, mafic and ultramafic rocks accreted to the western margin of northwest Colombia (in the Western Cordillera and Baudo range). Localized, small outcrops of oceanic affinity rocks seem to support this hypothesis. However, geophysical data do not support this northern extension, but clearly mark the boundary between the collisional Panamá terrane with northern South America and the over thrusting of the latter on top of the
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