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http://dx.doi.org/10.18419/opus-3804
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DC Element | Wert | Sprache |
---|---|---|
dc.contributor.author | Winsemann, Jutta | de |
dc.contributor.author | Seyfried, Hartmut | de |
dc.date.accessioned | 2009-09-04 | de |
dc.date.accessioned | 2016-03-31T08:06:44Z | - |
dc.date.available | 2009-09-04 | de |
dc.date.available | 2016-03-31T08:06:44Z | - |
dc.date.issued | 1991 | de |
dc.identifier.other | 316439797 | de |
dc.identifier.uri | http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-44913 | de |
dc.identifier.uri | http://elib.uni-stuttgart.de/handle/11682/3821 | - |
dc.identifier.uri | http://dx.doi.org/10.18419/opus-3804 | - |
dc.description.abstract | The incipient island-arc system of southern Central America (Cretaceous - early Oligocene) is characterized by thick turbidite systems, which mainly filled inner fore-arc troughs. Outcrop data show four second-order depositional sequences in the deep-water sediments. The formation of these depositional sequences is strongly related to the morphotectonic evolution of the island-arc system. Each depositional sequence reflects the complex interaction between global sea-level fluctuations, sediment supply and tectonic activity. Strong marginal uplift and high volcaniclastic sediment supply during early to late Paleocene and late Eocene times caused the formation of coarse-grained channel-lobe systems. During late Paleocene and mid-Eocene times, fine-grained, thin-bedded turbidite systems were deposited, owing to regional subsidence and a decrease in volcanic supply. Uplift and subsidence of sediment-source areas acted as major controls on deposition of basinal cycles. | en |
dc.language.iso | en | de |
dc.rights | info:eu-repo/semantics/openAccess | de |
dc.subject.classification | Meeresspiegelschwankung , Zentralamerika , Inselbogen | de |
dc.subject.ddc | 550 | de |
dc.title | Response of deep-water fore-arc systems to sea-level changes, tectonic activity and volcaniclastic input in Central America | en |
dc.type | bookPart | de |
ubs.fakultaet | Fakultät Luft- und Raumfahrttechnik und Geodäsie | de |
ubs.institut | Institut für Planetologie | de |
ubs.opusid | 4491 | de |
ubs.publikation.source | Macdonald, David I. M (Hrsg.): Sedimentation, tectonics and eustasy : Sea-level changes at active plate margins. Oxford : Blackwell Scientific Publ., 1991 (Special publication of the International Association of Sedimentologists, 12), S. 273-292 | de |
ubs.publikation.typ | Buchbeitrag | de |
Enthalten in den Sammlungen: | 06 Fakultät Luft- und Raumfahrttechnik und Geodäsie |
Dateien zu dieser Ressource:
Datei | Beschreibung | Größe | Format | |
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sey4.pdf | 1,02 MB | Adobe PDF | Öffnen/Anzeigen |
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