FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2884622882> ?p ?o ?g. }

• W2884622882 endingPage "3132" @default.
• W2884622882 startingPage "3114" @default.
• W2884622882 abstract "Abstract Emergent coral reef terraces in northwest Luzon Island, Philippines are studied to understand relative sea level (RSL) changes and uplift along the Manila Trench forearc region during the Late Quaternary. Coral reef sequences in Currimao, Badoc, and Badoc Island were mapped and were described based on geomorphological characteristics, elevation patterns, and ages. The lower emergent coral reef terraces, which are dated Holocene, are subdivided into three to possibly four terrace steps (TI–TIV in ascending order) with the highest terrace (TIII–TIV) rising up to ~7–9 m amsl. The well‐preserved staircase morphology and meter‐scale terrace risers possibly imply episodes of abrupt RSL changes that resulted from coseismic uplift during the mid‐Holocene. Around 6.8 kyr BP, ~3 m of rapid uplift (possibly coseismic) is inferred to account for the vertical separation of TI (6.2 kyr BP at 3.5 m amsl) and TII (6.8 kyr BP at 6.6 m amsl) in Currimao site. A subsequent episode of RSL fall occurred at 6 kyr BP, based on dated coral samples, and has emerged the lowest terraces in the study sites. New geomorphic and radiometric data suggest that the mid‐Holocene sea level highstand in northwest Luzon occurred at around 7–6 kyr BP. From the elevation and thorium‐230 age of dated terrace surfaces, we estimated Holocene uplift rates from 0.17 ± 0.12 to 0.82 ± 0.15 mm/yr across the three study sites. The estimated uplift rates of northwest Luzon are relatively lower than the uplift rates reported in similar tectonically active regions of the west Pacific such as Papua New Guinea, Taiwan, New Zealand, and Japan. The geomorphological characteristics and age of emergent coral reef terraces reported in this study offer insights on the preservation of long‐term deformation along the northwest Luzon coastal plain that is bordered by a subduction zone and upper‐plate faults. © 2018 John Wiley & Sons, Ltd." @default.
• W2884622882 created "2018-08-03" @default.
• W2884622882 creator A5008721510 @default.
• W2884622882 creator A5020724406 @default.
• W2884622882 creator A5022741502 @default.
• W2884622882 creator A5024729648 @default.
• W2884622882 creator A5029262436 @default.
• W2884622882 creator A5029414958 @default.
• W2884622882 date "2018-09-03" @default.
• W2884622882 modified "2023-10-17" @default.
• W2884622882 title "Late Quaternary uplift across northwest Luzon Island, Philippines constrained from emergent coral reef terraces" @default.
• W2884622882 cites W1540946605 @default.
• W2884622882 cites W1603555063 @default.
• W2884622882 cites W1761966220 @default.
• W2884622882 cites W179100328 @default.
• W2884622882 cites W1885327561 @default.
• W2884622882 cites W1965730925 @default.
• W2884622882 cites W1965858395 @default.
• W2884622882 cites W1966648776 @default.
• W2884622882 cites W1973899769 @default.
• W2884622882 cites W1981384673 @default.
• W2884622882 cites W1981419414 @default.
• W2884622882 cites W1987349355 @default.
• W2884622882 cites W1991465327 @default.
• W2884622882 cites W1993971903 @default.
• W2884622882 cites W1994155113 @default.
• W2884622882 cites W1995126499 @default.
• W2884622882 cites W1995967605 @default.
• W2884622882 cites W1996447421 @default.
• W2884622882 cites W1999941080 @default.
• W2884622882 cites W2004501456 @default.
• W2884622882 cites W2005944223 @default.
• W2884622882 cites W2010546608 @default.
• W2884622882 cites W2012397942 @default.
• W2884622882 cites W2012637865 @default.
• W2884622882 cites W2014995805 @default.
• W2884622882 cites W2015573300 @default.
• W2884622882 cites W2015965132 @default.
• W2884622882 cites W2016177052 @default.
• W2884622882 cites W2017629014 @default.
• W2884622882 cites W2018045480 @default.
• W2884622882 cites W2018190159 @default.
• W2884622882 cites W2022281308 @default.
• W2884622882 cites W2026976482 @default.
• W2884622882 cites W2030559447 @default.
• W2884622882 cites W2032173908 @default.
• W2884622882 cites W2033917509 @default.
• W2884622882 cites W2036336541 @default.
• W2884622882 cites W2036360871 @default.
• W2884622882 cites W2037407658 @default.
• W2884622882 cites W2045706691 @default.
• W2884622882 cites W2045801082 @default.
• W2884622882 cites W2047364685 @default.
• W2884622882 cites W2049175326 @default.
• W2884622882 cites W2051039802 @default.
• W2884622882 cites W2055866586 @default.
• W2884622882 cites W2064619083 @default.
• W2884622882 cites W2067264739 @default.
• W2884622882 cites W2069982509 @default.
• W2884622882 cites W2073526104 @default.
• W2884622882 cites W2074895286 @default.
• W2884622882 cites W2076111088 @default.
• W2884622882 cites W2081845564 @default.
• W2884622882 cites W2086436054 @default.
• W2884622882 cites W2088262025 @default.
• W2884622882 cites W2089885421 @default.
• W2884622882 cites W2093057413 @default.
• W2884622882 cites W2094033454 @default.
• W2884622882 cites W2094394939 @default.
• W2884622882 cites W2094988303 @default.
• W2884622882 cites W2097071434 @default.
• W2884622882 cites W2104425893 @default.
• W2884622882 cites W2110381646 @default.
• W2884622882 cites W2112285521 @default.
• W2884622882 cites W2132520319 @default.
• W2884622882 cites W2149153051 @default.
• W2884622882 cites W2154537721 @default.
• W2884622882 cites W2157681159 @default.
• W2884622882 cites W2161721809 @default.
• W2884622882 cites W2166559860 @default.
• W2884622882 cites W2197006047 @default.
• W2884622882 cites W2443976745 @default.
• W2884622882 cites W2586718984 @default.
• W2884622882 cites W2609209070 @default.
• W2884622882 cites W2612375735 @default.
• W2884622882 cites W2791699993 @default.
• W2884622882 cites W4205293238 @default.
• W2884622882 cites W4210968111 @default.
• W2884622882 doi "https://doi.org/10.1002/esp.4474" @default.
• W2884622882 hasPublicationYear "2018" @default.
• W2884622882 type Work @default.
• W2884622882 sameAs 2884622882 @default.
• W2884622882 citedByCount "4" @default.
• W2884622882 countsByYear W28846228822021 @default.
• W2884622882 countsByYear W28846228822022 @default.
• W2884622882 crossrefType "journal-article" @default.
• W2884622882 hasAuthorship W2884622882A5008721510 @default.
• W2884622882 hasAuthorship W2884622882A5020724406 @default.

• next