FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2036165710> ?p ?o ?g. }

• W2036165710 endingPage "11099" @default.
• W2036165710 startingPage "11083" @default.
• W2036165710 abstract "The Sr isotopic behavior in hydrothermally altered rocks of a complete section through the Wadi Fizh oceanic crust in the Oman ophiolite was investigated in order to evaluate seawater‐rock interaction through the oceanic crust. On the basis of rock‐types, secondary mineral assemblage, alteration temperature, average 87 Sr/ 86 Sr of hydrothermal fluids, and degree of alteration, the section is divided into the following 5 sequences: (1) mainly basalts and clay minerals, low alteration temperature, average 87 Sr/ 86 Sr 0.70634, and 78% degree of alteration; (2) mainly basalts and chlorite, clay minerals and calcite, fairly low alteration temperature, average 87 Sr/ 86 Sr 0.70584, and 76% degree of alteration; (3) basalts and sheeted dike diabase and prehnite‐actinolite facies, moderate alteration temperature, average 87 Sr/ 86 Sr 0.70519, and 85% degree of alteration; (4) dike diabase, plagiogranite, metagabbro and epidosite and prehnite‐free greenschist facies, high alteration temperature, average 87 Sr/ 86 Sr 0.70514, and 65% degree of alteration; and (5) noncumulate and cumulate gabbro and amphibolite facies, very high alteration temperature, average 87 Sr/ 86 Sr 0.70413, and 85% degree of alteration. Alteration (metamorphic) grade deduced from secondary mineral assemblages generally increases versus stratigraphic depth. Only 15% of the rocks have escaped hydrothermal alteration. The estimated strontium isotopic compositions of hydrothermal fluids are much more water‐dominated than those reported previously from modern and ophiolitic hydrothermal systems. On the basis of ideal model analysis we conclude that the whole sequence of oceanic crust in the Wadi Fizh section has experienced seawater recharge (downflow zone). The evidence suggests that the Wadi Fizh section was located close to a segment boundary of the oceanic crust along a spreading axis." @default.
• W2036165710 created "2016-06-24" @default.
• W2036165710 creator A5002598321 @default.
• W2036165710 creator A5009924676 @default.
• W2036165710 creator A5022662732 @default.
• W2036165710 creator A5051682987 @default.
• W2036165710 creator A5063015312 @default.
• W2036165710 date "2001-06-10" @default.
• W2036165710 modified "2023-10-12" @default.
• W2036165710 title "Sr isotope geochemistry and hydrothermal alteration of the Oman ophiolite" @default.
• W2036165710 cites W1964330751 @default.
• W2036165710 cites W1965405020 @default.
• W2036165710 cites W1967419857 @default.
• W2036165710 cites W1969589297 @default.
• W2036165710 cites W1970745642 @default.
• W2036165710 cites W1975864669 @default.
• W2036165710 cites W1979820932 @default.
• W2036165710 cites W1981145264 @default.
• W2036165710 cites W1985249297 @default.
• W2036165710 cites W1992567491 @default.
• W2036165710 cites W2003244714 @default.
• W2036165710 cites W2004054108 @default.
• W2036165710 cites W2006145761 @default.
• W2036165710 cites W2017647614 @default.
• W2036165710 cites W2018122760 @default.
• W2036165710 cites W2021676665 @default.
• W2036165710 cites W2022747145 @default.
• W2036165710 cites W2023257022 @default.
• W2036165710 cites W2027100004 @default.
• W2036165710 cites W2027182817 @default.
• W2036165710 cites W2029279017 @default.
• W2036165710 cites W2032513677 @default.
• W2036165710 cites W2042298495 @default.
• W2036165710 cites W2045078148 @default.
• W2036165710 cites W2056837545 @default.
• W2036165710 cites W2057339808 @default.
• W2036165710 cites W2058382324 @default.
• W2036165710 cites W2059945916 @default.
• W2036165710 cites W2064284858 @default.
• W2036165710 cites W2073040869 @default.
• W2036165710 cites W2076680648 @default.
• W2036165710 cites W2076981416 @default.
• W2036165710 cites W2078395190 @default.
• W2036165710 cites W2086724893 @default.
• W2036165710 cites W2087448142 @default.
• W2036165710 cites W2088305435 @default.
• W2036165710 cites W2088625233 @default.
• W2036165710 cites W2091429053 @default.
• W2036165710 cites W2091950619 @default.
• W2036165710 cites W2094709181 @default.
• W2036165710 cites W2103517719 @default.
• W2036165710 cites W2107983905 @default.
• W2036165710 cites W2110075944 @default.
• W2036165710 cites W2118168812 @default.
• W2036165710 cites W2126455993 @default.
• W2036165710 cites W2143045284 @default.
• W2036165710 cites W2152929627 @default.
• W2036165710 cites W2168482363 @default.
• W2036165710 cites W2169942443 @default.
• W2036165710 cites W2314777318 @default.
• W2036165710 cites W2903935235 @default.
• W2036165710 cites W2910354382 @default.
• W2036165710 cites W4254876612 @default.
• W2036165710 cites W642264229 @default.
• W2036165710 cites W93909832 @default.
• W2036165710 cites W95482156 @default.
• W2036165710 doi "https://doi.org/10.1029/2000jb900456" @default.
• W2036165710 hasPublicationYear "2001" @default.
• W2036165710 type Work @default.
• W2036165710 sameAs 2036165710 @default.
• W2036165710 citedByCount "70" @default.
• W2036165710 countsByYear W20361657102012 @default.
• W2036165710 countsByYear W20361657102013 @default.
• W2036165710 countsByYear W20361657102014 @default.
• W2036165710 countsByYear W20361657102015 @default.
• W2036165710 countsByYear W20361657102016 @default.
• W2036165710 countsByYear W20361657102017 @default.
• W2036165710 countsByYear W20361657102018 @default.
• W2036165710 countsByYear W20361657102019 @default.
• W2036165710 countsByYear W20361657102020 @default.
• W2036165710 countsByYear W20361657102021 @default.
• W2036165710 countsByYear W20361657102022 @default.
• W2036165710 countsByYear W20361657102023 @default.
• W2036165710 crossrefType "journal-article" @default.
• W2036165710 hasAuthorship W2036165710A5002598321 @default.
• W2036165710 hasAuthorship W2036165710A5009924676 @default.
• W2036165710 hasAuthorship W2036165710A5022662732 @default.
• W2036165710 hasAuthorship W2036165710A5051682987 @default.
• W2036165710 hasAuthorship W2036165710A5063015312 @default.
• W2036165710 hasBestOaLocation W20361657101 @default.
• W2036165710 hasConcept C120806208 @default.
• W2036165710 hasConcept C127313418 @default.
• W2036165710 hasConcept C151730666 @default.
• W2036165710 hasConcept C154200439 @default.
• W2036165710 hasConcept C156622251 @default.
• W2036165710 hasConcept C161509811 @default.
• W2036165710 hasConcept C165205528 @default.
• W2036165710 hasConcept C17409809 @default.

• next