Results 81 to 90 of about 32,456 (106)
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International Journal of Earth Sciences, 2004
Diorites and related rocks in the Merida area of northern Ossa-Morena (SW Iberia) are intrusive into Precambrian metavolcanic and metasedimentary sequences. Cumulate products from the H2O-rich magmas are amphibole-rich gabbros to hornblendites. Major and trace element compositions, including Sr and Nd isotope data, allow the definition of a calc ...
A. Bandr�s +7 more
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Diorites and related rocks in the Merida area of northern Ossa-Morena (SW Iberia) are intrusive into Precambrian metavolcanic and metasedimentary sequences. Cumulate products from the H2O-rich magmas are amphibole-rich gabbros to hornblendites. Major and trace element compositions, including Sr and Nd isotope data, allow the definition of a calc ...
A. Bandr�s +7 more
openaire +1 more source
, 2020
The Arabian-Nubian Shield (ANS) is a province of mostly juvenile Neoproterozoic continental crust in NE Africa and Arabia, forming the northern extension of the East-African orogen.
A. Abbo +4 more
semanticscholar +1 more source
The Arabian-Nubian Shield (ANS) is a province of mostly juvenile Neoproterozoic continental crust in NE Africa and Arabia, forming the northern extension of the East-African orogen.
A. Abbo +4 more
semanticscholar +1 more source
2023
Processes driving orogenic styles and long-term isostatic versus dynamic support of the topography have been largely debated in domains of plate convergence. The tectonic evolution of orogens reflect the interactions between mantle flow driving plates and the inherited rheology and composition of moving plates.
Frédéric Mouthereau, Paul Angrand
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Processes driving orogenic styles and long-term isostatic versus dynamic support of the topography have been largely debated in domains of plate convergence. The tectonic evolution of orogens reflect the interactions between mantle flow driving plates and the inherited rheology and composition of moving plates.
Frédéric Mouthereau, Paul Angrand
openaire +1 more source
Geological Journal
The late Cadomian magmatic evolution of the Central East Iranian Microcontinent (CEIM) remains a critical yet debated aspect of northern Gondwana tectonics.
Neda Tavakoli +6 more
semanticscholar +1 more source
The late Cadomian magmatic evolution of the Central East Iranian Microcontinent (CEIM) remains a critical yet debated aspect of northern Gondwana tectonics.
Neda Tavakoli +6 more
semanticscholar +1 more source
, 2021
Palaeomagnetic and isotope (U-Pb, 40Ar-Ar39) studies were conducted in the area of the Brno Massif (Central Europe). The basaltic and granitic dykes, so far regarded as Silurian, were sampled in four localities.
J. Nawrocki, J. Leichmann, M. Pańczyk
semanticscholar +1 more source
Palaeomagnetic and isotope (U-Pb, 40Ar-Ar39) studies were conducted in the area of the Brno Massif (Central Europe). The basaltic and granitic dykes, so far regarded as Silurian, were sampled in four localities.
J. Nawrocki, J. Leichmann, M. Pańczyk
semanticscholar +1 more source
Precambrian Research, 2018
The Avalonian–Cadomian belt formed as a collage of accretionary complexes, island arcs, and sedimentary basins along the northern margin of Gondwana during the Neoproterozoic times.
J. Hajná +4 more
semanticscholar +1 more source
The Avalonian–Cadomian belt formed as a collage of accretionary complexes, island arcs, and sedimentary basins along the northern margin of Gondwana during the Neoproterozoic times.
J. Hajná +4 more
semanticscholar +1 more source
Géosciences
The Sredogriv greenschist facies rocks belong to the Western Balkan Zone in northwestern Bulgaria. The low-grade rocks consist of clastic-tuffaceous precursors and presumably olistostromic magmatic bodies. We present U-Pb LA-ICP-MS zircon age constraints
N. Bonev +7 more
semanticscholar +1 more source
The Sredogriv greenschist facies rocks belong to the Western Balkan Zone in northwestern Bulgaria. The low-grade rocks consist of clastic-tuffaceous precursors and presumably olistostromic magmatic bodies. We present U-Pb LA-ICP-MS zircon age constraints
N. Bonev +7 more
semanticscholar +1 more source
Atlantic Geoscience
A U–Pb LA-ICP-MS zircon study was conducted on 22 rock samples from offshore southeastern Nova Scotia, Canada, to investigate the nature of the pre-Mesozoic basement and the provenance of the overlying syn-rift Late Triassic Eurydice Formation of the ...
Rémi Germain +3 more
semanticscholar +1 more source
A U–Pb LA-ICP-MS zircon study was conducted on 22 rock samples from offshore southeastern Nova Scotia, Canada, to investigate the nature of the pre-Mesozoic basement and the provenance of the overlying syn-rift Late Triassic Eurydice Formation of the ...
Rémi Germain +3 more
semanticscholar +1 more source
BSGF - Earth Sciences Bulletin
By re-examining the historical outcrops of Port-Béni located in the Trégor unit of the North Armorican Cadomian belt, the present work delivers four new ages that provide additional constraints on the Proterozoic history of northern Brittany.
Marc Poujol +3 more
semanticscholar +1 more source
By re-examining the historical outcrops of Port-Béni located in the Trégor unit of the North Armorican Cadomian belt, the present work delivers four new ages that provide additional constraints on the Proterozoic history of northern Brittany.
Marc Poujol +3 more
semanticscholar +1 more source
Schweizerische Mineralogische und Petrographische Mitteilungen: eine europäische Zeitschrift für Mineralogie, Geochemie und Petrographie, 2001
207Pb/206Pb evaporation age dating of euhedral detrital zircons from the Late Ordovician Uggwa Formation, eastern Carnic Alps, yields two age groups, including (1) a group with a pooled age of 650 ± 24 Ma and (2) a bad constrained age group of 518 ± 76 to 533 ± 106 Ma.
Neubauer, Franz M. +2 more
openaire +2 more sources
207Pb/206Pb evaporation age dating of euhedral detrital zircons from the Late Ordovician Uggwa Formation, eastern Carnic Alps, yields two age groups, including (1) a group with a pooled age of 650 ± 24 Ma and (2) a bad constrained age group of 518 ± 76 to 533 ± 106 Ma.
Neubauer, Franz M. +2 more
openaire +2 more sources

