FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2746308832> ?p ?o ?g. }

• W2746308832 endingPage "16" @default.
• W2746308832 startingPage "1" @default.
• W2746308832 abstract "Along the Sanriku coast, northeast Japan, discrepancies in crustal movement have been reported between uplift on a scale of 105 years versus subsidence on a scale of 101–102 years. Well-dated Holocene incised-valley-fill sediments provide records of millennial-scale vertical crustal movement, which is key to understanding the tectonic history in this area. Previous studies of the age and distribution of early Holocene intertidal deposits in incised valleys reported that the southern Sanriku coast has subsided during the Holocene at an average rate of about 1 mm/yr. Here we studied three sediment cores, TGI1, TGI2, and TGI3, collected from the Tsugaruishi plain on the central Sanriku coast, and recognized a Holocene deltaic sediment succession in all three cores. In core TGI3, from the farthest inland site, the intertidal sediment facies, deposited from 7500 to 7000 cal BP, and the overlying 6-m-thick floodplain facies, deposited from 7000 to 5000 cal BP, are both below the present sea level. Because a sea-level highstand due to hydroisostatic uplift around Japan occurred in the mid-Holocene, we inferred that the Tsugaruishi plain subsided during the Holocene, and the estimated subsidence rate, 1.1–1.9 mm/yr at maximum, is consistent with the recently reported subsidence rate along the southern Sanriku coast. The results of this study confirm that the central to southern Sanriku coast is subsiding, in contrast to an interpretation based on the study of marine terraces that this part of the coast is uplifting. The empirical data presented here will be useful for constructing an earthquake cycle model related to plate subduction." @default.
• W2746308832 created "2017-08-31" @default.
• W2746308832 creator A5039830492 @default.
• W2746308832 creator A5050523349 @default.
• W2746308832 creator A5057714769 @default.
• W2746308832 creator A5070486264 @default.
• W2746308832 date "2017-10-01" @default.
• W2746308832 modified "2023-10-15" @default.
• W2746308832 title "Subsidence along the central to southern Sanriku coast, northeast Japan, near the source region of the 2011 Tohoku-oki earthquake, estimated from the Holocene sedimentary succession along a ria coast" @default.
• W2746308832 cites W1807213132 @default.
• W2746308832 cites W1970979684 @default.
• W2746308832 cites W1976764610 @default.
• W2746308832 cites W1985059677 @default.
• W2746308832 cites W1994201485 @default.
• W2746308832 cites W1999797075 @default.
• W2746308832 cites W2007782885 @default.
• W2746308832 cites W2010297790 @default.
• W2746308832 cites W2014542246 @default.
• W2746308832 cites W2017611649 @default.
• W2746308832 cites W2021545108 @default.
• W2746308832 cites W2030685722 @default.
• W2746308832 cites W2031574943 @default.
• W2746308832 cites W2036007503 @default.
• W2746308832 cites W2052242710 @default.
• W2746308832 cites W2074992781 @default.
• W2746308832 cites W2075373452 @default.
• W2746308832 cites W2079749210 @default.
• W2746308832 cites W2097570511 @default.
• W2746308832 cites W2133305844 @default.
• W2746308832 cites W2133377555 @default.
• W2746308832 cites W2138481206 @default.
• W2746308832 cites W2140795339 @default.
• W2746308832 cites W2144792248 @default.
• W2746308832 cites W2145147906 @default.
• W2746308832 cites W2147044945 @default.
• W2746308832 cites W2160266092 @default.
• W2746308832 cites W2164522782 @default.
• W2746308832 cites W2167452694 @default.
• W2746308832 cites W2168168247 @default.
• W2746308832 cites W2170365501 @default.
• W2746308832 cites W2171306615 @default.
• W2746308832 cites W2183613433 @default.
• W2746308832 cites W2324460958 @default.
• W2746308832 cites W2327123359 @default.
• W2746308832 cites W2468191998 @default.
• W2746308832 cites W2570301540 @default.
• W2746308832 cites W2579366489 @default.
• W2746308832 cites W2588665305 @default.
• W2746308832 cites W400119023 @default.
• W2746308832 cites W4249751050 @default.
• W2746308832 cites W2335011063 @default.
• W2746308832 doi "https://doi.org/10.1016/j.quaint.2017.08.008" @default.
• W2746308832 hasPublicationYear "2017" @default.
• W2746308832 type Work @default.
• W2746308832 sameAs 2746308832 @default.
• W2746308832 citedByCount "13" @default.
• W2746308832 countsByYear W27463088322018 @default.
• W2746308832 countsByYear W27463088322019 @default.
• W2746308832 countsByYear W27463088322020 @default.
• W2746308832 countsByYear W27463088322021 @default.
• W2746308832 countsByYear W27463088322022 @default.
• W2746308832 countsByYear W27463088322023 @default.
• W2746308832 crossrefType "journal-article" @default.
• W2746308832 hasAuthorship W2746308832A5039830492 @default.
• W2746308832 hasAuthorship W2746308832A5050523349 @default.
• W2746308832 hasAuthorship W2746308832A5057714769 @default.
• W2746308832 hasAuthorship W2746308832A5070486264 @default.
• W2746308832 hasConcept C109007969 @default.
• W2746308832 hasConcept C111368507 @default.
• W2746308832 hasConcept C127313418 @default.
• W2746308832 hasConcept C140345934 @default.
• W2746308832 hasConcept C146588470 @default.
• W2746308832 hasConcept C151730666 @default.
• W2746308832 hasConcept C174580923 @default.
• W2746308832 hasConcept C180851071 @default.
• W2746308832 hasConcept C6494504 @default.
• W2746308832 hasConcept C74501621 @default.
• W2746308832 hasConceptScore W2746308832C109007969 @default.
• W2746308832 hasConceptScore W2746308832C111368507 @default.
• W2746308832 hasConceptScore W2746308832C127313418 @default.
• W2746308832 hasConceptScore W2746308832C140345934 @default.
• W2746308832 hasConceptScore W2746308832C146588470 @default.
• W2746308832 hasConceptScore W2746308832C151730666 @default.
• W2746308832 hasConceptScore W2746308832C174580923 @default.
• W2746308832 hasConceptScore W2746308832C180851071 @default.
• W2746308832 hasConceptScore W2746308832C6494504 @default.
• W2746308832 hasConceptScore W2746308832C74501621 @default.
• W2746308832 hasFunder F4320320912 @default.
• W2746308832 hasFunder F4320323584 @default.
• W2746308832 hasLocation W27463088321 @default.
• W2746308832 hasOpenAccess W2746308832 @default.
• W2746308832 hasPrimaryLocation W27463088321 @default.
• W2746308832 hasRelatedWork W127697715 @default.
• W2746308832 hasRelatedWork W2000745753 @default.
• W2746308832 hasRelatedWork W2078426495 @default.
• W2746308832 hasRelatedWork W2082235444 @default.
• W2746308832 hasRelatedWork W2165521607 @default.
• W2746308832 hasRelatedWork W2362747183 @default.

• next