FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2012306113> ?p ?o ?g. }

• W2012306113 endingPage "695" @default.
• W2012306113 startingPage "663" @default.
• W2012306113 abstract "The record of mafic magmatism from the Proterozoic to the Holocene in southern Australia reflects episodic incompatible element enrichment of the sub-continental lithospheric mantle (SCLM) recording periodic interaction of asthenosphere and lithosphere. The composition of Jurassic and Cainozoic mantle derived magmas is strongly influenced by the geochemical impact on the SCLM of events which took place during the Neoproterozoic and Cambrian. These events include rifting, passive margin development and orogenesis. Neoproterozoic to Cambrian basalts are widespread in western New South Wales, South Australia and Tasmania and reflect mantle decompression during extension and rifting of the Australian–East Antarctic Craton during the development of the proto-Pacific passive margin. These basalts fall into two regionally extensive and very different suites: (i) a voluminous suite of tholeiites and (ii) a highly undersaturated alkaline (nephelinite–basanite) series. Both Jurassic kimberlite magmas from the Adelaide Fold Belt and highly undersaturated Quaternary analcimites and basanites from the Mt. Gambier district of S.E. South Australia, have geochemical characteristics like those of the Precambrian–Cambrian alkaline suites. They have high concentrations of large ion lithophile (LIL), rare earth (RE) and high field strength (HFS) elements, and high HFSE/LILE and LREE/HREE ratios with TDMNd values of 0.5–0.8 Ga. The Jurassic kimberlites appear to sample lithospheric mantle enrichment zones of Late Neoproterozoic to Early Cambrian age. The Quaternary suites result from mixing of contemporary mantle plume components with this old lithospheric enrichment, which is also identified with the occurrence of metasomatic phlogopite, amphibole and apatite in lherzolite mantle xenoliths from a number of Cainozoic volcanoes in Western Victoria. A very different type of lithospheric mantle enrichment took place during the late stages of the Ross–Delamerian Orogeny. This yielded a crustally contaminated mantle zone that mirrors the Cambro-Ordovician position of that orogen. This zone of contaminated lithospheric mantle interacted with a large plume in the Jurassic to yield the highly anomalous Ferrar–Tasmanian–Kangaroo Island basalts and dolerites." @default.
• W2012306113 created "2016-06-24" @default.
• W2012306113 creator A5004188350 @default.
• W2012306113 creator A5073193745 @default.
• W2012306113 creator A5075666675 @default.
• W2012306113 creator A5076630029 @default.
• W2012306113 creator A5088982548 @default.
• W2012306113 creator A5089326778 @default.
• W2012306113 creator A5090734880 @default.
• W2012306113 date "2002-02-01" @default.
• W2012306113 modified "2023-09-23" @default.
• W2012306113 title "Geochemical evolution of lithospheric mantle beneath S.E. South Australia" @default.
• W2012306113 cites W1625450042 @default.
• W2012306113 cites W1661014045 @default.
• W2012306113 cites W1964358899 @default.
• W2012306113 cites W1971699179 @default.
• W2012306113 cites W1975633814 @default.
• W2012306113 cites W1982208132 @default.
• W2012306113 cites W1983142816 @default.
• W2012306113 cites W1983367474 @default.
• W2012306113 cites W1984397935 @default.
• W2012306113 cites W1985957692 @default.
• W2012306113 cites W1987389137 @default.
• W2012306113 cites W1989726031 @default.
• W2012306113 cites W1994235531 @default.
• W2012306113 cites W1995787462 @default.
• W2012306113 cites W1996555782 @default.
• W2012306113 cites W1998527267 @default.
• W2012306113 cites W1999710591 @default.
• W2012306113 cites W2002677375 @default.
• W2012306113 cites W2003126903 @default.
• W2012306113 cites W2006396228 @default.
• W2012306113 cites W2006599172 @default.
• W2012306113 cites W2010566952 @default.
• W2012306113 cites W2010979020 @default.
• W2012306113 cites W2011865824 @default.
• W2012306113 cites W2012740176 @default.
• W2012306113 cites W2014828526 @default.
• W2012306113 cites W2019890340 @default.
• W2012306113 cites W2020437910 @default.
• W2012306113 cites W2029905237 @default.
• W2012306113 cites W2030154085 @default.
• W2012306113 cites W2030711274 @default.
• W2012306113 cites W2033204481 @default.
• W2012306113 cites W2033683037 @default.
• W2012306113 cites W2038381700 @default.
• W2012306113 cites W2039135265 @default.
• W2012306113 cites W2041112329 @default.
• W2012306113 cites W2041931949 @default.
• W2012306113 cites W2042130595 @default.
• W2012306113 cites W2052383698 @default.
• W2012306113 cites W2052601169 @default.
• W2012306113 cites W2053979714 @default.
• W2012306113 cites W2060237332 @default.
• W2012306113 cites W2062440873 @default.
• W2012306113 cites W2063305856 @default.
• W2012306113 cites W2065636104 @default.
• W2012306113 cites W2066335781 @default.
• W2012306113 cites W2068530941 @default.
• W2012306113 cites W2081812021 @default.
• W2012306113 cites W2083733990 @default.
• W2012306113 cites W2088496938 @default.
• W2012306113 cites W2091754030 @default.
• W2012306113 cites W2093567690 @default.
• W2012306113 cites W2094845871 @default.
• W2012306113 cites W2095078676 @default.
• W2012306113 cites W2095419136 @default.
• W2012306113 cites W2096157355 @default.
• W2012306113 cites W2106510869 @default.
• W2012306113 cites W2111474515 @default.
• W2012306113 cites W2112650541 @default.
• W2012306113 cites W2139345858 @default.
• W2012306113 cites W2149084284 @default.
• W2012306113 cites W2328689481 @default.
• W2012306113 cites W2330355325 @default.
• W2012306113 cites W2558956011 @default.
• W2012306113 cites W4250496615 @default.
• W2012306113 cites W92306844 @default.
• W2012306113 doi "https://doi.org/10.1016/s0009-2541(01)00347-3" @default.
• W2012306113 hasPublicationYear "2002" @default.
• W2012306113 type Work @default.
• W2012306113 sameAs 2012306113 @default.
• W2012306113 citedByCount "62" @default.
• W2012306113 countsByYear W20123061132013 @default.
• W2012306113 countsByYear W20123061132014 @default.
• W2012306113 countsByYear W20123061132015 @default.
• W2012306113 countsByYear W20123061132016 @default.
• W2012306113 countsByYear W20123061132017 @default.
• W2012306113 countsByYear W20123061132018 @default.
• W2012306113 countsByYear W20123061132019 @default.
• W2012306113 countsByYear W20123061132020 @default.
• W2012306113 countsByYear W20123061132021 @default.
• W2012306113 countsByYear W20123061132022 @default.
• W2012306113 countsByYear W20123061132023 @default.
• W2012306113 crossrefType "journal-article" @default.
• W2012306113 hasAuthorship W2012306113A5004188350 @default.
• W2012306113 hasAuthorship W2012306113A5073193745 @default.
• W2012306113 hasAuthorship W2012306113A5075666675 @default.

• next