Marine deposits of late glacial times exposed by tectonic uplift on the east coast of Taiwan
Identifieur interne : 000500 ( France/Analysis ); précédent : 000499; suivant : 000501Marine deposits of late glacial times exposed by tectonic uplift on the east coast of Taiwan
Auteurs : P. A Pirazzoli [France] ; M. Arnold [France] ; P. Giresse [France] ; M. L Hsieh [République populaire de Chine] ; P. M Liew [République populaire de Chine]Source :
- Marine Geology [ 0025-3227 ] ; 1993.
Descripteurs français
- Wicri :
- geographic : Taïwan.
English descriptors
- KwdEn :
- Anodontia edentula, Average uplift rate, Barbados corals, Coastal area, Coastal range, Diodora suprapunicea, East coast, Eastern taiwan, Eustatic rise, Highest rates, Holocene changes, Marine deposits, Marine samples, Marine sediments, Mass spectrometry, Paleomagnetic studies, Paphia undulata, Past years, Pebble beach, Pirazzoli, Place aristide briand, River mouth deposits, Such rates, Taiwan, Tectonic, Tectonic uplift, Tectonic uplift rates, Time scale, Uplift, Uplift rate, Uplift rates.
- Teeft :
- Anodontia edentula, Average uplift rate, Barbados corals, Coastal area, Coastal range, Diodora suprapunicea, East coast, Eastern taiwan, Eustatic rise, Highest rates, Holocene changes, Marine deposits, Marine samples, Marine sediments, Mass spectrometry, Paleomagnetic studies, Paphia undulata, Past years, Pebble beach, Pirazzoli, Place aristide briand, River mouth deposits, Such rates, Taiwan, Tectonic, Tectonic uplift, Tectonic uplift rates, Time scale, Uplift, Uplift rate, Uplift rates.
Abstract
Abstract: Marine sediments deposited some 14,000 years ago, when the sea level was between 80 and 100 m below the present sea level, have been found exposed at about 17 m in altitude near Tu-lan, on the east coast of Taiwan. This implies a minimum average uplift rate of 7.6 ± 0.9 mm/yr; similar values of tectonic uplift are not uncommon on the eastern Coastal Range of Taiwan. Such rates of tectonic uplift, among the highest reported in the literature, are of the same order as present-day maximum glacio-isostatic uplift rates.
Url:
DOI: 10.1016/0025-3227(93)90101-Z
Affiliations:
- France, République populaire de Chine
- Languedoc-Roussillon, Occitanie (région administrative), Île-de-France
- Meudon-Bellevue, Perpignan
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ISTEX:B63B1C55FDB13AA8E6BE96A15595E76DBFB406D3Le document en format XML
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Giresse</name><affiliation wicri:level="3"><country xml:lang="fr">France</country><wicri:regionArea>Laboratoire de Recherches de Sédimentologie Marine, Université de Perpignan, 66025 Perpignan</wicri:regionArea><placeName><region type="region" nuts="2">Occitanie (région administrative)</region><region type="old region" nuts="2">Languedoc-Roussillon</region><settlement type="city">Perpignan</settlement></placeName></affiliation></author><author><name sortKey="Hsieh, M L" sort="Hsieh, M L" uniqKey="Hsieh M" first="M. L" last="Hsieh">M. L Hsieh</name><affiliation wicri:level="1"><country xml:lang="fr" wicri:curation="lc">République populaire de Chine</country><wicri:regionArea>Department of Geology, National Taiwan University, 245 Choushan Road, Taipei, Taiwan</wicri:regionArea><wicri:noRegion>Taiwan</wicri:noRegion></affiliation></author><author><name sortKey="Liew, P M" sort="Liew, P M" uniqKey="Liew P" first="P. M" last="Liew">P. M Liew</name><affiliation wicri:level="1"><country xml:lang="fr" wicri:curation="lc">République populaire de Chine</country><wicri:regionArea>Department of Geology, National Taiwan University, 245 Choushan Road, Taipei, Taiwan</wicri:regionArea><wicri:noRegion>Taiwan</wicri:noRegion></affiliation></author></analytic><monogr></monogr><series><title level="j">Marine Geology</title><title level="j" type="abbrev">MARGO</title><idno