Results 41 to 50 of about 32,456 (106)
We present new U/Pb and Pb/Pb radiometric age data from two tectono-stratigraphic units of the regionally extensive Bolu Massif, in the W Pontides (Istanbul Fragment), N Turkey.
Mundil, Roland +2 more
core +1 more source
The Almendral massif is located in the north-western branch of the Olivenza-Monesterio antiform (Ossa Morena Zone, Iberian Massif, Spain). The pluton is composed by gabbros, sienites and alkaline granites which define an alkaline/transitional association.
Alonso Olazabal, Ainhoa +3 more
core
U-Pb zircon geochronology and phase equilibria modelling of HP-LT rocks in the Ossa-Morena Zone, Portugal. [PDF]
Akker IV +3 more
europepmc +1 more source
Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone [PDF]
The Late Ediacaran (c. 560–550 Ma) Série Negra sediments of the Évora–Aracena metamorphic belt, Ossa-Morena Zone, SW Iberian Massif, preserve a record of the erosion of an Avalonian–Cadomian magmatic arc and subsequent related turbiditic sedimentation ...
Fernandez, C. +6 more
core
Metasedimentary schists and a small crosscutting metagranite underlie a Mesozoic metamorphosed carbonate platform within the regional Anatolide tectonic belt of northern Turkey. These lithologies are inferred to have formed part of the northern margin of
Ustaomer, Timur +3 more
core +1 more source
Inherited arc signature in Ediacaran and Early Cambrian basins of [PDF]
Geochemical data from clastic rocks of the Ossa-Morena Zone (Iberian Massif) show that the main source for the Ediacaran and the Early Cambrian sediments was a recycled Cadomian magmatic arc along the northern Gondwana margin. The geodynamic scenario for
Linnemann, Ulf +4 more
core
Metasedimentary schists and a small crosscutting metagranite underlie a Mesozoic metamorphosed carbonate platform within the regional Anatolide tectonic belt of northern Turkey.
Timur Ustaömer (2840900) +3 more
core +1 more source
New insights from U–Pb zircon dating of Early Ordovician magmatism on [PDF]
The Central Iberian–Ossa-Morena transition zone (SW Iberian Massif) represents a segment of the northern Gondwana margin with a long geodynamic evolution, characterized by the superposition of Cadomian and Variscan events.
Montero, Pilar +7 more
core
Late-Proterozoic to Paleozoic history of the peri-Gondwana Calabria-Peloritani Terrane inferred from a review of zircon chronology. [PDF]
Fornelli A, Micheletti F, Piccarreta G.
europepmc +1 more source
Geological archive of the onset of plate tectonics. [PDF]
Cawood PA +5 more
europepmc +1 more source

