FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2060555513> ?p ?o ?g. }

• W2060555513 endingPage "164" @default.
• W2060555513 startingPage "145" @default.
• W2060555513 abstract "New U–Pb zircon and monazite ages for syn- and post-kinematic pegmatites that cut major shear zones within the western Quebec portion of the Grenville Province constrain the timing of deformation and final terrane assembly within this region. From the Grenville Front SE along the present section, the Grenville Province consists of a reworked Archean promontory partly covered by Proterozoic allochthons and two Proterozoic metasedimentary and metaigneous terranes, which are probably allochthonous. The age of the Grenville Front is still poorly constrained in this area as pegmatites intersecting high-grade rocks exhumed some 30 km south of the Front have upper intercept U–Pb ages of 2642+6/−5 Ma. Field and geochronological data in this paper, however, lend support to the possibility of late-Archean exhumation of high-grade terranes along the Front. South of the Front, two types of ductile shear zone are responsible for the geometry of terranes in this part of the Grenville Province. The first type corresponds to the boundary of allochthons transported onto the Archean parautochthon. The corresponding structures are not directly dated, but reheating of the parautochthon at about 1020 Ma (U–Pb ages on monazite) sets a minimum age for thrusting in this area. Late movement along an east-dipping shear zone located within the parautochthon, the Cabonga thrust (CT; 998+9/−5 Ma), is rather unique in that it involves rocks of the parautochthon and is characterized by a westerly directed transport. The shear zones of the second type are subvertical, NE-trending, generally sinistral and intersect the parautochthon, the allochthon or both. From the Front towards the SE, these shear zones are: the Cadgecrib shear zone (998+16/−6 Ma) intersecting the parautochthon, the Renzy shear zone (1003+4/−5 Ma) involving allochthonous metasediments, the Baskatong shear zone (1020+2/−1 Ma) which marks the NW limit of Proterozoic rocks of the Mont-Laurier terrane, the Labelle shear zone (1078±6 Ma) separating the Mont-Laurier and the Morin terrane, and the Taureau shear zone (1074±4 Ma) bounding the Morin terrane to the east. All the above timing constraints are from U–Pb ages on syn- to post-kinematic pegmatites emplaced within the respective shear zones. This age distribution suggests a propagation of transcurrent deformation towards the NW, which is responsible for the final configuration of terranes." @default.
• W2060555513 created "2016-06-24" @default.
• W2060555513 creator A5002959414 @default.
• W2060555513 creator A5054142255 @default.
• W2060555513 date "1998-10-01" @default.
• W2060555513 modified "2023-10-01" @default.
• W2060555513 title "Geochronological constraints on the last stages of terrane assembly in the central part of the Grenville Province" @default.
• W2060555513 cites W1583745181 @default.
• W2060555513 cites W1965596825 @default.
• W2060555513 cites W1970038673 @default.
• W2060555513 cites W1974203049 @default.
• W2060555513 cites W1976648441 @default.
• W2060555513 cites W1982056930 @default.
• W2060555513 cites W1983684752 @default.
• W2060555513 cites W1993563335 @default.
• W2060555513 cites W2005408708 @default.
• W2060555513 cites W2007105153 @default.
• W2060555513 cites W2013007066 @default.
• W2060555513 cites W2015562381 @default.
• W2060555513 cites W2026387367 @default.
• W2060555513 cites W2026969831 @default.
• W2060555513 cites W2029362637 @default.
• W2060555513 cites W2043335427 @default.
• W2060555513 cites W2050467182 @default.
• W2060555513 cites W2052241580 @default.
• W2060555513 cites W2054155041 @default.
• W2060555513 cites W2058147354 @default.
• W2060555513 cites W2071578732 @default.
• W2060555513 cites W2073720208 @default.
• W2060555513 cites W2079493558 @default.
• W2060555513 cites W2080994074 @default.
• W2060555513 cites W2087013591 @default.
