Zobrazeno 1 - 10
of 77
pro vyhledávání: '"J.M. Tubía"'
Publikováno v:
The Journal of Geology. 122:99-111
The Sierras Interiores preserve an outstanding record of the alpine deformation along the northern border of the South Pyrenean Zone, in northern Spain. New mapping and structural data illustrate the existence of two thrust systems developed from com
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84aa57e9a42dd8602ceab5ac7012bcd3
https://doi.org/10.1086/674413
https://doi.org/10.1086/674413
Akademický článek
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Age of the magmatism related to the inverted Stephanian–Permian basin of the Sallent area (Pyrenees)
Autor:
José Julián Esteban, J.M. Tubía, Julia Cuevas, Alexander N. Larionov, Lidia Rodríguez-Méndez, Sergei Sergeev
Publikováno v:
Geological Society, London, Special Publications. 394:101-111
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2116cd54d67664f6c66e6dcba5de8aa1
https://doi.org/10.1144/sp394.2
https://doi.org/10.1144/sp394.2
Publikováno v:
Journal of Maps. 9:596-603
The Pyrenees are an Alpine chain, located between France and Spain. This map covers 592 km2 (27 × 22 km) at 1:40,000 scale of the Central Pyrenees. The map comprises the South Pyrenean Zone, an Upper Cretaceous to Paleogene succession of complex thr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e344d04056a2c0d1f59a822e3e585df
https://doi.org/10.1080/17445647.2013.839962
https://doi.org/10.1080/17445647.2013.839962
Autor:
J.M. Tubía, Julia Cuevas, Sergey Sergeev, José Julián Esteban, Diane Seward, Francisco Navarro-Vilá, Alexander N. Larionov
Publikováno v:
Tectonophysics. 603:179-188
A combination of the U–Pb SHRIMP and zircon fission-track analyses has been used to constrain the age and evolution of the extensional tectonics in the Betic Cordilleras, southern Spain. The studied rocks are dolerite dykes intruded in the Malaguid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a1d3fffc3bccc999ac50aa1069e5fda8
https://doi.org/10.1016/j.tecto.2013.05.027
https://doi.org/10.1016/j.tecto.2013.05.027
Publikováno v:
Journal of Structural Geology. 50:148-160
The Ronda peridotites form the largest mass of subcontinental mantle outcropping on land. Unlike other orogenic lherzolite massifs, the two main bodies of Ronda (the Sierra Bermeja and Sierra Alpujata massifs) are unique cases where ductile shear zon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c8b3ea2c84a46f76ab093af496433b2
https://doi.org/10.1016/j.jsg.2012.06.010
https://doi.org/10.1016/j.jsg.2012.06.010
Autor:
J.M. Tubía, Sergey Sergeev, Alexander N. Larionov, José Julián Esteban, Néstor Vegas, Julia Cuevas
Publikováno v:
Gondwana Research. 20:443-449
The main orogenic reworking of the Betic Cordillera, in southern Spain, is a consequence of a short but severe Alpine event of Aquitanian to Burdigalian age that almost erased any evidence of pre-Mesozoic orogenies. New SHRIMP analyses on zircons fro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da619d76a39ad6a70a800924c0be71ea
https://doi.org/10.1016/j.gr.2010.11.006
https://doi.org/10.1016/j.gr.2010.11.006
Publikováno v:
Journal of Structural Geology. 60:102-104
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a1e87b1bebe2ff1e54b82a2780e690e
https://doi.org/10.1016/j.jsg.2013.12.012
https://doi.org/10.1016/j.jsg.2013.12.012
Publikováno v:
Geological Magazine. 148:183-187
The hot emplacement of the Ronda peridotites (Betic Cordilleras) developed a dynamothermal aureole and partial melts that led to the intrusion of granite dykes in the peridotites. Previous geochronological data place rather broad limits for this even
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d13f649fdf0f20392d197a7278b7127c
https://doi.org/10.1017/s0016756810000737
https://doi.org/10.1017/s0016756810000737
Publikováno v:
Journal of Structural Geology. 30:380-393
This work deals with the structural evolution and kinematics of the basal dynamothermal aureole of the Ronda peridotites, located in the Sierra Bermeja massif of the Western Betic Cordilleras, in southern Spain. This aureole is characterized by: 1) a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f54cfe30c1b5c48b700039a41a24e54a
https://doi.org/10.1016/j.jsg.2007.11.010
https://doi.org/10.1016/j.jsg.2007.11.010