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Sierra Maestra Range

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Eastern Cuba and isoseismals scheme and the epicenter of the August 20, 185...
Published: 01 November 2010
: Cauto River, G: Guantánamo, GG: Guacanayabo Gulf, GI: Gibara, GP: Gran Piedra Range, H: Holguín, J: Jiguaní, JO: Jobabo, M: Manzanillo, MA: Mayarí, N: Niquero, NV: Nuevitas, P: Pilón, PPA: Puerto Padre, PM: Punta de Maisí, SC: Santiago de Cuba, SL. San Luis, SMR: Sierra Maestra Range, ST: Sagua de
Image
Santiago de Cuba area (SANTO DOMINGO 066 (–AI denomination–)). 1: Cathedral...
Published: 01 November 2010
of the bay, 10: Sierra Maestra Range, 11: Mar Verde Fort, SC Bay: Santiago de Cuba Bay, SCC: Santiago de Cuba City.
Image
Cuban megablock according to  Cotilla et al. (1991) . ( a ) Heavy black lin...
Published: 01 February 2010
; SC, Santiago de Cuba City; SCB, Santiago de Cuba Bay. Other structures: GPR, Gran Piedra Range. ( c ) Eastern Cuba. Localities: B, Baitiquirí; C, Camgüey; G, Guantánamo; H, Holguín; M, Mayarí; SC, Santiago de Cuba City; SMR, Sierra Maestra Range. Other structures: OF, Oriente Fault; OT, Oriente
Journal Article
Published: 01 November 2010
Russ. Geol. Geophys. (2010) 51 (11): 1227–1246.
...: Cauto River, G: Guantánamo, GG: Guacanayabo Gulf, GI: Gibara, GP: Gran Piedra Range, H: Holguín, J: Jiguaní, JO: Jobabo, M: Manzanillo, MA: Mayarí, N: Niquero, NV: Nuevitas, P: Pilón, PPA: Puerto Padre, PM: Punta de Maisí, SC: Santiago de Cuba, SL. San Luis, SMR: Sierra Maestra Range, ST: Sagua de...
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Journal Article
Published: 01 June 2007
Russ. Geol. Geophys. (2007) 48 (6): 505–522.
...) linked to the aforementioned regional structures ( Cotilla and Alvarez, 1999 ). The Sierra Maestra tectonic structure is essential for understanding the seismic activity of eastern Cuba ( Fig. 5 ). The Sierra Maestra is an E-W trending mountain range. In particular, its southern margin has rocks...
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Journal Article
Published: 01 December 1922
Bulletin of the Seismological Society of America (1922) 12 (4): 199–219.
..., thus separating the two islands. According to this hypothesis the Southern Range of Haiti extending~ along the Tiburon Peninstfla would be a horst lying between the two branches of a fault system. The Cayman Islands-Sierra Maestra-North Haiti fault zone .ex- tends along the north side of the Bartlett...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1932
AAPG Bulletin (1932) 16 (6): 533–555.
... up to a kilometer in length are included within the serpentine areas of Camaguey and western Oriente provinces. Cretaceous pyroclastics and limestones are reported on the northern flank of the Sierra Maestra in Oriente Province. Also the lignite series which occurs in the upper Cauto Valley...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1969
AAPG Bulletin (1969) 53 (12): 2494–2500.
... (1967a , b) regards the Tres Guanos as a Late Jurassic intrusion; Meyerhoff and Hatten (1968) believe the Tres Guanos to be Paleozoic. Localities 7–9 ( Table 1 ; Fig. 1 ) are in the Sierra Maestra west and east of Santiago de Cuba, along the south coast of Oriente Province. The 46–58 m.y. dates...
FIGURES
Journal Article
Published: 01 September 1912
Bulletin of the Seismological Society of America (1912) 2 (3): 161–180.
... between the two great land-masses of the southern range: La Selle and La Hotte. The fact that an earth- quake "transgresses," in the etymological sense of the word, has been seen equally well in the earthquake of 1842, which shook the north of the Grande Hilera of Haiti and the south of the Sierra Maestra...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1975
AAPG Bulletin (1975) 59 (5): 838–855.
