Gotowe bibliografie tematyczne / Northern Caribbean plate

Gotowa bibliografia na temat „Northern Caribbean plate”

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Data publikacji: 25 maja 2024

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Artykuły w czasopismach na temat "Northern Caribbean plate"

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Corbeau, J., F. Rolandone, S. Leroy, B. Meyer, B. Mercier de Lépinay, N. Ellouz-Zimmermann i R. Momplaisir. "How transpressive is the northern Caribbean plate boundary?" Tectonics 35, nr 4 (kwiecień 2016): 1032–46. http://dx.doi.org/10.1002/2015tc003996.

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Styron, Richard, Julio García-Pelaez i Marco Pagani. "CCAF-DB: the Caribbean and Central American active fault database". Natural Hazards and Earth System Sciences 20, nr 3 (25.03.2020): 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/GEMScienceTools/central_am_carib_faults, last access: 23 March 2020), will be updated progressively as new data become available, and is open to community contribution. The active fault data show deformation in the region to be centered around the margins of the Caribbean plate. Northern Central America has sinistral and reverse faults north of the sinistral Motagua–Polochic fault zone, which accommodates sinistral Caribbean–North American relative motion. The Central Highlands in Central America extend east–west along a broad array of normal faults, bound by the Motagua–Polochic fault zone in the north and trench-parallel dextral faulting in the southwest between the Caribbean plate and the Central American forearc. Faulting in southern Central America is complicated, with trench-parallel reverse and sinistral faults. The northern Caribbean–North American plate boundary is sinistral off the shore of Central America, with transpressive stepovers through Jamaica, southern Cuba and Hispaniola. Farther east, deformation becomes more contractional closer to the Lesser Antilles subduction zone, with minor extension and sinistral shear throughout the upper plate, accommodating oblique convergence of the Caribbean and North American plates.
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Davison, I., J. N. F. Hull i 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, nr 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 evolution of the basins and crustal elements of the northern Caribbean. This book and its extensive datasets are essential for all academic and exploration geoscientists working in this area. The volume also includes two large maps detailing the Mexican Gulf of Mexico and the Northern Caribbean areas.
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Calais, Eric, i 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, nr 3-4 (luty 1991): 329–50. http://dx.doi.org/10.1016/0040-1951(91)90367-2.

