FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4302278169> ?p ?o ?g. }

• W4302278169 endingPage "106851" @default.
• W4302278169 startingPage "106851" @default.
• W4302278169 abstract "The Rottenstone Domain (RD) is a complex lithotectonic supracrustal belt of the Paleoproterozoic Trans-Hudson Orogen in Saskatchewan, Canada, located between the Archean Hearne craton and the juvenile Paleoproterozoic Reindeer Zone (RZ). Its evolution and crustal affinity have been under considerable debate in the past few decades, with most interpretations considering it to be part of RZ, but some hinting that certain elements might have affinities to the Archean hinterland. On the basis of bedrock mapping, U-Pb, Sm-Nd and lithogeochemical data, the rocks of the southwestern RD were subdivided into several lithodemic entities, which were used to reconstruct a plate tectonic framework for the western part of the Trans-Hudson Orogen during Orosirian time. A U-Pb zircon crystallization age of 2518 ± 6 Ma and depleted mantle model age (TDM) of 2.8 Ga for an augen granite confirmed that the western part of RD is part of the Hearne craton. A newly discovered structural inlier at the eastern boundary of RD consists of a central unit of 2045 ± 9 Ma augen granite, with TDM ages between 2.8 and 2.6 Ga, that was intruded into gneissic granite with a TDM of 3.3 Ga. The augen granite was interpreted as representing a rift-related granite, emplaced into Archean rocks of the Hearne craton. Two lithotectonic assemblages, one dominated by feldspathic quartzite and psammite the other by migmatitic psammite-psammopelite, are in structural contact with the granitic inliers and have model ages of 2.6–2.4 Ga. One of the feldspathic quartzite samples contains detrital zircon age modes at 1910 and 1860 Ma, and lesser Archean modes. Both assemblages were likely deposited in a forearc basin to the 1.865–1.850 Ga Wathaman continental arc. Recognition of Archean components and metasedimentary assemblages with older model ages than those in the RZ to the east, suggest that this southern part of RD is more closely affiliated with the Hearne craton. The eastern edge of RD coincides with a mylonite zone (Howard Lake shear zone), which likely represents a fundamental, although multiply reactivated, structural break separating Archean granitoids and structurally overlying metasedimentary rocks from rocks of the more juvenile Reindeer Zone." @default.
• W4302278169 created "2022-10-06" @default.
• W4302278169 creator A5009297314 @default.
• W4302278169 creator A5019558955 @default.
• W4302278169 creator A5028906953 @default.
• W4302278169 creator A5083732449 @default.
• W4302278169 date "2022-10-01" @default.
• W4302278169 modified "2023-10-16" @default.
• W4302278169 title "Constraints on the evolution of the eastern margin of the Hearne craton: New data from the southwestern Rottenstone Domain, Trans-Hudson Orogen, Saskatchewan" @default.
• W4302278169 cites W1963502697 @default.
• W4302278169 cites W1964747585 @default.
• W4302278169 cites W1971044831 @default.
• W4302278169 cites W1974933984 @default.
• W4302278169 cites W1976008625 @default.
• W4302278169 cites W1976081525 @default.
• W4302278169 cites W1978699470 @default.
• W4302278169 cites W1988572292 @default.
• W4302278169 cites W1989189038 @default.
• W4302278169 cites W1991494408 @default.
• W4302278169 cites W1992565879 @default.
• W4302278169 cites W1992996299 @default.
• W4302278169 cites W1996949238 @default.
• W4302278169 cites W2000448287 @default.
• W4302278169 cites W2004061693 @default.
• W4302278169 cites W2004638555 @default.
• W4302278169 cites W2006705360 @default.
• W4302278169 cites W2007581769 @default.
• W4302278169 cites W2011342565 @default.
• W4302278169 cites W2016848487 @default.
• W4302278169 cites W2020696829 @default.
• W4302278169 cites W2021908084 @default.
• W4302278169 cites W2044350598 @default.
• W4302278169 cites W2053911093 @default.
• W4302278169 cites W2057406163 @default.
• W4302278169 cites W2058505271 @default.
• W4302278169 cites W2065851830 @default.
• W4302278169 cites W2070142384 @default.
• W4302278169 cites W2080588058 @default.
• W4302278169 cites W2084481447 @default.
• W4302278169 cites W2086465833 @default.
• W4302278169 cites W2087958038 @default.
• W4302278169 cites W2088440167 @default.
• W4302278169 cites W2108971421 @default.
• W4302278169 cites W2112096417 @default.
• W4302278169 cites W2117834512 @default.
• W4302278169 cites W2119438235 @default.
• W4302278169 cites W2125771345 @default.
• W4302278169 cites W2138351677 @default.
• W4302278169 cites W2144663013 @default.
• W4302278169 cites W2145604970 @default.
• W4302278169 cites W2146462471 @default.
• W4302278169 cites W2152588796 @default.
• W4302278169 cites W2161188118 @default.
• W4302278169 cites W2169982338 @default.
• W4302278169 cites W2476550529 @default.
• W4302278169 cites W2587853641 @default.
• W4302278169 cites W2783100684 @default.
• W4302278169 cites W2909223431 @default.
• W4302278169 cites W2909675537 @default.
• W4302278169 cites W2910819475 @default.
• W4302278169 cites W2911214421 @default.
• W4302278169 cites W2995224727 @default.
• W4302278169 cites W3162926388 @default.
• W4302278169 cites W4200301553 @default.
• W4302278169 cites W4236848473 @default.
• W4302278169 cites W4250239246 @default.
• W4302278169 doi "https://doi.org/10.1016/j.precamres.2022.106851" @default.
• W4302278169 hasPublicationYear "2022" @default.
• W4302278169 type Work @default.
• W4302278169 citedByCount "1" @default.
• W4302278169 countsByYear W43022781692023 @default.
• W4302278169 crossrefType "journal-article" @default.
• W4302278169 hasAuthorship W4302278169A5009297314 @default.
• W4302278169 hasAuthorship W4302278169A5019558955 @default.
• W4302278169 hasAuthorship W4302278169A5028906953 @default.
• W4302278169 hasAuthorship W4302278169A5083732449 @default.
• W4302278169 hasConcept C127313418 @default.
• W4302278169 hasConcept C147717901 @default.
• W4302278169 hasConcept C149347711 @default.
• W4302278169 hasConcept C150999391 @default.
• W4302278169 hasConcept C151730666 @default.
• W4302278169 hasConcept C17409809 @default.
• W4302278169 hasConcept C2778849375 @default.
• W4302278169 hasConcept C34122518 @default.
• W4302278169 hasConcept C77928131 @default.
• W4302278169 hasConceptScore W4302278169C127313418 @default.
• W4302278169 hasConceptScore W4302278169C147717901 @default.
• W4302278169 hasConceptScore W4302278169C149347711 @default.
• W4302278169 hasConceptScore W4302278169C150999391 @default.
• W4302278169 hasConceptScore W4302278169C151730666 @default.
• W4302278169 hasConceptScore W4302278169C17409809 @default.
• W4302278169 hasConceptScore W4302278169C2778849375 @default.
• W4302278169 hasConceptScore W4302278169C34122518 @default.
• W4302278169 hasConceptScore W4302278169C77928131 @default.
• W4302278169 hasLocation W43022781691 @default.
• W4302278169 hasOpenAccess W4302278169 @default.
• W4302278169 hasPrimaryLocation W43022781691 @default.
• W4302278169 hasRelatedWork W2017300140 @default.

• next