FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2007616056> ?p ?o ?g. }

• W2007616056 endingPage "1227" @default.
• W2007616056 startingPage "1210" @default.
• W2007616056 abstract "Thermal, alternating field (AF), and two-stage (AF followed by thermal) experiments performed on one Silurian (Mascarene Group) and two Devonian (St. George and St. Stephen plutons) rock units indicate that considerable polar movement relative to New Brunswick took place in Siluro-Devonian times. The Mascarene Group yields a pole at 122°E, 02°S, the St. Stephen pluton, a pole at 136°E, 43°S, and the St. George pluton, two poles at 085°E, 38°S and 093°E, 29°N respectively. Although the southern poles lie some 70° south of most North American Silurian and Devonian poles, they are in agreement with poles obtained from two recent studies of Newfoundland rock units. It is unknown if this apparent polar displacement is representative of the entire North American craton or of its eastern margin only. A graphic representation of all available North American data is disconcerting and shows that little is known about the behaviour of the Lower Paleozoic field relative to North America and that many more data are needed to reconstruct the paleomagnetic record.The St. George pluton carries two dual polarity remanences which often are not easily discernible, especially since one of the remanences has an intensity much weaker than the other. The usefulness of vector diagrams for the analysis of multicomponent remanences is demonstrated. Examples are shown where the dual polarity of the weaker remanence, which might otherwise escape notice, can be readily detected on enlarged scale vector diagrams." @default.
• W2007616056 created "2016-06-24" @default.
• W2007616056 creator A5002530767 @default.
• W2007616056 creator A5023332671 @default.
• W2007616056 creator A5041394777 @default.
• W2007616056 date "1979-06-01" @default.
• W2007616056 modified "2023-10-18" @default.
• W2007616056 title "Paleomagnetic results from three rock units of New Brunswick and their bearing on the Lower Paleozoic tectonics of North America" @default.
• W2007616056 cites W1964536273 @default.
• W2007616056 cites W1970537131 @default.
• W2007616056 cites W1979876066 @default.
• W2007616056 cites W1983325321 @default.
• W2007616056 cites W1996047396 @default.
• W2007616056 cites W2014757385 @default.
• W2007616056 cites W2021925885 @default.
• W2007616056 cites W2022591175 @default.
• W2007616056 cites W2031986008 @default.
• W2007616056 cites W2034029151 @default.
• W2007616056 cites W2038180652 @default.
• W2007616056 cites W2046794147 @default.
• W2007616056 cites W2047406994 @default.
• W2007616056 cites W2051997415 @default.
• W2007616056 cites W2057540139 @default.
• W2007616056 cites W2061850905 @default.
• W2007616056 cites W2083269596 @default.
• W2007616056 cites W2085435956 @default.
• W2007616056 cites W2086955228 @default.
• W2007616056 cites W2088564865 @default.
• W2007616056 cites W2091859674 @default.
• W2007616056 cites W2095798748 @default.
• W2007616056 cites W2111964401 @default.
• W2007616056 cites W2126642978 @default.
• W2007616056 cites W2144412412 @default.
• W2007616056 cites W2148388312 @default.
• W2007616056 cites W2160226174 @default.
• W2007616056 cites W2167474223 @default.
• W2007616056 cites W2168474072 @default.
• W2007616056 cites W2170160785 @default.
• W2007616056 cites W2267387765 @default.
• W2007616056 doi "https://doi.org/10.1139/e79-107" @default.
• W2007616056 hasPublicationYear "1979" @default.
• W2007616056 type Work @default.
• W2007616056 sameAs 2007616056 @default.
• W2007616056 citedByCount "27" @default.
• W2007616056 countsByYear W20076160562013 @default.
• W2007616056 crossrefType "journal-article" @default.
• W2007616056 hasAuthorship W2007616056A5002530767 @default.
• W2007616056 hasAuthorship W2007616056A5023332671 @default.
• W2007616056 hasAuthorship W2007616056A5041394777 @default.
• W2007616056 hasConcept C107832698 @default.
• W2007616056 hasConcept C109007969 @default.
• W2007616056 hasConcept C127313418 @default.
• W2007616056 hasConcept C13106087 @default.
• W2007616056 hasConcept C147717901 @default.
• W2007616056 hasConcept C149918038 @default.
• W2007616056 hasConcept C151730666 @default.
• W2007616056 hasConcept C181727316 @default.
• W2007616056 hasConcept C189479680 @default.
• W2007616056 hasConcept C2781121502 @default.
• W2007616056 hasConcept C34122518 @default.
• W2007616056 hasConcept C77928131 @default.
• W2007616056 hasConcept C91442348 @default.
• W2007616056 hasConceptScore W2007616056C107832698 @default.
• W2007616056 hasConceptScore W2007616056C109007969 @default.
• W2007616056 hasConceptScore W2007616056C127313418 @default.
• W2007616056 hasConceptScore W2007616056C13106087 @default.
• W2007616056 hasConceptScore W2007616056C147717901 @default.
• W2007616056 hasConceptScore W2007616056C149918038 @default.
• W2007616056 hasConceptScore W2007616056C151730666 @default.
• W2007616056 hasConceptScore W2007616056C181727316 @default.
• W2007616056 hasConceptScore W2007616056C189479680 @default.
• W2007616056 hasConceptScore W2007616056C2781121502 @default.
• W2007616056 hasConceptScore W2007616056C34122518 @default.
• W2007616056 hasConceptScore W2007616056C77928131 @default.
• W2007616056 hasConceptScore W2007616056C91442348 @default.
• W2007616056 hasIssue "6" @default.
• W2007616056 hasLocation W20076160561 @default.
• W2007616056 hasOpenAccess W2007616056 @default.
• W2007616056 hasPrimaryLocation W20076160561 @default.
• W2007616056 hasRelatedWork W1993867113 @default.
• W2007616056 hasRelatedWork W2019208667 @default.
• W2007616056 hasRelatedWork W2033665198 @default.
• W2007616056 hasRelatedWork W2049565557 @default.
• W2007616056 hasRelatedWork W2051139768 @default.
• W2007616056 hasRelatedWork W2056514599 @default.
• W2007616056 hasRelatedWork W2074517757 @default.
• W2007616056 hasRelatedWork W2092299172 @default.
• W2007616056 hasRelatedWork W2377459518 @default.
• W2007616056 hasRelatedWork W261909130 @default.
• W2007616056 hasVolume "16" @default.
• W2007616056 isParatext "false" @default.
• W2007616056 isRetracted "false" @default.
• W2007616056 magId "2007616056" @default.
• W2007616056 workType "article" @default.