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Escuder-Viruete, J., A. Suárez-Rodríguez, J. Gabites i 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, nr 2 (26.06.2015): 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 from a pre-collisional forearc to a syn-collisional piggy-back basin. This piggy-back basin was transported on top of the Puerto Plata ophiolitic complex slab and structurally underlying accreted units of the Rio San Juan complex, as it was emplaced onto the North America continental margin units. The Imbert Fm unconformably overlies different structural levels of the Caribbean subduction-accretionary prism, including a supra-subduction zone ophiolite, and consists of three laterally discontinuous units that record the exhumation of the underlying basement. The distal turbiditic lower unit includes the latest volcanic activity of the Caribbean island arc; the more proximal turbiditic intermediate unit is moderately affected by syn-sedimentary faulting; and the upper unit is a (caotic) olistostromic unit, composed of serpentinite-rich polymictic breccias, conglomerates and sandstones, strongly deformed by syn-sedimentary faulting, slumping and sliding processes. The Imbert Fm is followed by subsidence and turbiditic deposition of the overlying El Mamey Group. The 40Ar / 39Ar plagioclase plateau ages obtained in gabbroic rocks from the Puerto Plata ophiolitic complex indicate its exhumation at ∼ 45–40 Ma (lower-to-middle Eocene), contemporaneously to the sedimentation of the overlying Imbert Fm. These cooling ages imply the uplift to the surface and submarine erosion of the complex to be the source of the ophiolitic fragments in the Imbert Fm, during of shortly after the emplacement of the intra-oceanic Caribbean island-arc onto the continental margin.
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Escuder-Viruete, J., Á. Suárez-Rodríguez, J. Gabites i 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, nr 1 (15.01.2016): 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 from a pre-collisional forearc to a syn-collisional basin. This basin was transported on top of the Puerto Plata ophiolitic complex slab and structurally underlying accreted units of the Rio San Juan complex, as it was emplaced onto the North America continental margin units.The Imbert Fm unconformably overlies different structural levels of the Caribbean subduction-accretionary prism, including a supra-subduction zone ophiolite, and consists of three laterally discontinuous units that record the exhumation of the underlying basement. The distal turbiditic lower unit includes the latest volcanic activity of the Caribbean island arc; the more proximal turbiditic intermediate unit is moderately affected by syn-sedimentary faulting; and the upper unit is a (chaotic) olistostromic unit, composed of serpentinite-rich polymictic breccias, conglomerates and sandstones, strongly deformed by syn-sedimentary faulting, slumping and sliding processes. The Imbert Fm is followed by subsidence and turbiditic deposition of the overlying El Mamey Group.The 40Ar ∕ 39Ar plagioclase plateau ages obtained in gabbroic rocks from the Puerto Plata ophiolitic complex indicate its exhumation at ∼ 45–40 Ma (lower-to-middle Eocene), contemporaneously to the sedimentation of the overlying Imbert Fm. These cooling ages imply the uplift to the surface and submarine erosion of the complex to be the source of the ophiolitic fragments in the Imbert Fm, during or shortly after the emplacement of the intra-oceanic Caribbean island arc onto the continental margin.
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Larue, D. K. "Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone". Marine and Petroleum Geology 17, nr 5 (maj 2000): 656. http://dx.doi.org/10.1016/s0264-8172(99)00067-7.

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Corbeau, J., F. Rolandone, S. Leroy, B. Mercier de Lépinay, B. Meyer, N. Ellouz-Zimmermann i R. Momplaisir. "The northern Caribbean plate boundary in the Jamaica Passage: Structure and seismic stratigraphy". Tectonophysics 675 (kwiecień 2016): 209–26. http://dx.doi.org/10.1016/j.tecto.2016.03.022.

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Rodríguez-Zurrunero, A., J. L. Granja-Bruña, A. Muñoz-Martín, S. Leroy, U. ten Brink, J. M. Gorosabel-Araus, L. Gómez de la Peña, M. Druet i A. Carbó-Gorosabel. "Along-strike segmentation in the northern Caribbean plate boundary zone (Hispaniola sector): Tectonic implications". Tectonophysics 776 (luty 2020): 228322. http://dx.doi.org/10.1016/j.tecto.2020.228322.

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Cerón, John F., James N. Kellogg i Germán Y. Ojeda. "BASEMENT CONFIGURATION OF THE NORTHWESTERN SOUTH AMERICA - CARIBBEAN MARGIN FROM RECENT GEOPHYSICAL DATA". CT&F - Ciencia, Tecnología y Futuro 3, nr 3 (31.12.2007): 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 obliquely convergent Caribbean plate. We produced maps to basement and Moho topography by integrated modeling of gravity, magnetics, seismic reflection surveys and well data from northwest Colombia and the southwestern Caribbean. In areas with good seismic coverage, the basement under the Lower Magdalena Basins (LMB) is represented by a clear reflector. In areas where seismic data shows poor imaging or is absent, we use a back stripping methodology to model first the sedimentary section, with known densities, composition and geometry controlled by oil wells and high quality seismic data, and then the deeper section. 2,5D gravity and magnetics modeling results in an initial Moho that can be extended to the entire region based on the control of available seismic refraction points. This controlled Moho provides the basis for basement modeling for the whole area and this sequence is iterated for several sections across the region. Our results indicate that the crust under northern Colombia is continental to thinned continental (transitional) in nature, with densities between 2,6 and 2,7 g/cm3. Our model also requires a dense wedge of sediments (density 2,5 g/cm3) at the base of the modern fold belt, which may represent a fossil sedimentary wedge attached to the continental margin. This wedge may have served as a backstop for the modern fold belt. The gravity modeling does not require oceanic crust to form the basement in the Sinú and San Jacinto fold belts as previously suggested. Discrete layers and thin slivers of oceanic sediments and basement could have been scrapped off the incoming plate and thrusted into an accretionary mélange, and eventually exposed at the surface, as seen in the Mulatos, Chalan and Cansona locations. The shape of the continental wedge / oceanic crust boundary resembles that of a very low angle/flat subduction zone (ß angle between 2º to 3º), and is interpreted here as a low angle over thrusting of northern South America riding in a highly oblique direction over the underlying Caribbean plate. The map to basement depth obtained during this study forms the basis for basin analysis, oil maturation and evolutionary studies of the region. As an example, we apply our map to a flexural analysis of the LMB.
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Rozprawy doktorskie na temat "Northern Caribbean plate"

