Results 211 to 220 of about 6,005,072 (242)

Central Cordillera

2021
Arthur W. Snoke, James B. Chapman
openaire   +1 more source

Radiocarbon Dates on Deglaciation, Cordillera Central, Northern Peruvian Andes

Quaternary Research, 1989
AbstractThree radiocarbon dates along with relative-dating criteria place limits on the deglaciation history of Manachaque Valley, Cordillera Central. Ice retreated from the late-glacial maximum by at least 12,100 yr B.P. During ice retreat numerous moraines were deposited throughout the valley.
P.W. Birkeland, D.T. Rodbell, S.K. Short
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Crustal and uppermost mantle velocity structure beneath the Cordillera Central and Cordillera Oriental, Dominican Republic

The oblique convergence between the Caribbean and North American plates produces the tectonic complexity of Hispaniola Island. The western region is characterized by high topography bounded by dominantly reverse and oblique-slip faults along the edges of the uplifted mountain ranges, while the eastern part is lower in elevation and no important active ...
Diana Núñez, Diego Córdoba
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Magnetic Characterisation of the Tectonic Domains in the Central Cordillera, Dominican Republic

69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007, 2007
P342 Magnetic Characterisation of the Tectonic Domains in the Central Cordillera Dominican Republic C. Ayala* (IGME-Geological and Mining Institute of Spain) J.L. Garcia- Lobon (IGME-Geological and Mining Institute of Spain) J. Escuder-Viruete (IGME-Geological and Mining Institute of Spain) C. Rey-Moral (IGME- Geological and Mining Institute of Spain) &
C. Ayala, J. L. García-Lobón, J. Escuder-Viruete, C. Rey-Moral, A. Pérez-Estaún   +4 more
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An obducted ophiolite complex in the Cordillera Central of the Dominican Republic

Geological Society of America Bulletin, 1983
A weakly folded layer of ultramafic and mafic rocks characterizes the peaks and ridges of the Cordillera Central in the Dominican Republic. This layer is separated from underlying volcanic and sedimentary rocks by a prominent, highly disrupted shear zone and is interpreted as an obducted and overturned ophiolite nappe.
openaire   +1 more source

Sedimentology of large olistoliths, Southern Cordillera Central, Hispaniola

Journal of Sedimentary Research, 1992
Abstract More than 500 large, well exposed, calcareous olistoliths of Paleocene to Eocene age are exposed in the Eocene deep-water Rio Ocoa Formation of southern Hispaniola. Due to the low degree of tectonic overprint, their sedimentary characteristics can be studied in detail.
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Petrogenetic and Metallogenetic Relationships in the Eastern Cordillera Occidental of Central Peru

The Journal of Geology, 2009
Abstract Ore deposits spatially and temporally related to high‐K calc‐alkaline intrusions or domes are widespread in the central Peruvian Cordillera Occidental. Geochronology and petrochemistry of intrusive rocks associated with mineralization reveal that most ore deposits (1) were emplaced in the late Middle to early late Miocene and (2) are related ...
Thomas Bissig, Richard M. Tosdal
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Tectonosedimentary evolution of the Coastal Cordillera and Central Depression of south-Central Chile (36°30′-42°S)

Earth-Science Reviews, 2021
Andres Echaurren, Alfonso Encinas, V Valencia   +2 more
exaly  

Active Collapse in the Central Betic Cordillera: Development of the Extensional System of the Granada Basin

Applied Sciences (Switzerland), 2023
A Madarieta-Txurruka, Lourdes Gonzalez Castillo, Jesus Galindo-Zaldívar   +2 more
exaly  

Characterization of the Soapaga Fault Deformation in the Central Part of the Eastern Cordillera, Colombia

Journal of South American Earth Sciences, 2023
German Pardo-Torres, Guillermo Camargo
openaire   +1 more source