FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2007654325> ?p ?o ?g. }

• W2007654325 endingPage "520" @default.
• W2007654325 startingPage "510" @default.
• W2007654325 abstract "Some insights into the origin of cratonic mantle can be gained from “eclogite” (loosely defined here as an assemblage containing garnet and any pyroxene) xenoliths hosted in kimberlites erupted through Archean (~ 2.5­3.5 Gy) cratons. One subset of Archean eclogite xenoliths, the low MgO Archean xenoliths, is presently believed to represent metamorphosed fragments of ancient altered oceanic crust, leading to the suggestion that Archean cratons were built, at least in part, by the accretion of oceanic lithospheric segments. However, another Archean subset, the high MgO Archean eclogite xenoliths, have major and compatible trace-element (Ni and Cr) systematics similar to high MgO arc-eclogite xenoliths originating from the lithospheric root underlying the Sierra Nevada batholith in California, an example of a Phanerozoic arc. The Sierran high MgO arc-eclogites represent cumulates from hydrous basaltic magmas beneath a thick continental arc. The compositional similarities between the Archean and Sierran high MgO eclogites suggest that not only might the Archean high MgO eclogites have a cumulate origin, as has previously been suggested, but they may be arc-related. If so, Archean high MgO eclogites provide evidence from within the mantle roots of cratons that some form of arc magmatism contributed to the formation and evolution of Archean continents." @default.
• W2007654325 created "2016-06-24" @default.
• W2007654325 creator A5000404492 @default.
• W2007654325 creator A5065495069 @default.
• W2007654325 creator A5085973002 @default.
• W2007654325 date "2007-04-01" @default.
• W2007654325 modified "2023-10-16" @default.
• W2007654325 title "Similarities between Archean high MgO eclogites and Phanerozoic arc-eclogite cumulates and the role of arcs in Archean continent formation" @default.
• W2007654325 cites W1553799086 @default.
• W2007654325 cites W1568052543 @default.
• W2007654325 cites W1629623139 @default.
• W2007654325 cites W1671054346 @default.
• W2007654325 cites W1678990270 @default.
• W2007654325 cites W1739136493 @default.
• W2007654325 cites W1964175282 @default.
• W2007654325 cites W1966167298 @default.
• W2007654325 cites W1967700183 @default.
• W2007654325 cites W1968516644 @default.
• W2007654325 cites W1970458022 @default.
• W2007654325 cites W1977980012 @default.
• W2007654325 cites W1981756317 @default.
• W2007654325 cites W1982949455 @default.
• W2007654325 cites W1990672888 @default.
• W2007654325 cites W1995318237 @default.
• W2007654325 cites W2000505371 @default.
• W2007654325 cites W2000752806 @default.
• W2007654325 cites W2003424749 @default.
• W2007654325 cites W2010432538 @default.
• W2007654325 cites W2012177214 @default.
• W2007654325 cites W2016245690 @default.
• W2007654325 cites W2018281973 @default.
• W2007654325 cites W2020179468 @default.
• W2007654325 cites W2020950712 @default.
• W2007654325 cites W2022700538 @default.
• W2007654325 cites W2026722663 @default.
• W2007654325 cites W2027323798 @default.
• W2007654325 cites W2033593736 @default.
• W2007654325 cites W2035670944 @default.
• W2007654325 cites W2040868581 @default.
• W2007654325 cites W2042904816 @default.
• W2007654325 cites W2044271523 @default.
• W2007654325 cites W2050480893 @default.
• W2007654325 cites W2052516684 @default.
• W2007654325 cites W2056206848 @default.
• W2007654325 cites W2062995566 @default.
• W2007654325 cites W2078181903 @default.
• W2007654325 cites W2084422999 @default.
• W2007654325 cites W2089876889 @default.
• W2007654325 cites W2092151651 @default.
• W2007654325 cites W2092235841 @default.
• W2007654325 cites W2096648343 @default.
• W2007654325 cites W2103490462 @default.
• W2007654325 cites W2103910212 @default.
• W2007654325 cites W2108537504 @default.
• W2007654325 cites W2115357102 @default.
• W2007654325 cites W2120794222 @default.
• W2007654325 cites W2123291756 @default.
• W2007654325 cites W2123975486 @default.
• W2007654325 cites W2129174376 @default.
• W2007654325 cites W2133103627 @default.
• W2007654325 cites W2139755763 @default.
• W2007654325 cites W2142196194 @default.
• W2007654325 cites W2148876776 @default.
• W2007654325 cites W2149259280 @default.
• W2007654325 cites W2153863709 @default.
• W2007654325 cites W2157353434 @default.
• W2007654325 cites W2331893182 @default.
• W2007654325 cites W2772186758 @default.
• W2007654325 cites W4238977959 @default.
• W2007654325 cites W4241183408 @default.
• W2007654325 doi "https://doi.org/10.1016/j.epsl.2007.02.006" @default.
• W2007654325 hasPublicationYear "2007" @default.
• W2007654325 type Work @default.
• W2007654325 sameAs 2007654325 @default.
• W2007654325 citedByCount "25" @default.
• W2007654325 countsByYear W20076543252012 @default.
• W2007654325 countsByYear W20076543252013 @default.
• W2007654325 countsByYear W20076543252014 @default.
• W2007654325 countsByYear W20076543252015 @default.
• W2007654325 countsByYear W20076543252016 @default.
• W2007654325 countsByYear W20076543252017 @default.
• W2007654325 countsByYear W20076543252020 @default.
• W2007654325 countsByYear W20076543252022 @default.
• W2007654325 countsByYear W20076543252023 @default.
• W2007654325 crossrefType "journal-article" @default.
• W2007654325 hasAuthorship W2007654325A5000404492 @default.
• W2007654325 hasAuthorship W2007654325A5065495069 @default.
• W2007654325 hasAuthorship W2007654325A5085973002 @default.
• W2007654325 hasConcept C120806208 @default.
• W2007654325 hasConcept C127313418 @default.
• W2007654325 hasConcept C147717901 @default.
• W2007654325 hasConcept C149347711 @default.
• W2007654325 hasConcept C151730666 @default.
• W2007654325 hasConcept C161509811 @default.
• W2007654325 hasConcept C173347748 @default.
• W2007654325 hasConcept C17409809 @default.
• W2007654325 hasConcept C192241223 @default.
• W2007654325 hasConcept C2779430719 @default.

• next