Results 81 to 90 of about 242 (121)
U-Pb dating of volcaniclastic deposits from the Sinj Basin: implications for provenance and the tectono-sedimentary evolution of the External Dinarides. [PDF]
Šamarija R +6 more
europepmc +1 more source
In the western Jabal Akhdar Dome of northeastern Oman and within the Neoproterozoic Huqf Supergroup, well-exposed sedimentary formations span the Cryogenian to Ediacaran periods. These rocks bear the marks of the distant Cadomian Orogeny.
Callegari, Ivan +6 more
core +1 more source
Precambrian Terrane accretion and Ovestepping Successions in thé Iberian Massif (Spain and Portugal)
The Iberian Massif shows the existence of four tectonostratigraphic terranes of Precambrian age which have been accreted in two different orogenic periods and sealed by overstepping successions which have been masked by intense deformation thereafter ...
Martínez García, E.
core
A novel sample pre-screening methodology for accurate in situ U-Pb dating of zircon crystals. [PDF]
Kis A.
europepmc +1 more source
Microstructural surveying of pebbles of the early Cambrian «Anguiano Conglomerates» permits to recognize a variety of microstructures and textures that resulted from syn-metamorphic (up to 400°C, low-temperature greenschists facies) ductile deformations.
Ábalos, Benito
core
Palaeozoic Geography and Palaeomagnetism of the Central European Variscan and Alpine Fold Belts [PDF]
Schätz, Michael
core
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The Brioverian (Upper Proterozoic) and the Cadomian orogeny in the Armorican Massif
Geological Society Special Publication, 1990Abstract The Brioverian in Brittany has generally been divided into the volcanogenic Lower Brioverian and the detrital Upper Brioverian, representing respectively the first and second episodes of the Cadomian orogeny, Cadomian I and Cadomian II.
D Rabu, J Chantraine, J J Chauvel
exaly +2 more sources
The Cadomian orogeny in the North Armorican Massif: a brief review
Geological Society Special Publication, 1990The North Armorican Massif (NAM) of NW France is the type locality of the late Precambrian Cadomian orogenic belt. The NAM largely escaped reworking during the Upper Palaeozoic Variscan cycle, with the result that earlier geological relationships are commonly preserved intact. A large part of the Cadomian belt of the NAM comprises variably deformed and
R S D'Lemos, R A Strachan
exaly +2 more sources

