FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2081541737> ?p ?o ?g. }

• W2081541737 endingPage "1220" @default.
• W2081541737 startingPage "1211" @default.
• W2081541737 abstract "Studies of the coastal sedimentary record have allowed both the reconstruction of relative sea-level changes and the determination of local rates and magnitudes of tectonic deformation, particularly in tectonically active areas. Despite their successful use elsewhere, studies of this type are much less common for the Mexican Pacific coast, which parallels the Cocos-North America subduction plate boundary. Stratigraphic, geochemical and microfossil data from sediments in Laguna Mitla, the Pacific coast of Guerrero, Mexico, document late-Holocene sea-level changes induced by tectonic activity in the Mexican subduction zone. Three major events are identified. First, the formation of the lagoon by c. 4630 yr BP, as indicated by a freshwater to brackish peat. Second, a relative sea-level rise, or land subsidence, as indicated by a shift from a freshwater marginal lagoon environment to a marine setting, preceded by a marine inundation represented by a sand unit (possibly a tsunami deposit), by c. 3400 yr BP. And finally, a return to lagoonal conditions indicating a drop in relative sea level or coastal uplift by c. 2300 yr BP. The Laguna Mitla stratigraphy indicates general coastal subsidence or relative sea level rise of c. 1 mm/yr. We argue that these relative sea-level (land-level) changes have been induced by tectonic activity associated with the Mexican megathrust. A plausible explanation for the 3400 yr BP marine inundation is probably a tsunami produced by a large seismic event accompanied by coastal subsidence. Discrete fining upward, fine to coarse, sand units with an erosional basal contact, medium to poor sorting, and clay/mud rip-up clasts; an increase in Na and Sr elemental concentrations, indicative of a marine origin; and the landward extent of the sands support a tsunamigenic source for these deposits. However, these apparent tsunami deposits require further study to determine their lateral extent and to assess whether they can be correlated from one site to another. This study demonstrates the applicability of a multiproxy sedimentary approach in interpreting relative sea-level (land-level) changes and to derive data on related earthquake and tsunami events in tropical coastal lagoons." @default.
• W2081541737 created "2016-06-24" @default.
• W2081541737 creator A5018077943 @default.
• W2081541737 creator A5024092397 @default.
• W2081541737 creator A5033464481 @default.
• W2081541737 creator A5058720077 @default.
• W2081541737 creator A5078128691 @default.
• W2081541737 creator A5087923399 @default.
• W2081541737 date "2007-12-01" @default.
• W2081541737 modified "2023-10-17" @default.
• W2081541737 title "Sedimentary record of late-Holocene relative sea-level change and tectonic deformation from the Guerrero Seismic Gap, Mexican Pacific Coast" @default.
• W2081541737 cites W1515675093 @default.
• W2081541737 cites W1528448801 @default.
• W2081541737 cites W1574636466 @default.
• W2081541737 cites W1977866652 @default.
• W2081541737 cites W1990473022 @default.
• W2081541737 cites W1993837889 @default.
• W2081541737 cites W1996727194 @default.
• W2081541737 cites W2002572096 @default.
• W2081541737 cites W2004401359 @default.
• W2081541737 cites W2006677963 @default.
• W2081541737 cites W2010078767 @default.
• W2081541737 cites W2013752021 @default.
• W2081541737 cites W2020792364 @default.
• W2081541737 cites W2029003391 @default.
• W2081541737 cites W2029219438 @default.
• W2081541737 cites W2029818683 @default.
• W2081541737 cites W2039802692 @default.
• W2081541737 cites W2053870388 @default.
• W2081541737 cites W2065159548 @default.
• W2081541737 cites W2071448765 @default.
• W2081541737 cites W2073745380 @default.
• W2081541737 cites W2074088098 @default.
• W2081541737 cites W2077823623 @default.
• W2081541737 cites W2087242768 @default.
• W2081541737 cites W2095725119 @default.
• W2081541737 cites W2098333110 @default.
• W2081541737 cites W2101538035 @default.
• W2081541737 cites W2104598833 @default.
• W2081541737 cites W2107098077 @default.
• W2081541737 cites W2109602197 @default.
• W2081541737 cites W2130833734 @default.
• W2081541737 cites W2154276443 @default.
• W2081541737 cites W2157609091 @default.
• W2081541737 cites W2158743207 @default.
• W2081541737 cites W2163311663 @default.
• W2081541737 cites W2280624662 @default.
• W2081541737 cites W4254196321 @default.
• W2081541737 cites W2330521211 @default.
• W2081541737 doi "https://doi.org/10.1177/0959683607085127" @default.
• W2081541737 hasPublicationYear "2007" @default.
• W2081541737 type Work @default.
• W2081541737 sameAs 2081541737 @default.
• W2081541737 citedByCount "43" @default.
• W2081541737 countsByYear W20815417372012 @default.
• W2081541737 countsByYear W20815417372013 @default.
• W2081541737 countsByYear W20815417372014 @default.
• W2081541737 countsByYear W20815417372015 @default.
• W2081541737 countsByYear W20815417372016 @default.
• W2081541737 countsByYear W20815417372017 @default.
• W2081541737 countsByYear W20815417372018 @default.
• W2081541737 countsByYear W20815417372019 @default.
• W2081541737 countsByYear W20815417372020 @default.
• W2081541737 countsByYear W20815417372021 @default.
• W2081541737 countsByYear W20815417372022 @default.
• W2081541737 countsByYear W20815417372023 @default.
• W2081541737 crossrefType "journal-article" @default.
• W2081541737 hasAuthorship W2081541737A5018077943 @default.
• W2081541737 hasAuthorship W2081541737A5024092397 @default.
• W2081541737 hasAuthorship W2081541737A5033464481 @default.
• W2081541737 hasAuthorship W2081541737A5058720077 @default.
• W2081541737 hasAuthorship W2081541737A5078128691 @default.
• W2081541737 hasAuthorship W2081541737A5087923399 @default.
• W2081541737 hasConcept C100951216 @default.
• W2081541737 hasConcept C109007969 @default.
• W2081541737 hasConcept C111368507 @default.
• W2081541737 hasConcept C127313418 @default.
• W2081541737 hasConcept C139419234 @default.
• W2081541737 hasConcept C140345934 @default.
• W2081541737 hasConcept C151730666 @default.
• W2081541737 hasConcept C180851071 @default.
• W2081541737 hasConcept C200646496 @default.
• W2081541737 hasConcept C58097730 @default.
• W2081541737 hasConcept C6494504 @default.
• W2081541737 hasConcept C74501621 @default.
• W2081541737 hasConcept C77928131 @default.
• W2081541737 hasConceptScore W2081541737C100951216 @default.
• W2081541737 hasConceptScore W2081541737C109007969 @default.
• W2081541737 hasConceptScore W2081541737C111368507 @default.
• W2081541737 hasConceptScore W2081541737C127313418 @default.
• W2081541737 hasConceptScore W2081541737C139419234 @default.
• W2081541737 hasConceptScore W2081541737C140345934 @default.
• W2081541737 hasConceptScore W2081541737C151730666 @default.
• W2081541737 hasConceptScore W2081541737C180851071 @default.
• W2081541737 hasConceptScore W2081541737C200646496 @default.
• W2081541737 hasConceptScore W2081541737C58097730 @default.
• W2081541737 hasConceptScore W2081541737C6494504 @default.
• W2081541737 hasConceptScore W2081541737C74501621 @default.

• next