FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022141535> ?p ?o ?g. }

• W2022141535 endingPage "42" @default.
• W2022141535 startingPage "33" @default.
• W2022141535 abstract "The thermal and exhumation history of late Hercynian granitoids from Calabria (Sila and Serre massifs) has been studied using thermobarometry and radiometric age determinations. The uplift and erosion which followed contractional tectonics of Tertiary age exposed in Calabria a nearly complete section of the Hercynian crust. Field data, constrained by igneous thermobarometrical data, have enabled us to draw simplified crustal profiles. In both the Sila and Serre massifs, granitoids make up the intermediate portions of the crustal sections and are stacked as tabular intrusions for up to 13 km cumulative thickness. Shallow granitoids are characterized by a weak fabric, mostly developed in the magmatic stage, whereas deep-seated granitoids display a strong fabric developed in the magmatic state and, with decreasing temperatures, in the subsolidus state. The intrusive bodies were emplaced at 300–290 Ma, at a time when the Calabrian crust was undergoing extensional tectonics and crustal thinning. The subsequent post-Hercynian evolution is recorded by Rb-Sr dates of micas and fission track ages of zircon and apatite obtained from granitoids emplaced at different depths. A decrease in Rb-Sr and fission track ages is observed as depth of emplacement increases. Data on the post-Hercynian geological evolution of Calabria were used to model in three stages the cooling and exhumation history of deep-seated and shallow granitoids. The first stage, in Permian to Triassic times, was characterized by slow erosion. It was followed by a second stage of extensional tectonics in Jurassic times. The third stage was exhumation during the Apenninic Orogeny. The model has generated two P–T–t arrays, one for deep-seated and the other for shallow granitoids of the Serre massif. The T–t paths suggest that the dates of micas, zircon and apatite are cooling ages. They also show that deep-seated granitoids remained at temperatures above the brittle–plastic transition for a long time, whereas shallow granitoids cooled rapidly. Distinct P–T–t paths explain why deep-seated and shallow granitoids display different fabric and microstructural features. Copyright © 2000 John Wiley & Sons, Ltd." @default.
• W2022141535 created "2016-06-24" @default.
• W2022141535 creator A5004966836 @default.
• W2022141535 creator A5008724323 @default.
• W2022141535 creator A5075085715 @default.
• W2022141535 date "2000-01-01" @default.
• W2022141535 modified "2023-10-09" @default.
• W2022141535 title "Cooling and exhumation history of deep-seated and shallow level, late Hercynian granitoids from Calabria" @default.
• W2022141535 cites W1975212574 @default.
• W2022141535 cites W1986667802 @default.
• W2022141535 cites W2001120389 @default.
• W2022141535 cites W2024243891 @default.
• W2022141535 cites W2040549377 @default.
• W2022141535 cites W2051168002 @default.
• W2022141535 cites W2053381713 @default.
• W2022141535 cites W2073440210 @default.
• W2022141535 cites W2075751020 @default.
• W2022141535 cites W2087946500 @default.
• W2022141535 cites W2105662998 @default.
• W2022141535 cites W2116902285 @default.
• W2022141535 cites W2132593853 @default.
• W2022141535 cites W2150896271 @default.
• W2022141535 cites W2178505927 @default.
• W2022141535 cites W2323045186 @default.
• W2022141535 cites W2335919622 @default.
• W2022141535 cites W2735472696 @default.
• W2022141535 doi "https://doi.org/10.1002/(sici)1099-1034(200001/03)35:1<33::aid-gj836>3.0.co;2-u" @default.
• W2022141535 hasPublicationYear "2000" @default.
• W2022141535 type Work @default.
• W2022141535 sameAs 2022141535 @default.
• W2022141535 citedByCount "23" @default.
• W2022141535 countsByYear W20221415352012 @default.
• W2022141535 countsByYear W20221415352014 @default.
• W2022141535 countsByYear W20221415352015 @default.
• W2022141535 countsByYear W20221415352018 @default.
• W2022141535 countsByYear W20221415352019 @default.
• W2022141535 countsByYear W20221415352020 @default.
• W2022141535 countsByYear W20221415352021 @default.
• W2022141535 crossrefType "journal-article" @default.
• W2022141535 hasAuthorship W2022141535A5004966836 @default.
• W2022141535 hasAuthorship W2022141535A5008724323 @default.
• W2022141535 hasAuthorship W2022141535A5075085715 @default.
• W2022141535 hasConcept C127313418 @default.
• W2022141535 hasConcept C136137745 @default.
• W2022141535 hasConcept C146357865 @default.
• W2022141535 hasConcept C151730666 @default.
• W2022141535 hasConcept C160776313 @default.
• W2022141535 hasConcept C17409809 @default.
• W2022141535 hasConcept C195963834 @default.
• W2022141535 hasConcept C203457885 @default.
• W2022141535 hasConcept C2776698055 @default.
• W2022141535 hasConcept C2777241186 @default.
• W2022141535 hasConcept C2778849375 @default.
• W2022141535 hasConcept C42787717 @default.
• W2022141535 hasConcept C77928131 @default.
• W2022141535 hasConcept C92217149 @default.
• W2022141535 hasConceptScore W2022141535C127313418 @default.
• W2022141535 hasConceptScore W2022141535C136137745 @default.
• W2022141535 hasConceptScore W2022141535C146357865 @default.
• W2022141535 hasConceptScore W2022141535C151730666 @default.
• W2022141535 hasConceptScore W2022141535C160776313 @default.
• W2022141535 hasConceptScore W2022141535C17409809 @default.
• W2022141535 hasConceptScore W2022141535C195963834 @default.
• W2022141535 hasConceptScore W2022141535C203457885 @default.
• W2022141535 hasConceptScore W2022141535C2776698055 @default.
• W2022141535 hasConceptScore W2022141535C2777241186 @default.
• W2022141535 hasConceptScore W2022141535C2778849375 @default.
• W2022141535 hasConceptScore W2022141535C42787717 @default.
• W2022141535 hasConceptScore W2022141535C77928131 @default.
• W2022141535 hasConceptScore W2022141535C92217149 @default.
• W2022141535 hasIssue "1" @default.
• W2022141535 hasLocation W20221415351 @default.
• W2022141535 hasOpenAccess W2022141535 @default.
• W2022141535 hasPrimaryLocation W20221415351 @default.
• W2022141535 hasRelatedWork W1778167562 @default.
• W2022141535 hasRelatedWork W1987634561 @default.
• W2022141535 hasRelatedWork W2022141535 @default.
• W2022141535 hasRelatedWork W2033953445 @default.
• W2022141535 hasRelatedWork W2043608081 @default.
• W2022141535 hasRelatedWork W2361053869 @default.
• W2022141535 hasRelatedWork W2369420054 @default.
• W2022141535 hasRelatedWork W2905635526 @default.
• W2022141535 hasRelatedWork W2980623078 @default.
• W2022141535 hasRelatedWork W4247328597 @default.
• W2022141535 hasVolume "35" @default.
• W2022141535 isParatext "false" @default.
• W2022141535 isRetracted "false" @default.
• W2022141535 magId "2022141535" @default.
• W2022141535 workType "article" @default.