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Oliveira, de Sa Alana. "Relations entre systèmes tectoniques et sédimentaires à la limite Nord de la plaque Caraïbe (Cuba-Hispaniola) : implications géodynamiques". Electronic Thesis or Diss., Sorbonne université, 2023. http://www.theses.fr/2023SORUS625.

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La bordure nord de la plaque Caraïbe, comprenant Cuba, Hispaniola et la République dominicaine, constitue une limite de plaque où le mouvement relatif entre les plaques Caraïbes et Amérique du Nord est accommodé par un système complexe de failles et de blocs tectoniques. Deux failles décrochantes sismogènes associées à ce système se trouvent en Haïti : la zone de faille d'Enriquillo-Plantain Garden (EGPFZ) au sud d'Haïti et la zone de faille Oriente-Septentrionale (SOFZ) au large du nord d'Haïti. Après les séismes dévastateurs de magnitude 7,0 qui s'est produit le 12 janvier 2010 au sud d'Haïti, à Leogâne, près de la capitale Port-au-Prince, et celui survenu dans la région de la faille Septentrionale à Port-de-Paix (magnitude 5,9, le 7 octobre 2018), la géologie et le contexte géodynamique d'Haïti font l'objet de nombreuses études. Cette thèse a pour objectifs principaux les suivants : 1. Identifier les phases de déformation terrestres et marines, évaluer leur impact régional, analyser leur style structural et comprendre leur évolution. 2. Retracer l'histoire de la déformation de la limite nord de la plaque Caraïbe, en relation avec le domaine marin. 3. Caractériser l'interaction entre la dynamique sédimentaire et la déformation en examinant la tectonique dans les deux régions, afin de mieux comprendre le partitionnement de la déformation et ses relations avec les systèmes sédimentaires dans un contexte de collision oblique à grande échelle de décrochements. Pour atteindre ces objectifs, cette thèse combine des données géologiques et des observations sur le terrain en Haïti, recueillies lors de deux campagnes de terrain. Les données stratigraphiques et structurales terrestres seront complétées par l'étude de cartes bathymétriques obtenues lors des récentes campagnes marines (Haitis-sis 1 & 2, Norcaribe), ainsi que par l'analyse de profils sismiques réflexion et de données du sondeur de sédiments. Cette a permis de reconstituer l'histoire de la déformation de la bordure nord de la plaque Caraïbe et d'intégrer l'ensemble des résultats dans un modèle géodynamique global
The northern boundary of the Caribbean Plate, including Cuba, Hispaniola, and the Dominican Republic, constitutes a plate boundary where the relative motion between the Caribbean and North American plates is accommodated by a complex system of faults and tectonic blocks. Two seismogenic strike-slip faults associated with this system are found in Haiti: the Enriquillo-Plantain Garden fault zone (EPGFZ) to the south of Haiti, and the Oriente-Septentrional fault zone (SOFZ) offshore to the north of Haiti. Following the devastating magnitude 7.0 earthquakes that occurred on January 12, 2010, in southern Haiti near Leogâne, close to the capital Port-au-Prince, and the earthquake that occurred in the Northern fault region in Port-de-Paix (magnitude 5.9, on October 7, 2018), the geology and geodynamic context of Haiti have been the subject of numerous studies. The main objectives of this thesis are as follows: 1. Identify terrestrial and marine deformation phases, assess their regional impact, analyze their structural style, and understand their evolution. 2. Trace the history of deformation at the northern boundary of the Caribbean Plate in relation to the marine domain. 3. Characterize the interaction between sedimentary dynamics and deformation by examining tectonics in both regions to better understand the partitioning of deformation and its relationships with sedimentary systems in the context of large-scale oblique collision of strike-slip faults. To achieve these objectives, this thesis combines geological data and field observations in Haiti collected during two field campaigns. Terrestrial stratigraphic and structural data will be supplemented by the study of bathymetric maps obtained during recent marine campaigns (Haitis-sis 1 & 2, Norcaribe), as well as the analysis of reflection seismic profiles and sediment sonar data. This has allowed for the reconstruction of the deformation history of the northern boundary of the Caribbean Plate and the integration of all the results into a global geodynamic model
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Książki na temat "Northern Caribbean plate"

