FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1987081901> ?p ?o ?g. }

• W1987081901 endingPage "152" @default.
• W1987081901 startingPage "136" @default.
• W1987081901 abstract "Serpentinites in the Eastern Desert (ED) of Egypt represent integral components of the ophiolites. Metamorphic textures of the serpentinites preserve the complex mineralogical evolution from primary peridotite through metamorphism, and late-stage hydrothermal alteration. Two textural types are distinguished in the olivines of the present serpentinized peridotites, namely (a) highly-strained olivine grains with kink bands, as in the deformed mantle tectonites from ophiolites, and (b) non-strained grains. The latter may represent recrystallized crystals during later thermal metamorphic events due to the intrusion of granite. On the basis of X-ray diffraction analysis, antigorite is the main serpentine minerals with lesser chrysotile and lizardite which indicates that serpentinites were formed under prograde metamorphism. Relict primary minerals of the serpentinites are Cr-spinel, olivine and pyroxene. Chrome spinel relicts have high Cr# (0.60–0.80), whereas primary olivines are Mg-rich nature (Fo = 89–96). Geochemical compositions of serpentinites indicate that they formed not at mid-ocean ridges but at spreading centers associated with subduction zones and this could have happened in a supra-subduction zone either in the fore-arc or back-arc environments. Mineral compositions of primary chrome spinels and olivines are similar to those of modern fore-arcs. High Cr# in the relict chrome spinels and Fo in the primary olivines of serpentinites indicate that they are residual after extensive partial melting and originated by sea-floor spreading during subduction initiation." @default.
• W1987081901 created "2016-06-24" @default.
• W1987081901 creator A5059460438 @default.
• W1987081901 creator A5073715306 @default.
• W1987081901 date "2007-11-01" @default.
• W1987081901 modified "2023-10-12" @default.
• W1987081901 title "Supra-subduction affinity in the Neoproterozoic serpentinites in the Eastern Desert, Egypt: Evidence from mineral composition" @default.
• W1987081901 cites W1966685022 @default.
• W1987081901 cites W1967383895 @default.
• W1987081901 cites W1969633270 @default.
• W1987081901 cites W1974198533 @default.
• W1987081901 cites W1977079376 @default.
• W1987081901 cites W1978340247 @default.
• W1987081901 cites W1983507683 @default.
• W1987081901 cites W1987808340 @default.
• W1987081901 cites W1997561609 @default.
• W1987081901 cites W1998332981 @default.
• W1987081901 cites W2002996518 @default.
• W1987081901 cites W2003512977 @default.
• W1987081901 cites W2004433271 @default.
• W1987081901 cites W2005692153 @default.
• W1987081901 cites W2009407007 @default.
• W1987081901 cites W2012546453 @default.
• W1987081901 cites W2019243990 @default.
• W1987081901 cites W2029622065 @default.
• W1987081901 cites W2035117002 @default.
• W1987081901 cites W2041176411 @default.
• W1987081901 cites W2047519592 @default.
• W1987081901 cites W2056097083 @default.
• W1987081901 cites W2061154266 @default.
• W1987081901 cites W2063274044 @default.
• W1987081901 cites W2064909748 @default.
• W1987081901 cites W2078521830 @default.
• W1987081901 cites W2080198117 @default.
• W1987081901 cites W2081103505 @default.
• W1987081901 cites W2081926816 @default.
• W1987081901 cites W2091211617 @default.
• W1987081901 cites W2122668781 @default.
• W1987081901 cites W2124201542 @default.
• W1987081901 cites W2125733132 @default.
• W1987081901 cites W2133692287 @default.
• W1987081901 cites W2139564482 @default.
• W1987081901 cites W2159008758 @default.
• W1987081901 cites W2161866809 @default.
• W1987081901 cites W2166828164 @default.
• W1987081901 cites W2168672163 @default.
• W1987081901 cites W2169111811 @default.
• W1987081901 cites W2263943679 @default.
• W1987081901 cites W2365796915 @default.
• W1987081901 cites W4229814417 @default.
• W1987081901 cites W4243774149 @default.
• W1987081901 doi "https://doi.org/10.1016/j.jafrearsci.2007.08.002" @default.
• W1987081901 hasPublicationYear "2007" @default.
• W1987081901 type Work @default.
• W1987081901 sameAs 1987081901 @default.
• W1987081901 citedByCount "75" @default.
• W1987081901 countsByYear W19870819012012 @default.
• W1987081901 countsByYear W19870819012013 @default.
• W1987081901 countsByYear W19870819012014 @default.
• W1987081901 countsByYear W19870819012015 @default.
• W1987081901 countsByYear W19870819012016 @default.
• W1987081901 countsByYear W19870819012017 @default.
• W1987081901 countsByYear W19870819012018 @default.
• W1987081901 countsByYear W19870819012019 @default.
• W1987081901 countsByYear W19870819012020 @default.
• W1987081901 countsByYear W19870819012021 @default.
• W1987081901 countsByYear W19870819012022 @default.
• W1987081901 countsByYear W19870819012023 @default.
• W1987081901 crossrefType "journal-article" @default.
• W1987081901 hasAuthorship W1987081901A5059460438 @default.
• W1987081901 hasAuthorship W1987081901A5073715306 @default.
• W1987081901 hasConcept C112764850 @default.
• W1987081901 hasConcept C127313418 @default.
• W1987081901 hasConcept C151730666 @default.
• W1987081901 hasConcept C17409809 @default.
• W1987081901 hasConcept C23923706 @default.
• W1987081901 hasConcept C26687426 @default.
• W1987081901 hasConcept C2778998827 @default.
• W1987081901 hasConcept C2780364934 @default.
• W1987081901 hasConcept C58097730 @default.
• W1987081901 hasConcept C67236022 @default.
• W1987081901 hasConcept C77928131 @default.
• W1987081901 hasConcept C84372278 @default.
• W1987081901 hasConceptScore W1987081901C112764850 @default.
• W1987081901 hasConceptScore W1987081901C127313418 @default.
• W1987081901 hasConceptScore W1987081901C151730666 @default.
• W1987081901 hasConceptScore W1987081901C17409809 @default.
• W1987081901 hasConceptScore W1987081901C23923706 @default.
• W1987081901 hasConceptScore W1987081901C26687426 @default.
• W1987081901 hasConceptScore W1987081901C2778998827 @default.
• W1987081901 hasConceptScore W1987081901C2780364934 @default.
• W1987081901 hasConceptScore W1987081901C58097730 @default.
• W1987081901 hasConceptScore W1987081901C67236022 @default.
• W1987081901 hasConceptScore W1987081901C77928131 @default.
• W1987081901 hasConceptScore W1987081901C84372278 @default.
• W1987081901 hasIssue "4-5" @default.
• W1987081901 hasLocation W19870819011 @default.
• W1987081901 hasOpenAccess W1987081901 @default.

• next