About: Incised valleys     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : owl:Thing, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
QRcode icon
http://dbpedia.demo.openlinksw.com/describe/?url=http%3A%2F%2Fdbpedia.org%2Fresource%2FIncised_valleys&invfp=IFP_OFF&sas=SAME_AS_OFF&graph=http%3A%2F%2Fdbpedia.org&graph=http%3A%2F%2Fdbpedia.org

Incised valleys are mountain-valley-like features that commonly result from river down cutting into coastal plains and continental shelves in response to marine regression. They are the key evidence to identify sequence boundary on seismic profiles and outcrops. The magnitudes of their down cutting have been used to estimate the global sea-level variations.

AttributesValues
rdfs:label
  • Incised valleys (en)
  • 下切谷 (zh)
rdfs:comment
  • Incised valleys are mountain-valley-like features that commonly result from river down cutting into coastal plains and continental shelves in response to marine regression. They are the key evidence to identify sequence boundary on seismic profiles and outcrops. The magnitudes of their down cutting have been used to estimate the global sea-level variations. (en)
  • 下切谷(incised valley)是冲积体系在向盆地扩展其河道时和由于海平面相对下降时侵蚀下覆地层而形成的水道或谷地。海平面下降時,侵蝕基準面(erosion base level)也跟著下降,導致河流向下切割形成河谷,海平面上升時,河谷被填。形成下切谷。此後此地質名詞也被廣泛應用到地表岩層露頭。下切谷是研究全球海平面升降的主要證據之一,亦是用來佐證全球古氣候的及古地理變遷。它也是被用來鑒定在地震地層學的層序界面(sequence boundary)。它的下切幅度可用來推算全球海平面下降及古氣候變遷。 (zh)
dcterms:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
sameAs
dbp:wikiPageUsesTemplate
has abstract
  • Incised valleys are mountain-valley-like features that commonly result from river down cutting into coastal plains and continental shelves in response to marine regression. They are the key evidence to identify sequence boundary on seismic profiles and outcrops. The magnitudes of their down cutting have been used to estimate the global sea-level variations. (en)
  • 下切谷(incised valley)是冲积体系在向盆地扩展其河道时和由于海平面相对下降时侵蚀下覆地层而形成的水道或谷地。海平面下降時,侵蝕基準面(erosion base level)也跟著下降,導致河流向下切割形成河谷,海平面上升時,河谷被填。形成下切谷。此後此地質名詞也被廣泛應用到地表岩層露頭。下切谷是研究全球海平面升降的主要證據之一,亦是用來佐證全球古氣候的及古地理變遷。它也是被用來鑒定在地震地層學的層序界面(sequence boundary)。它的下切幅度可用來推算全球海平面下降及古氣候變遷。 (zh)
prov:wasDerivedFrom
page length (characters) of wiki page
foaf:isPrimaryTopicOf
is Link from a Wikipage to another Wikipage of
is foaf:primaryTopic of
Faceted Search & Find service v1.17_git139 as of Feb 29 2024


Alternative Linked Data Documents: ODE     Content Formats:   [cxml] [csv]     RDF   [text] [turtle] [ld+json] [rdf+json] [rdf+xml]     ODATA   [atom+xml] [odata+json]     Microdata   [microdata+json] [html]    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 08.03.3330 as of Mar 19 2024, on Linux (x86_64-generic-linux-glibc212), Single-Server Edition (378 GB total memory, 59 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software