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1956-, Mann Paul, red. Geologic and tectonic development of the Caribbean plate boundary in northern Central America. Boulder, Colo: Geological Society of America, 2007.

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1959-, Dolan James F., i Mann Paul 1956-, red. Active strike-slip and collisional tectonics of the Northern Caribbean plate boundary zone. Boulder, Colo: Geological Society of America, 1998.

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Dolan, James F., i Paul Mann. Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone. Geological Society of America, 1998. http://dx.doi.org/10.1130/spe326.

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Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone (Special Paper (Geological Society of America)). Geological Society of America, 1998.

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Special Paper 326: Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone. Geological Society of America, 1998. http://dx.doi.org/10.1130/0-8137-2326-4.

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Special Paper 428: Geologic and Tectonic Development of the Caribbean Plate Boundary in Northern Central America. Geological Society of America, 2007. http://dx.doi.org/10.1130/978-0-8137-2428-7.

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Mann, Paul. Special Paper 428 Geologic and Tectonic Development of the Caribbean Plate Boundary in Northern Central America. Geological Society of America, 2007. http://dx.doi.org/10.1130/spe428.

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Rivers, Larry Eugene. Destinations of Runaways. University of Illinois Press, 2017. http://dx.doi.org/10.5406/illinois/9780252036910.003.0006.

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This chapter discusses how questions related to where enslaved blacks fled have occupied historians of the southern experience for generations. Traditionally, the answers reached have pointed to the majority absconding to other southern states as opposed to the northern states. In that vein, John Hope Franklin and Loren Schweninger focused in one recent study on fugitives who fled, primarily, from one place in the South to another in the same region. Florida′s situation, however, offers a somewhat different view. Although considerable numbers of its fugitives replicated the traditional patterns noted by Franklin, Schweninger, and other historians, a significant number possessed what could be described as an Atlantic worldview. This is to say that they sought freedom in various parts of the Atlantic and Caribbean regions, particularly in the Bahamas.
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Części książek na temat "Northern Caribbean plate"

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Ostos, Marino, i Virginia B. Sisson. "Geochemistry and tectonic setting of igneous and metaigneous rocks of northern Venezuela". W Caribbean-South American plate interactions, Venezuela. Geological Society of America, 2005. http://dx.doi.org/10.1130/0-8137-2394-9.119.

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Wessels, Richard J. F. "Strike-Slip Fault Systems Along the Northern Caribbean Plate Boundary". W Transform Plate Boundaries and Fracture Zones, 375–95. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-812064-4.00015-3.

