{"id":"W2054522734","doi":"10.1016/j.tecto.2008.05.002","title":"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)","year":2008,"lang":"en","type":"article","venue":"Tectonophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":459,"is_retracted":false,"has_abstract":false,"ca_institutions":"","funders":"University of Victoria","keywords":"Geology; Gondwana; Massif; Zircon; Paleontology; Subduction; Orogeny; Oceanic crust; Continental crust; Back-arc basin; Supercontinent; Geochemistry; Island arc; Craton; Crust; Structural basin; Tectonics","routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false,"invisible_to_affiliation_only":true},"retraction":null,"screen":null,"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.00508674395978957,"score_gpt":0.1621845245993647,"score_spread":0.1570977806395752,"validation_status":"score_only:v0-immature-baseline","note":"Baseline scores from an immature model (maturity gate not passed). Scores rank; they never assert a category."}}