• W2060555513 cites W2088091813 @default.
• W2060555513 cites W2092742668 @default.
• W2060555513 cites W2112605217 @default.
• W2060555513 cites W2162811155 @default.
• W2060555513 cites W2195162144 @default.
• W2060555513 cites W2317655919 @default.
• W2060555513 cites W2748546549 @default.
• W2060555513 cites W2908726219 @default.
• W2060555513 cites W2910370187 @default.
• W2060555513 cites W2911206162 @default.
• W2060555513 cites W4233448357 @default.
• W2060555513 cites W4234983532 @default.
• W2060555513 doi "https://doi.org/10.1016/s0301-9268(98)00072-2" @default.
• W2060555513 hasPublicationYear "1998" @default.
• W2060555513 type Work @default.
• W2060555513 sameAs 2060555513 @default.
• W2060555513 citedByCount "35" @default.
• W2060555513 countsByYear W20605555132012 @default.
• W2060555513 countsByYear W20605555132013 @default.
• W2060555513 countsByYear W20605555132014 @default.
• W2060555513 countsByYear W20605555132015 @default.
• W2060555513 countsByYear W20605555132017 @default.
• W2060555513 countsByYear W20605555132023 @default.
• W2060555513 crossrefType "journal-article" @default.
• W2060555513 hasAuthorship W2060555513A5002959414 @default.
• W2060555513 hasAuthorship W2060555513A5054142255 @default.
• W2060555513 hasConcept C111368507 @default.
• W2060555513 hasConcept C127313418 @default.
• W2060555513 hasConcept C149347711 @default.
• W2060555513 hasConcept C150999391 @default.
• W2060555513 hasConcept C151730666 @default.
• W2060555513 hasConcept C165205528 @default.
• W2060555513 hasConcept C17409809 @default.
• W2060555513 hasConcept C23295444 @default.
• W2060555513 hasConcept C2776212575 @default.
• W2060555513 hasConcept C2777551076 @default.
• W2060555513 hasConcept C2778849375 @default.
• W2060555513 hasConcept C50047906 @default.
• W2060555513 hasConcept C77928131 @default.
• W2060555513 hasConcept C93033518 @default.
• W2060555513 hasConceptScore W2060555513C111368507 @default.
• W2060555513 hasConceptScore W2060555513C127313418 @default.
• W2060555513 hasConceptScore W2060555513C149347711 @default.
• W2060555513 hasConceptScore W2060555513C150999391 @default.
• W2060555513 hasConceptScore W2060555513C151730666 @default.
• W2060555513 hasConceptScore W2060555513C165205528 @default.
• W2060555513 hasConceptScore W2060555513C17409809 @default.
• W2060555513 hasConceptScore W2060555513C23295444 @default.
• W2060555513 hasConceptScore W2060555513C2776212575 @default.
• W2060555513 hasConceptScore W2060555513C2777551076 @default.
• W2060555513 hasConceptScore W2060555513C2778849375 @default.
• W2060555513 hasConceptScore W2060555513C50047906 @default.
• W2060555513 hasConceptScore W2060555513C77928131 @default.
• W2060555513 hasConceptScore W2060555513C93033518 @default.
• W2060555513 hasIssue "2" @default.
• W2060555513 hasLocation W20605555131 @default.
• W2060555513 hasOpenAccess W2060555513 @default.
• W2060555513 hasPrimaryLocation W20605555131 @default.
• W2060555513 hasRelatedWork W1501477135 @default.
• W2060555513 hasRelatedWork W2012247338 @default.
• W2060555513 hasRelatedWork W2060555513 @default.
• W2060555513 hasRelatedWork W2068238646 @default.
• W2060555513 hasRelatedWork W2074749531 @default.
• W2060555513 hasRelatedWork W2075063530 @default.
• W2060555513 hasRelatedWork W2081513947 @default.
• W2060555513 hasRelatedWork W2151271029 @default.

• next