Matches in SemOpenAlex for { <https://semopenalex.org/work/W2087360401> ?p ?o ?g. }
- W2087360401 endingPage "1207" @default.
- W2087360401 startingPage "1186" @default.
- W2087360401 abstract "Foraminiferal and diatom assemblages in 11 cores (3–7.5 m deep) of Holocene sediment from brackish marine Ahuriri Inlet in southern Hawke's Bay, New Zealand, provide a record of 8.5 m of subsidence followed by 1.5 m of uplift in the last 7200 cal years, in a region overlying the subduction zone between the Australian and Pacific Plates. Modern Analogue Technique was used to estimate paleotidal elevation of the 97 richest foraminiferal assemblages. The most precise estimates are for high-tidal salt marsh assemblages cored in marginal settings in the north and south of the former inlet. The least precise estimates are from low-tidal and subtidal assemblages from cores in the middle of the inlet. These paleoelevation estimates combined with sediment thicknesses, age determinations (from tephrostratigraphy and radiocarbon dates), the New Zealand Holocene sea level curve, and estimates of compaction, identify the Holocene land elevation changes and earthquake-displacement events in each core. The following major, earthquake-related displacements are inferred: ca 7000 cal yr BP (>−0.6 m displacement); ca 5800 cal yr BP (>−0.5 m; ca 4200 cal yr BP (ca −1.5 m); ca 3000 cal yr BP (−1.4 to −1.8 m); ca 1600 cal yr BP (ca −1.7 m); ca 600 cal yr BP (ca −1 m); 1931AD Napier Earthquake (+1.5 m). Further smaller events involving regional subsidence or earthquake-shake compaction are indicated during the 7000–3000 yr BP interval, but cannot be identified precisely. The six (possibly subduction interface) subsidence events in the last 7000 years have had a return time of 1000–1400 years. Identified displacement events have a range of sedimentary expressions, from an eroded and burrowed hiatus surface, to an abrupt lithologic switch from mud to sand, or peat to shelly mud, or in some places no change in sediment character whatsoever." @default.
- W2087360401 created "2016-06-24" @default.
- W2087360401 creator A5003425296 @default.
- W2087360401 creator A5003891757 @default.
- W2087360401 creator A5008978671 @default.
- W2087360401 creator A5012369143 @default.
- W2087360401 creator A5037983021 @default.
- W2087360401 creator A5082265594 @default.
- W2087360401 creator A5089110935 @default.
- W2087360401 creator A5090260994 @default.
- W2087360401 date "2006-06-01" @default.
- W2087360401 modified "2023-10-13" @default.
- W2087360401 title "Micropaleontological evidence of large earthquakes in the past 7200 years in southern Hawke's Bay, New Zealand" @default.
- W2087360401 cites W1507372749 @default.
- W2087360401 cites W1517018339 @default.
- W2087360401 cites W1567810246 @default.
- W2087360401 cites W1604687641 @default.
- W2087360401 cites W1971217395 @default.
- W2087360401 cites W1971395039 @default.
- W2087360401 cites W1974322665 @default.
- W2087360401 cites W1974708490 @default.
- W2087360401 cites W1976616660 @default.
- W2087360401 cites W1979270150 @default.
- W2087360401 cites W1995435055 @default.
- W2087360401 cites W2000081741 @default.
- W2087360401 cites W2002494458 @default.
- W2087360401 cites W2005139953 @default.
- W2087360401 cites W2005818714 @default.
- W2087360401 cites W2006338549 @default.
- W2087360401 cites W2017530838 @default.
- W2087360401 cites W2019491275 @default.
- W2087360401 cites W2020305042 @default.
- W2087360401 cites W2026415010 @default.
- W2087360401 cites W2029219438 @default.
- W2087360401 cites W2033490733 @default.
- W2087360401 cites W2037981373 @default.
- W2087360401 cites W2040614796 @default.
- W2087360401 cites W2043735744 @default.
- W2087360401 cites W2046179515 @default.
- W2087360401 cites W2047364685 @default.
- W2087360401 cites W2049175326 @default.
- W2087360401 cites W2053870388 @default.
- W2087360401 cites W2062486320 @default.
- W2087360401 cites W2071985072 @default.
- W2087360401 cites W2072266422 @default.
- W2087360401 cites W2073660985 @default.
- W2087360401 cites W2075419906 @default.
- W2087360401 cites W2076918935 @default.
- W2087360401 cites W2077556666 @default.
- W2087360401 cites W2078670946 @default.
- W2087360401 cites W2079493775 @default.
- W2087360401 cites W2081741199 @default.
- W2087360401 cites W2096103597 @default.
- W2087360401 cites W2106741180 @default.
- W2087360401 cites W2107098077 @default.
- W2087360401 cites W2107178771 @default.
- W2087360401 cites W2110689430 @default.
- W2087360401 cites W2117133909 @default.
- W2087360401 cites W2125192462 @default.
- W2087360401 cites W2143307800 @default.
- W2087360401 cites W2145138604 @default.
- W2087360401 cites W2147716188 @default.
- W2087360401 cites W2153747804 @default.
- W2087360401 cites W2155175103 @default.
- W2087360401 cites W2314022116 @default.
- W2087360401 cites W2334599547 @default.
- W2087360401 cites W2488622718 @default.
- W2087360401 cites W413189428 @default.
- W2087360401 cites W598760174 @default.
- W2087360401 cites W2476857619 @default.
- W2087360401 doi "https://doi.org/10.1016/j.quascirev.2005.10.013" @default.
- W2087360401 hasPublicationYear "2006" @default.
- W2087360401 type Work @default.
- W2087360401 sameAs 2087360401 @default.
- W2087360401 citedByCount "50" @default.
- W2087360401 countsByYear W20873604012012 @default.
- W2087360401 countsByYear W20873604012013 @default.
- W2087360401 countsByYear W20873604012014 @default.
- W2087360401 countsByYear W20873604012015 @default.
- W2087360401 countsByYear W20873604012016 @default.
- W2087360401 countsByYear W20873604012017 @default.
- W2087360401 countsByYear W20873604012018 @default.
- W2087360401 countsByYear W20873604012019 @default.
- W2087360401 countsByYear W20873604012021 @default.
- W2087360401 countsByYear W20873604012022 @default.
- W2087360401 crossrefType "journal-article" @default.
- W2087360401 hasAuthorship W2087360401A5003425296 @default.
- W2087360401 hasAuthorship W2087360401A5003891757 @default.
- W2087360401 hasAuthorship W2087360401A5008978671 @default.
- W2087360401 hasAuthorship W2087360401A5012369143 @default.
- W2087360401 hasAuthorship W2087360401A5037983021 @default.
- W2087360401 hasAuthorship W2087360401A5082265594 @default.
- W2087360401 hasAuthorship W2087360401A5089110935 @default.
- W2087360401 hasAuthorship W2087360401A5090260994 @default.
- W2087360401 hasConcept C100134115 @default.
- W2087360401 hasConcept C109007969 @default.
- W2087360401 hasConcept C111368507 @default.
- W2087360401 hasConcept C115880899 @default.