type="ISSN">0025-3227</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1993">1993</date><biblScope unit="volume">110</biblScope><biblScope unit="issue">1–2</biblScope><biblScope unit="page" from="1">1</biblScope><biblScope unit="page" to="6">6</biblScope></imprint><idno type="ISSN">0025-3227</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0025-3227</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Anodontia edentula</term><term>Average uplift rate</term><term>Barbados corals</term><term>Coastal area</term><term>Coastal range</term><term>Diodora suprapunicea</term><term>East coast</term><term>Eastern taiwan</term><term>Eustatic rise</term><term>Highest rates</term><term>Holocene changes</term><term>Marine deposits</term><term>Marine samples</term><term>Marine sediments</term><term>Mass spectrometry</term><term>Paleomagnetic studies</term><term>Paphia undulata</term><term>Past years</term><term>Pebble beach</term><term>Pirazzoli</term><term>Place aristide briand</term><term>River mouth deposits</term><term>Such rates</term><term>Taiwan</term><term>Tectonic</term><term>Tectonic uplift</term><term>Tectonic uplift rates</term><term>Time scale</term><term>Uplift</term><term>Uplift rate</term><term>Uplift rates</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Anodontia edentula</term><term>Average uplift rate</term><term>Barbados corals</term><term>Coastal area</term><term>Coastal range</term><term>Diodora suprapunicea</term><term>East coast</term><term>Eastern taiwan</term><term>Eustatic rise</term><term>Highest rates</term><term>Holocene changes</term><term>Marine deposits</term><term>Marine samples</term><term>Marine sediments</term><term>Mass spectrometry</term><term>Paleomagnetic studies</term><term>Paphia undulata</term><term>Past years</term><term>Pebble beach</term><term>Pirazzoli</term><term>Place aristide briand</term><term>River mouth deposits</term><term>Such rates</term><term>Taiwan</term><term>Tectonic</term><term>Tectonic uplift</term><term>Tectonic uplift rates</term><term>Time scale</term><term>Uplift</term><term>Uplift rate</term><term>Uplift rates</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Taïwan</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Marine sediments deposited some 14,000 years ago, when the sea level was between 80 and 100 m below the present sea level, have been found exposed at about 17 m in altitude near Tu-lan, on the east coast of Taiwan. This implies a minimum average uplift rate of 7.6 ± 0.9 mm/yr; similar values of tectonic uplift are not uncommon on the eastern Coastal Range of Taiwan. Such rates of tectonic uplift, among the highest reported in the literature, are of the same order as present-day maximum glacio-isostatic uplift rates.</div></front></TEI><affiliations><list><country><li>France</li><li>République populaire de Chine</li></country><region><li>Languedoc-Roussillon</li><li>Occitanie (région administrative)</li><li>Île-de-France</li></region><settlement><li>Meudon-Bellevue</li><li>Perpignan</li></settlement></list><tree><country name="France"><region name="Île-de-France"><name sortKey="Pirazzoli, P A" sort="Pirazzoli, P A" uniqKey="Pirazzoli P" first="P. A" last="Pirazzoli">P. A Pirazzoli</name></region><name sortKey="Arnold, M" sort="Arnold, M" uniqKey="Arnold M" first="M" last="Arnold">M. Arnold</name><name sortKey="Giresse, P" sort="Giresse, P" uniqKey="Giresse P" first="P" last="Giresse">P. Giresse</name></country><country name="République populaire de Chine"><noRegion><name sortKey="Hsieh, M L" sort="Hsieh, M L" uniqKey="Hsieh M" first="M. L" last="Hsieh">M. L Hsieh</name></noRegion><name sortKey="Liew, P M" sort="Liew, P M" uniqKey="Liew P" first="P. M" last="Liew">P. M Liew</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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