FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016746988> ?p ?o ?g. }

• W2016746988 endingPage "14" @default.
• W2016746988 startingPage "1" @default.
• W2016746988 abstract "The discovery of serpentinite-bearing conglomerate including detrital blue amphibole grains in Cretaceous forearc basin sediments in the northern part of Japan supports large tectonic movement in the forearc basin during the Early Cretaceous. Conglomerate and sandstone are intercalated in the Lower Cretaceous offshore mudstone sequence and contain serpentinite clasts, chromian spinels, blue amphiboles, and oolitic grains with chromian spinel nuclei. The conglomerate and sandstones were deposited as a debris flow consisting of an admixture of siliciclastic terrigenous sediments and calcareous biogenic material with serpentinite-derived sediments. The sandstones consist of feldspathic–lithic arenites and wackes, and their composition suggests that most of the terrigenous material was derived from the Cretaceous volcanic terrane and the Jurassic accretionary complex located to the west of the depositional basin. However, the serpentinite body correlated with the provenance of the sediments is not distributed in these terranes. Because the oolitic grains in the matrix of the conglomerate include only angular chromian spinels and serpentine clasts without quartz and feldspar grains, most of the serpentinite-derived sediments are considered to have been supplied primarily from a serpentinite body exposed along the shallow marine environments near the sedimentary basin. Therefore, the serpentine-derived sediments and feldspathic and lithic materials have essentially different sources. Thus, we may infer that the examined sediments are due to large slope failure affecting a relatively wide area of shallow coast involving the place where the serpentine body was emplaced and the place where river-fed terrigenous siliciclastic sediments accumulated. The stratigraphic range of the serpentinite-derived sediments, which are sporadically distributed in the Cretaceous forearc basin of northern Japan, suggests that the serpentinite-derived material was actively supplied to the forearc basin in Albian times. Recent tectono-stratigraphy of the Late Mesozoic accretionary complex in Japan reveals a strike–slip movement in the subduction zone around northeastern Asia. Large earthquakes affected by active strike–slip motion of the oceanic plate are inferred to be the trigger of tectonic movement, such as large slope failure following serpentine intrusion in the forearc region. Another possibility is that subduction of a large number of seamount on the oceanic plate might also cause a large change in basin morphology, bringing about large slope failure." @default.
• W2016746988 created "2016-06-24" @default.
• W2016746988 creator A5011965085 @default.
• W2016746988 creator A5050371820 @default.
• W2016746988 creator A5055291015 @default.
• W2016746988 creator A5057761089 @default.
• W2016746988 creator A5076329210 @default.
• W2016746988 creator A5077343835 @default.
• W2016746988 date "2010-12-01" @default.
• W2016746988 modified "2023-09-24" @default.
• W2016746988 title "Deposition of serpentine-bearing conglomerate and its implications for Early Cretaceous tectonics in northern Japan" @default.
• W2016746988 cites W1481297934 @default.
• W2016746988 cites W1967694846 @default.
• W2016746988 cites W1977493051 @default.
• W2016746988 cites W1980072019 @default.
• W2016746988 cites W1983950806 @default.
• W2016746988 cites W1991771183 @default.
• W2016746988 cites W1992603582 @default.
• W2016746988 cites W1994935654 @default.
• W2016746988 cites W1997578008 @default.
• W2016746988 cites W2000253152 @default.
• W2016746988 cites W2003636517 @default.
• W2016746988 cites W2009944200 @default.
• W2016746988 cites W2011838931 @default.
• W2016746988 cites W2016273083 @default.
• W2016746988 cites W2026391469 @default.
• W2016746988 cites W2029531882 @default.
• W2016746988 cites W2031295342 @default.
• W2016746988 cites W2036393594 @default.
• W2016746988 cites W2038630418 @default.
• W2016746988 cites W2039267678 @default.
• W2016746988 cites W2042994231 @default.
• W2016746988 cites W2043593891 @default.
• W2016746988 cites W2050836721 @default.
• W2016746988 cites W2064999564 @default.
• W2016746988 cites W2066637465 @default.
• W2016746988 cites W2067231302 @default.
• W2016746988 cites W2070345742 @default.
• W2016746988 cites W2071947096 @default.
• W2016746988 cites W2082710068 @default.
• W2016746988 cites W2083609953 @default.
• W2016746988 cites W2090799987 @default.
• W2016746988 cites W2093021831 @default.
• W2016746988 cites W2095024065 @default.
• W2016746988 cites W2097417267 @default.
• W2016746988 cites W2098679585 @default.
• W2016746988 cites W2106161981 @default.
• W2016746988 cites W2111968655 @default.
• W2016746988 cites W2118259484 @default.
• W2016746988 cites W2122668781 @default.
• W2016746988 cites W2127691210 @default.
• W2016746988 cites W2128883863 @default.
• W2016746988 cites W2132342875 @default.
• W2016746988 cites W2133703571 @default.
• W2016746988 cites W2138368467 @default.
• W2016746988 cites W2150826815 @default.
• W2016746988 cites W2156744603 @default.
• W2016746988 cites W2159141265 @default.
• W2016746988 cites W2164390400 @default.
• W2016746988 cites W2168457689 @default.
• W2016746988 cites W221666880 @default.
• W2016746988 cites W2314025506 @default.
• W2016746988 cites W2320258584 @default.
• W2016746988 cites W2322964912 @default.
• W2016746988 cites W2323501590 @default.
• W2016746988 cites W2324279894 @default.
• W2016746988 cites W2328601970 @default.
• W2016746988 cites W2341338809 @default.
• W2016746988 doi "https://doi.org/10.1016/j.sedgeo.2010.09.002" @default.
• W2016746988 hasPublicationYear "2010" @default.
• W2016746988 type Work @default.
• W2016746988 sameAs 2016746988 @default.
• W2016746988 citedByCount "4" @default.
• W2016746988 countsByYear W20167469882014 @default.
• W2016746988 countsByYear W20167469882016 @default.
• W2016746988 countsByYear W20167469882020 @default.
• W2016746988 crossrefType "journal-article" @default.
• W2016746988 hasAuthorship W2016746988A5011965085 @default.
• W2016746988 hasAuthorship W2016746988A5050371820 @default.
• W2016746988 hasAuthorship W2016746988A5055291015 @default.
• W2016746988 hasAuthorship W2016746988A5057761089 @default.
• W2016746988 hasAuthorship W2016746988A5076329210 @default.
• W2016746988 hasAuthorship W2016746988A5077343835 @default.
• W2016746988 hasConcept C106804226 @default.
• W2016746988 hasConcept C109007969 @default.
• W2016746988 hasConcept C12015391 @default.
• W2016746988 hasConcept C120806208 @default.
• W2016746988 hasConcept C12294951 @default.
• W2016746988 hasConcept C126753816 @default.
• W2016746988 hasConcept C127313418 @default.
• W2016746988 hasConcept C138170599 @default.
• W2016746988 hasConcept C150999391 @default.
• W2016746988 hasConcept C151730666 @default.
• W2016746988 hasConcept C17409809 @default.
• W2016746988 hasConcept C192241223 @default.
• W2016746988 hasConcept C199285206 @default.
• W2016746988 hasConcept C2780049196 @default.
• W2016746988 hasConcept C41440632 @default.

• next