Results 261 to 270 of about 165,337 (293)
Some of the next articles are maybe not open access.
, 2021
The occurrence of Lower Paleozoic mafic magmatic rocks in the Central Iberian Zone (CIZ) of the Variscan Orogen is rare. Amphibolites and metagabbros embedded in the metasediments of the Douro-Beiras Supergroup outcrop at Farminhao, Viseu (central-north ...
B. Cotrim +4 more
semanticscholar +1 more source
The occurrence of Lower Paleozoic mafic magmatic rocks in the Central Iberian Zone (CIZ) of the Variscan Orogen is rare. Amphibolites and metagabbros embedded in the metasediments of the Douro-Beiras Supergroup outcrop at Farminhao, Viseu (central-north ...
B. Cotrim +4 more
semanticscholar +1 more source
Geological Magazine, 2010
AbstractTrilobites from the upper unit of the Lower Cambrian Pusa Formation (south-central Spain) substantially antedate other Iberian trilobites, according to widely published correlation schemes, and arguably would be among the earliest trilobites globally.
Jensen, Rolf Sören +2 more
openaire +2 more sources
AbstractTrilobites from the upper unit of the Lower Cambrian Pusa Formation (south-central Spain) substantially antedate other Iberian trilobites, according to widely published correlation schemes, and arguably would be among the earliest trilobites globally.
Jensen, Rolf Sören +2 more
openaire +2 more sources
Cadomian orogenic collapse in the Ibor and Alcudia anticlines of the Central Iberian Zone, Spain
Geological Magazine, 2021In the Central Iberian Zone, the Cadomian orogenic collapse is represented by chaotic megabreccias, olistostromes and mélange deposits reflecting a drastic change from slope-related deposits, fed by denudation of the Cadomian arc, to offshore-dominant ...
J. Álvaro, S. Lorenzo
semanticscholar +1 more source
The basal Cambrian carbon isotope excursion revealed in the Central Iberian Zone, Spain
Precambrian ResearchThe causes of early metazoan diversification during the Ediacaran-Cambrian transition interval are controversial, partly because the global correlation of the Ediacaran-Cambrian boundary remains problematic due to a lack of unambiguous stratigraphic ...
Kun Zhang +5 more
semanticscholar +1 more source
2023
The Iberian Massif presents a complex Late Paleozoic evolution, with intense compressional tectonics followed by gravitational collapse of the thickened crust and orocline development. In NW Iberia, extensional detachments and associated shear zones developed during high temperature-low pressure metamorphism in relation to partial melting in gneiss ...
Irene Pérez Cáceres +9 more
openaire +1 more source
The Iberian Massif presents a complex Late Paleozoic evolution, with intense compressional tectonics followed by gravitational collapse of the thickened crust and orocline development. In NW Iberia, extensional detachments and associated shear zones developed during high temperature-low pressure metamorphism in relation to partial melting in gneiss ...
Irene Pérez Cáceres +9 more
openaire +1 more source
Minerals
The Junqueira massif is a syn- to late-kinematic Variscan batholith intruded into Ediacaran-Cambrian metasedimentary rocks of the Douro-Beiras Supergroup (DBSG) in the Central Iberian Zone.
L. Portela +4 more
semanticscholar +1 more source
The Junqueira massif is a syn- to late-kinematic Variscan batholith intruded into Ediacaran-Cambrian metasedimentary rocks of the Douro-Beiras Supergroup (DBSG) in the Central Iberian Zone.
L. Portela +4 more
semanticscholar +1 more source
The Canadian Journal of Mineralogy and Petrology
The Belvís de Monroy granite-pegmatite system (Cáceres, Spain) is located in the Central Iberian Zone and intrudes the Schist-Graywacke Complex between the Belvís de Monroy granite-pegmatite system and the Navalmoral de la Mata granites.
Nora Santos-Loyola +4 more
semanticscholar +1 more source
The Belvís de Monroy granite-pegmatite system (Cáceres, Spain) is located in the Central Iberian Zone and intrudes the Schist-Graywacke Complex between the Belvís de Monroy granite-pegmatite system and the Navalmoral de la Mata granites.
Nora Santos-Loyola +4 more
semanticscholar +1 more source
Insights into petrogenesis of the Jálama pluton (Central Iberian Zone, western Spain)
International Geology Review, 2018ABSTRACTThe Jalama pluton (JP) is a Variscan peraluminous granitoid that intruded into low-grade metasediments from the Central Iberian Zone (CIZ). It comprises a sillimanite-bearing two-mica monzogranite in the inner zone, followed by a tourmaline-bearing two-mica monzogranite, and a marginal tourmaline-muscovite leucogranite in the northern half of ...
A. Pesquera +3 more
semanticscholar +2 more sources
, 2021
In this paper we report a combined zircon U–Pb–O isotopes and bulk-rock Sr–Nd–O isotopes study on granitic rocks from the Jalama pluton, Central Iberian Zone. Zircon U--Pb ages of representative granitic rock samples are bracketed in the range of 306–304
A. Pesquera, P. Montero, P. Gil-Crespo
semanticscholar +1 more source
In this paper we report a combined zircon U–Pb–O isotopes and bulk-rock Sr–Nd–O isotopes study on granitic rocks from the Jalama pluton, Central Iberian Zone. Zircon U--Pb ages of representative granitic rock samples are bracketed in the range of 306–304
A. Pesquera, P. Montero, P. Gil-Crespo
semanticscholar +1 more source

