Results 51 to 60 of about 242 (121)
This study focuses on bimodal meta-volcanic rocks present in the Iberian Massif, in the ´Evora-Aracena Metamorphic Belt of the Ossa-Morena Zone (OMZ), near the boundary with the South Portuguese Zone. New petrological, geochemical (whole-rock and Sr–Nd isotopes) and LA-ICP-MS U–Pb zircon geochronology data are presented to track the magmatic evolution ...
Cachapuz, P. +13 more
openaire +4 more sources
The present work describes two early Cambrian folding events within Cryogenian to earliest Cambrian rocks of the western Jabal Akhdar Dome (Central Oman Mountains).
Ivan Callegari
core +1 more source
Detrital zircon U-Pb ages and source of the late Palaeocene Thanet Formation, Kent, SE England
The sources of the Paleocene London Basin marine to fluviodeltaic sandstones are currently unclear. High analysis number detrital zircon U-Pb age investigation of an early-mid Thanetian marine sand from East Kent, reveals a large spread of zircon age ...
Baykal, Yunus +3 more
core +1 more source
Abstract Zircon U‐Pb‐He double dating (ZDD) provides the opportunity to derive high temperature crystallization ages and low temperature cooling ages from the very same mineral grain, making it especially attractive for zircon provenance studies. We present the combination of in situ detrital zircon U‐Pb‐He double dating and Raman spectroscopy‐based ...
I. Dunkl +4 more
wiley +1 more source
In the Sandikli (Afyon) region, western Taurides, the Late Proterozoic rocks of the Sandikli basement complex are composed of low-grade meta-sedimentary rocks (Guvercinoluk Formation) intruded by felsic rocks (Kestel Cayi Porphyroid Suite, KCPS).
Guersu, Semih, Goencueoglu, M. Cemal
core +1 more source
The Merida Massif,a cadomian volcanic arc reactivates into Hercynic Orogeny
The Merida igneous outcrops are situated in the Obejo-Valsequillo-Puebla de la Reina Domain (DOVPR) of the northern Ossa-Morena Zone (Iberian Massif). This massif is composed by plutonic and volcanic rocks.
Bandrés, A. +3 more
core
International audienceThe Armorican Massif experienced a poly-orogenic evolution, represented by the Neoproterozoic Cadomian and the Devonian-Carboniferous Variscan tectonothermal events.
Li, Xian-Hua +3 more
core +1 more source
Large-scale geological structures of the Egyptian Nubian Shield. [PDF]
Hamimi Z +3 more
europepmc +1 more source
Non-coaxial deformation of foreland basement involved in a fold-and-thrust belt: a strain partitioning approach to the Eastern Variscan orogen. [PDF]
Mareček L +5 more
europepmc +1 more source
Phanerozoic flooding of North America and the Great Unconformity. [PDF]
Tasistro-Hart AR, Macdonald FA.
europepmc +1 more source

