FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022966061> ?p ?o ?g. }

• W2022966061 endingPage "161" @default.
• W2022966061 startingPage "141" @default.
• W2022966061 abstract "The succession recovered in ODP hole 107–651 in the young oceanic Vavilov basin (Tyrrhenian Sea) comprises, beneath a thick Pleistocene to Upper Pliocene sedimentary cover (chiefly volcanoclastics), four basement units: (1) MORB-type basaltic pillows and breccias; (2) a complex succession made of dolerites, albitites, basaltic breccias, metadolerite pebbles (including an intercalated sandy layer with periodotite clasts); (3) MORB-type basaltic pillows and breccias; (4) highly serpentinized peridotite. Between units 3 and 4, granitoid pebbles occur. This sequence is surprisingly similar to successions known in the Western Alps' Tethyan ophiolites. There, the sediments (Callovian-Oxfordian radiolarian cherts) lie stratigraphically upon breccias mostly derived from underlying serpentinite, and sometimes gabbroic basement. At some places, thin basaltic (tholeiitic) pillows and breccias occur between the radiolarian cherts and the breccias. From the comparison between a present day setting (the central Tyrrhenian Sea) and a formerly emplaced basement succession (the Western Alps), we stress the following (a) both the here-discussed ophiolites and oceanic basement are different from classical ophiolite sequences; (b) both occurrences imply unroofing of mantle rocks that therefore were directly outcropping on the seafloor; (c) such a comparison may indicate a very slow spreading rate for the Alpine Tethyan ocean." @default.
• W2022966061 created "2016-06-24" @default.
• W2022966061 creator A5010751948 @default.
• W2022966061 creator A5028436288 @default.
• W2022966061 creator A5052883373 @default.
• W2022966061 creator A5077897964 @default.
• W2022966061 creator A5084300899 @default.
• W2022966061 date "1991-01-01" @default.
• W2022966061 modified "2023-10-01" @default.
• W2022966061 title "Ophiolites and the oceanic crust: New evidence from the Tyrrhenian sea and the Western Alps" @default.
• W2022966061 cites W1964284264 @default.
• W2022966061 cites W1971570059 @default.
• W2022966061 cites W1975437244 @default.
• W2022966061 cites W1980341531 @default.
• W2022966061 cites W1981945610 @default.
• W2022966061 cites W2010269787 @default.
• W2022966061 cites W2016384800 @default.
• W2022966061 cites W2018177817 @default.
• W2022966061 cites W2023326037 @default.
• W2022966061 cites W2030900556 @default.
• W2022966061 cites W2035413994 @default.
• W2022966061 cites W2052338065 @default.
• W2022966061 cites W2065431202 @default.
• W2022966061 cites W2070679270 @default.
• W2022966061 cites W2095668284 @default.
• W2022966061 cites W2131688094 @default.
• W2022966061 cites W2602690113 @default.
• W2022966061 doi "https://doi.org/10.1016/0264-3707(91)90036-e" @default.
• W2022966061 hasPublicationYear "1991" @default.
• W2022966061 type Work @default.
• W2022966061 sameAs 2022966061 @default.
• W2022966061 citedByCount "9" @default.
• W2022966061 countsByYear W20229660612012 @default.
• W2022966061 countsByYear W20229660612014 @default.
• W2022966061 countsByYear W20229660612017 @default.
• W2022966061 crossrefType "journal-article" @default.
• W2022966061 hasAuthorship W2022966061A5010751948 @default.
• W2022966061 hasAuthorship W2022966061A5028436288 @default.
• W2022966061 hasAuthorship W2022966061A5052883373 @default.
• W2022966061 hasAuthorship W2022966061A5077897964 @default.
• W2022966061 hasAuthorship W2022966061A5084300899 @default.
• W2022966061 hasConcept C117485682 @default.
• W2022966061 hasConcept C120806208 @default.
• W2022966061 hasConcept C127313418 @default.
• W2022966061 hasConcept C127413603 @default.
• W2022966061 hasConcept C138170599 @default.
• W2022966061 hasConcept C147176958 @default.
• W2022966061 hasConcept C151730666 @default.
• W2022966061 hasConcept C154200439 @default.
• W2022966061 hasConcept C161509811 @default.
• W2022966061 hasConcept C17409809 @default.
• W2022966061 hasConcept C192241223 @default.
• W2022966061 hasConcept C193944797 @default.
• W2022966061 hasConcept C23923706 @default.
• W2022966061 hasConcept C2781297371 @default.
• W2022966061 hasConcept C58097730 @default.
• W2022966061 hasConcept C5900021 @default.
• W2022966061 hasConcept C62074269 @default.
• W2022966061 hasConcept C6494504 @default.
• W2022966061 hasConcept C77928131 @default.
• W2022966061 hasConcept C84372278 @default.
• W2022966061 hasConceptScore W2022966061C117485682 @default.
• W2022966061 hasConceptScore W2022966061C120806208 @default.
• W2022966061 hasConceptScore W2022966061C127313418 @default.
• W2022966061 hasConceptScore W2022966061C127413603 @default.
• W2022966061 hasConceptScore W2022966061C138170599 @default.
• W2022966061 hasConceptScore W2022966061C147176958 @default.
• W2022966061 hasConceptScore W2022966061C151730666 @default.
• W2022966061 hasConceptScore W2022966061C154200439 @default.
• W2022966061 hasConceptScore W2022966061C161509811 @default.
• W2022966061 hasConceptScore W2022966061C17409809 @default.
• W2022966061 hasConceptScore W2022966061C192241223 @default.
• W2022966061 hasConceptScore W2022966061C193944797 @default.
• W2022966061 hasConceptScore W2022966061C23923706 @default.
• W2022966061 hasConceptScore W2022966061C2781297371 @default.
• W2022966061 hasConceptScore W2022966061C58097730 @default.
• W2022966061 hasConceptScore W2022966061C5900021 @default.
• W2022966061 hasConceptScore W2022966061C62074269 @default.
• W2022966061 hasConceptScore W2022966061C6494504 @default.
• W2022966061 hasConceptScore W2022966061C77928131 @default.
• W2022966061 hasConceptScore W2022966061C84372278 @default.
• W2022966061 hasIssue "2-4" @default.
• W2022966061 hasLocation W20229660611 @default.
• W2022966061 hasOpenAccess W2022966061 @default.
• W2022966061 hasPrimaryLocation W20229660611 @default.
• W2022966061 hasRelatedWork W1989887413 @default.
• W2022966061 hasRelatedWork W2022966061 @default.
• W2022966061 hasRelatedWork W2024983567 @default.
• W2022966061 hasRelatedWork W2060383077 @default.
• W2022966061 hasRelatedWork W2061235729 @default.
• W2022966061 hasRelatedWork W2380676993 @default.
• W2022966061 hasRelatedWork W2753243649 @default.
• W2022966061 hasRelatedWork W2758547694 @default.
• W2022966061 hasRelatedWork W295388858 @default.
• W2022966061 hasRelatedWork W3141953751 @default.
• W2022966061 hasVolume "13" @default.
• W2022966061 isParatext "false" @default.
• W2022966061 isRetracted "false" @default.

• next