FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2063837252> ?p ?o ?g. }

• W2063837252 endingPage "734" @default.
• W2063837252 startingPage "719" @default.
• W2063837252 abstract "Several Ordovician volcanic terranes are preserved between the Paleozoic North American margin and the Avalon Terrane in the northern Appalachians of Maine. They have been interpreted as remnants of an island arc on the basis of their current position in the Appalachians or as ocean islands near the margin of Avalon on the basis of paleontologic data. A study of one of these terranes, the Lunksoos terrane in northern Maine, was undertaken through a combination of paleomagnetic and structural analyses in order to understand its tectonic evolution. Paleomagnetic study of the pre‐Caradoeian (pre‐Late Ordovician) Stacyville volcanics revealed three components of magnetization. The final magnetization removed (D=90°, I=36°, α95=11.8°) is interpreted to be primary and yields a paleolatitude of approximately 20°S; however, a Late Ordovician remagnetization cannot be excluded. The Stacyville volcanics now overlie a Cambrian and Lower Ordovician sequence (the Grand Pitch and Shin Brook formations) that is believed to have been deposited at the southern side of Iapetus, possibly near the margin of Avalon. During the Middle and Late Ordovieian, Avalon was at paleolatitude s higher than 40°S, while the volcanics were either formed or remagnetized at a paleolatitude of 20°S. The pre‐Caradocian Stacyville volcanics therefore could not have been deposited directly on the Grand Pitch‐Shin Brook sequence but must have been tectonically emplaced. The Rockabema Diorite which intrudes the entire Cambro‐Ordovician sequence constrains the timing of this emplacement to be pre‐late Early Silurian. These relationships indicate that the Lunksoos area is a composite terrane within the Maine Appalachians. The tectonic emplacement scenario is unnecessary if the Grand Pitch and Shin Brook formations were not located on the south side of Iapetus during the Ordovician. This alternative, however, poses conflicts with the interpretation of faunal affinities." @default.
• W2063837252 created "2016-06-24" @default.
• W2063837252 creator A5001092442 @default.
• W2063837252 creator A5019697617 @default.
• W2063837252 creator A5053042095 @default.
• W2063837252 creator A5082393508 @default.
• W2063837252 date "1990-08-01" @default.
• W2063837252 modified "2023-10-14" @default.
• W2063837252 title "Tectonic history of the Lunksoos Composite Terrane in the Maine Appalachians" @default.
• W2063837252 cites W132292592 @default.
• W2063837252 cites W1820659196 @default.
• W2063837252 cites W1970375021 @default.
• W2063837252 cites W2000377954 @default.
• W2063837252 cites W2004201462 @default.
• W2063837252 cites W2004630600 @default.
• W2063837252 cites W2005884918 @default.
• W2063837252 cites W2009719142 @default.
• W2063837252 cites W2021484134 @default.
• W2063837252 cites W2032011718 @default.
• W2063837252 cites W2039451635 @default.
• W2063837252 cites W2039475211 @default.
• W2063837252 cites W2041522432 @default.
• W2063837252 cites W2046357824 @default.
• W2063837252 cites W2047406994 @default.
• W2063837252 cites W2055770229 @default.
• W2063837252 cites W2061099667 @default.
• W2063837252 cites W2066112052 @default.
• W2063837252 cites W2079243753 @default.
• W2063837252 cites W2083269596 @default.
• W2063837252 cites W2083396660 @default.
• W2063837252 cites W2089222943 @default.
• W2063837252 cites W2090547754 @default.
• W2063837252 cites W2092177060 @default.
• W2063837252 cites W2109949228 @default.
• W2063837252 cites W2112945014 @default.
• W2063837252 cites W2117052568 @default.
• W2063837252 cites W2118204502 @default.
• W2063837252 cites W2137066876 @default.
• W2063837252 cites W2138999972 @default.
• W2063837252 cites W2139555350 @default.
• W2063837252 cites W2172241261 @default.
• W2063837252 cites W2300688371 @default.
• W2063837252 cites W2313420282 @default.
• W2063837252 cites W2316078832 @default.
• W2063837252 cites W2317463277 @default.
• W2063837252 cites W2321515355 @default.
• W2063837252 cites W2323347294 @default.
• W2063837252 cites W2462222741 @default.
• W2063837252 cites W2487302123 @default.
• W2063837252 cites W2911046965 @default.
• W2063837252 doi "https://doi.org/10.1029/tc009i004p00719" @default.
• W2063837252 hasPublicationYear "1990" @default.
• W2063837252 type Work @default.
• W2063837252 sameAs 2063837252 @default.
• W2063837252 citedByCount "20" @default.
• W2063837252 countsByYear W20638372522015 @default.
• W2063837252 countsByYear W20638372522016 @default.
• W2063837252 countsByYear W20638372522017 @default.
• W2063837252 countsByYear W20638372522022 @default.
• W2063837252 crossrefType "journal-article" @default.
• W2063837252 hasAuthorship W2063837252A5001092442 @default.
• W2063837252 hasAuthorship W2063837252A5019697617 @default.
• W2063837252 hasAuthorship W2063837252A5053042095 @default.
• W2063837252 hasAuthorship W2063837252A5082393508 @default.
• W2063837252 hasConcept C120806208 @default.
• W2063837252 hasConcept C127313418 @default.
• W2063837252 hasConcept C13106087 @default.
• W2063837252 hasConcept C150999391 @default.
• W2063837252 hasConcept C151730666 @default.
• W2063837252 hasConcept C189479680 @default.
• W2063837252 hasConcept C192241223 @default.
• W2063837252 hasConcept C77928131 @default.
• W2063837252 hasConcept C91442348 @default.
• W2063837252 hasConceptScore W2063837252C120806208 @default.
• W2063837252 hasConceptScore W2063837252C127313418 @default.
• W2063837252 hasConceptScore W2063837252C13106087 @default.
• W2063837252 hasConceptScore W2063837252C150999391 @default.
• W2063837252 hasConceptScore W2063837252C151730666 @default.
• W2063837252 hasConceptScore W2063837252C189479680 @default.
• W2063837252 hasConceptScore W2063837252C192241223 @default.
• W2063837252 hasConceptScore W2063837252C77928131 @default.
• W2063837252 hasConceptScore W2063837252C91442348 @default.
• W2063837252 hasIssue "4" @default.
• W2063837252 hasLocation W20638372521 @default.
• W2063837252 hasOpenAccess W2063837252 @default.
• W2063837252 hasPrimaryLocation W20638372521 @default.
• W2063837252 hasRelatedWork W1936140173 @default.
• W2063837252 hasRelatedWork W1966541379 @default.
• W2063837252 hasRelatedWork W2030407912 @default.
• W2063837252 hasRelatedWork W2051139768 @default.
• W2063837252 hasRelatedWork W2091125213 @default.
• W2063837252 hasRelatedWork W2139635493 @default.
• W2063837252 hasRelatedWork W2152480689 @default.
• W2063837252 hasRelatedWork W2337712059 @default.
• W2063837252 hasRelatedWork W2911869918 @default.
• W2063837252 hasRelatedWork W3159243423 @default.
• W2063837252 hasVolume "9" @default.
• W2063837252 isParatext "false" @default.

• next