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Lallemant, Hans G. Avé, i Virginia B. Sisson. "Exhumation of eclogites and blueschists in northern Venezuela: Constraints from kinematic analysis of deformation structures". W Caribbean-South American plate interactions, Venezuela. Geological Society of America, 2005. http://dx.doi.org/10.1130/0-8137-2394-9.193.

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Sisson, Virginia B., Rebecca Kessler Cardoso, Caren Chaika Harris, Saijin Huang i Layla M. Unger. "Exhumation history of two high-pressure belts, northern Venezuela, based on fluid inclusions in quartz and calcite veins". W Caribbean-South American plate interactions, Venezuela. Geological Society of America, 2005. http://dx.doi.org/10.1130/0-8137-2394-9.157.

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Sisson, Virginia B., Hans G. Avé Lallemant, Marino Ostos, Ann E. Blythe, Lawrence W. Snee, Peter Copeland, James E. Wright, Raymond A. Donelick i Lawrence R. Guth. "Overview of radiometric ages in three allochthonous belts of northern Venezuela: Old ones, new ones, and their impact on regional geology". W Caribbean-South American plate interactions, Venezuela. Geological Society of America, 2005. http://dx.doi.org/10.1130/0-8137-2394-9.91.

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Rogers, Robert D., i Paul Mann. "Transtensional deformation of the western Caribbean–North America plate boundary zone". W Special Paper 428 Geologic and Tectonic Development of the Caribbean Plate Boundary in Northern Central America. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.2428(03).

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Calais, E., J. Perrot i B. Mercier de Lépinay. "Strike-slip tectonics and seismicity along the northern Caribbean plate boundary from Cuba to Hispaniola". W Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone. Geological Society of America, 1998. http://dx.doi.org/10.1130/0-8137-2326-4.125.

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Mann, Paul. "Overview of the tectonic history of northern Central America". W Special Paper 428 Geologic and Tectonic Development of the Caribbean Plate Boundary in Northern Central America. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.2428(01).

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Dolan, James F., Henry T. Mullins i David J. Wald. "Active tectonics of the north-central Caribbean: Oblique collision, strain partitioning, and opposing subducted slabs". W Active Strike-Slip and Collisional Tectonics of the Northern Caribbean Plate Boundary Zone. Geological Society of America, 1998. http://dx.doi.org/10.1130/0-8137-2326-4.1.

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Jordan, B. R., H. Sigurdsson, S. Carey, S. Lundin, R. D. Rogers, B. Singer i M. Barquero-Molina. "Petrogenesis of Central American Tertiary ignimbrites and associated Caribbean Sea tephra". W Special Paper 428 Geologic and Tectonic Development of the Caribbean Plate Boundary in Northern Central America. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.2428(07).

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Streszczenia konferencji na temat "Northern Caribbean plate"

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Conrad, Ethan, Claudio Faccenna, Daniel F. Stockli i Thorsten Becker. "CENOZOIC EVOLUTION OF THE NORTHERN CARIBBEAN PLATE BOUNDARY: INSIGHTS FROM THERMOCHRONOMETRIC, KINEMATIC AND GEOMORPHIC DATA". W GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-353996.

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Conrad, Ethan, Claudio Faccenna, Claudio Faccenna, Daniel F. Stockli, Daniel F. Stockli, Thorsten W. Becker i Thorsten W. Becker. "DEFORMATION AND EXHUMATION AT OBLIQUE MARGINS: A STUDY OF THE NORTHERN CARIBBEAN PLATE BOUNDARY IN THE DOMINICAN REPUBLIC, HISPANIOLA". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380024.

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Boschman, Lydian M., Douwe J. J. van Hinsbergen, Menno Fraters i Wim Spakman. "WAS THE EOCENE REORGANIZATION OF THE NORTHERN CARIBBEAN PLATE BOUNDARY FROM THE CUBAN TRENCH TO THE CAYMAN STRIKE-SLIP SYSTEM REGIONALLY OF GLOBALLY FORCED?" W GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-278675.

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