... similar to that proposed by Malfait and Dinkelman (1972 , their Fig. 9). The minor deformation of the volcanic belt of the Sierra Maestra of Oriente Province, contrasted with the deformation in the volcanic rocks of the rest of Cuba, is explained by the fact that this range is somewhat removed from...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1949
AAPG Bulletin (1949) 33 (8): 1319–1335.
... of an uplift whose axis probably passes through the Coxcomb Mountains and perhaps continues through the Cayman Islands toward the Sierra Maestra of southeast Cuba. In the Taxco-Chilpancingo basin, whose separation from the Balsas basin is not well defined, are several folds such as the Zapotitlan...
FIGURES
Journal Article
Published: 01 February 2010
Russ. Geol. Geophys. (2010) 51 (2): 228–236.
...; SC, Santiago de Cuba City; SCB, Santiago de Cuba Bay. Other structures: GPR, Gran Piedra Range. ( c ) Eastern Cuba. Localities: B, Baitiquirí; C, Camgüey; G, Guantánamo; H, Holguín; M, Mayarí; SC, Santiago de Cuba City; SMR, Sierra Maestra Range. Other structures: OF, Oriente Fault; OT, Oriente...
FIGURES
Journal Article
Published: 01 November 2009
The Journal of Geology (2009) 117 (6): 685–692.
... physiographic domains of northwestern South America. BGB = Baja Guajira basin, GS = Guajira Serranias, MB = Maracaibo basin, PR = Perija Range, RB = Ranchería basin, SDB = south Caribbean deformed belt, SM = Sierra Nevada de Santa Marta. B , Geological map of northern Colombia and location...
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Journal Article
Published: 01 November 2011
The Journal of Geology (2011) 119 (6): 619–640.
... within the ophiolites of eastern Cuba ( fig. 1 c ; Iturralde-Vinent et al. 2006 ; Proenza et al. 2006 ), and a tholeiitic Paleogene complex (Sierra Maestra), which developed only in eastern Cuba (fig. 1 b , 1 c ; 60.5 ± 2.2 to 46.9 ± 0.1 Ma; Kysar et al. 1998 ; Rojas-Agramonte et...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1954
AAPG Bulletin (1954) 38 (5): 707–773.
... and the Sierra Maestra of Cuba through Hispaniola and Puerto Rico. As in the ranges that form their counterpart in the south, the axes of individual folds trend obliquely across the ranges and shore lines. But here they trend east-southeastward, while there they bear east-northeastward. A complementary set...
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Journal Article
Published: 01 September 2004
The Journal of Geology (2004) 112 (5): 521–542.
... ; Iturralde-Vinent 1997 , 1998 ; Kerr et al. 1999 ). On its south side, the ophiolite mélange is overthrust by a belt containing the main Cretaceous volcano-plutonic arc that forms the axis of the island. A younger, east-west trending Paleogene volcanic arc that makes up the Sierra Maestra covers...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1943
AAPG Bulletin (1943) 27 (11): 1407–1533.
..., and in the Sierra Madre Oriental from the region of Saltillo southward to southern Nuevo León and southwestern Tamaulipas. Its thickness ranges from about 200 to more than 1,400 feet. The La Caja formation is the offshore equivalent of the La Casita formation and consists of thin-bedded limestone, marl, and shale...
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Journal Article
Journal: Geosphere
Published: 21 November 2019
Geosphere (2020) 16 (1): 210–228.
... – 38 . Rojas-Agramonte , Y. , Neubauer , F. , Bojar , A.-V. , Hejl , E. , Handler , R. , and García-Delgado , D.E. , 2006 , Geology, age and tectonic evolution of the Sierra Maestra Mountains, southeastern Cuba : Geologica Acta , v. 4 , p. 123 – 150 , https://doi.org...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1960
AAPG Bulletin (1960) 44 (8): 1273–1315.
... where they attain their maximum southerly extent, lies for the most part in the Department of Alta Verapaz but extends southward into northern Baja Verapaz. Of the frontal ranges in the report area, the most prominent are the Sierra de Chama and the Sierra de Chichen. These are an eastward extension...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1953
AAPG Bulletin (1953) 37 (4): 690–777.
... or received its principal configuration in the movements of that period. The Mio-Pliocene movements are also responsible for the development of the large geographic features of the country. The Andes and Sierra de Perijá attained their maximum elevations and extension. The Lara-Falcón ranges rose...
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