The Cadomian Orogeny and the opening of the Rheic Ocean: The diacrony of geotectonic processes constrained by LA-ICP-MS U–Pb zircon dating (Ossa-Morena and Saxo-Thuringian Zones, Iberian and Bohemian Massifs)

The Cadomian Orogeny and the opening of the Rheic Ocean: The diacrony of geotectonic processes constrained by LA-ICP-MS U–Pb zircon dating (Ossa-Morena and Saxo-Thuringian Zones, Iberian and Bohemian Massifs)

Item
http://www.wikidata.org/entity/Q29040065
Late-Proterozoic to Paleozoic history of the peri-Gondwana Calabria-Peloritani Terrane inferred from a review of zircon chronologyContinental arc volcanism as the principal driver of icehouse-greenhouse variability.How far did the Cadomian ʽterranesʼ travel from Gondwana during early Palaeozoic? A critical reappraisal based on detrital zircon geochronologyGrowth of accretionary wedges and pulsed ophiolitic mélange formation by successive subduction of trench-parallel volcanic elevationsTiming, styles, and kinematics of Cambro–Ordovician extension in the Teplá–Barrandian Unit, Bohemian Massif, and its bearing on the opening of the Rheic OceanDetrital zircon geochronology of the Cretaceous succession from the Iberian Atlantic Margin: palaeogeographic implicationsReply to comment by M. Francisco Pereira et al. on “Geodynamic evolution of the SW Europe Variscides”The provenance of Western Irish Namurian Basin sedimentary strata inferred using detrital zircon U-Pb LA-ICP-MS geochronologyMagmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean—evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)Provenance of upper Triassic sandstone, southwest Iberia (Alentejo and Algarve basins): tracing variability in the sourcesVariability over time in the sources of South Portuguese Zone turbidites: evidence of denudation of different crustal blocks during the assembly of PangaeaLong-lasting Cadomian magmatic activity along an active northern Gondwana margin: U–Pb zircon and Sr–Nd isotopic evidence from the Brunovistulian Domain, eastern Bohemian MassifAge and nature of 560–520 Ma calc-alkaline granitoids of Biarjmand, northeast Iran: insights into Cadomian arc magmatism in northern GondwanaThe multistage crystallization of zircon in calc-alkaline granitoids: U–Pb age constraints on the timing of Variscan tectonic activity in SW IberiaLocation of the Rheic suture in the eastern Bohemian Massif: evidence from detrital zircon dataSubduction, high-P metamorphism, and collision fingerprints in South Iran: Constraints from zircon U-Pb and mica Rb-Sr geochronology
P2860

The Cadomian Orogeny and the opening of the Rheic Ocean: The diacrony of geotectonic processes constrained by LA-ICP-MS U–Pb zircon dating (Ossa-Morena and Saxo-Thuringian Zones, Iberian and Bohemian Massifs)

Item
http://www.wikidata.org/entity/Q29040065
description
2008 nî lūn-bûn
@nan
2008 թուականի Դեկտեմբերին հրատարակուած գիտական յօդուած
@hyw
2008 թվականի դեկտեմբերին հրատարակված գիտական հոդված
@hy
2008年の論文
@ja
2008年論文
@yue
2008年論文
@zh-hant
2008年論文
@zh-hk
2008年論文
@zh-mo
2008年論文
@zh-tw
2008年论文
@wuu
name
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@ast
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@en
type
label
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@ast
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@en
prefLabel
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@ast
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@en
P1433
P1476
P2093
P304
P31
P356
P433
P478
P577
P5875
P356
P1433
P1476
The Cadomian Orogeny and the o ...... Iberian and Bohemian Massifs)
@en
P2093
P304
P31
P356
10.1016/J.TECTO.2008.05.002
P433
P478
P577
P5875