FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2220228056> ?p ?o ?g. }

• W2220228056 endingPage "45" @default.
• W2220228056 startingPage "36" @default.
• W2220228056 abstract "We have studied feldspar from crystalline rocks for its textural and spectral cathodoluminescence (CL) characteristics with the aim to reveal their provenance potential. We analyzed ca. 60 rock samples of plutonic, volcanic, metamorphic, and pegmatitic origin from different continents and of 16 Ma to 2 Ga age for their feldspar CL textures and ca. 1200 feldspar crystals from these rocks for their CL color spectra. Among the analyzed rocks, igneous feldspar is most commonly zoned, whereby oscillatory zoning can be confirmed to be typical for volcanic plagioclase. The volcanic plagioclase also less commonly contains twin lamellae that are visible in CL light than crystals from other rock types. Alkali feldspar, particularly from igneous and pegmatitic rocks, was noted to be most affected by alteration features, visible as dark spots, lines and irregular areas. The size of all textural features of up to ca. 150 μm, in combination with possible alteration in both the source area and the sedimentary system, makes the CL textures of feldspar possible to use for qualitative provenance research only. We observed alkali feldspar mostly to luminesce in a bluish color and sometimes in red, and plagioclase in green to yellow. The corresponding CL spectra are dominated by three apparent intensity peaks at 440–520 nm (mainly blue), 540–620 nm (mainly green) and 680–740 nm (red to infrared). A dominance of the peak in the green wavelength interval over the blue one for plagioclase makes CL particularly useful for the differentiation of plagioclase from alkali feldspar. An apparent peak position in red to infrared at < 710 nm for plagioclase mainly is present in mafic rocks. Present-day coastal sand from Peru containing feldspar with the red to infrared peak position mainly exceeding 725 nm for northern Peruvian sand and a larger variety for sand from southern Peru illustrates a discriminative effect of different source areas. We conclude that the provenance application particularly can reveal first-cycle input from mafic rocks and source variations for detritus from arid areas that has been affected by little feldspar alteration." @default.
• W2220228056 created "2016-06-24" @default.
• W2220228056 creator A5075644769 @default.
• W2220228056 creator A5079566558 @default.
• W2220228056 date "2016-05-01" @default.
• W2220228056 modified "2023-09-28" @default.
• W2220228056 title "Can cathodoluminescence of feldspar be used as provenance indicator?" @default.
• W2220228056 cites W1965536973 @default.
• W2220228056 cites W1966610036 @default.
• W2220228056 cites W1966743027 @default.
• W2220228056 cites W1969026638 @default.
• W2220228056 cites W1980900466 @default.
• W2220228056 cites W1981257150 @default.
• W2220228056 cites W1984649966 @default.
• W2220228056 cites W1990738627 @default.
• W2220228056 cites W1992409488 @default.
• W2220228056 cites W1995834166 @default.
• W2220228056 cites W1998536804 @default.
• W2220228056 cites W2001452758 @default.
• W2220228056 cites W2006771799 @default.
• W2220228056 cites W2014716391 @default.
• W2220228056 cites W2016223358 @default.
• W2220228056 cites W2018208607 @default.
• W2220228056 cites W2024136445 @default.
• W2220228056 cites W2025695689 @default.
• W2220228056 cites W2033615573 @default.
• W2220228056 cites W2034153820 @default.
• W2220228056 cites W2034671041 @default.
• W2220228056 cites W2048456559 @default.
• W2220228056 cites W2067494608 @default.
• W2220228056 cites W2073603856 @default.
• W2220228056 cites W2077040595 @default.
• W2220228056 cites W2078261387 @default.
• W2220228056 cites W2082055190 @default.
• W2220228056 cites W2088450895 @default.
• W2220228056 cites W2088732846 @default.
• W2220228056 cites W2090011292 @default.
• W2220228056 cites W2106345479 @default.
• W2220228056 cites W2112939371 @default.
• W2220228056 cites W2116130991 @default.
• W2220228056 cites W2122181363 @default.
• W2220228056 cites W2128900796 @default.
• W2220228056 cites W2135979974 @default.
• W2220228056 cites W2138587114 @default.
• W2220228056 cites W2161130424 @default.
• W2220228056 cites W2162662157 @default.
• W2220228056 cites W2165562992 @default.
• W2220228056 cites W2171527602 @default.
• W2220228056 cites W2321999060 @default.
• W2220228056 cites W2332091137 @default.
• W2220228056 cites W2335763525 @default.
• W2220228056 cites W67357498 @default.
• W2220228056 cites W7942603 @default.
• W2220228056 doi "https://doi.org/10.1016/j.sedgeo.2015.11.005" @default.
• W2220228056 hasPublicationYear "2016" @default.
• W2220228056 type Work @default.
• W2220228056 sameAs 2220228056 @default.
• W2220228056 citedByCount "5" @default.
• W2220228056 countsByYear W22202280562017 @default.
• W2220228056 countsByYear W22202280562019 @default.
• W2220228056 countsByYear W22202280562020 @default.
• W2220228056 countsByYear W22202280562022 @default.
• W2220228056 crossrefType "journal-article" @default.
• W2220228056 hasAuthorship W2220228056A5075644769 @default.
• W2220228056 hasAuthorship W2220228056A5079566558 @default.
• W2220228056 hasConcept C120806208 @default.
• W2220228056 hasConcept C127313418 @default.
• W2220228056 hasConcept C139861200 @default.
• W2220228056 hasConcept C148869448 @default.
• W2220228056 hasConcept C151730666 @default.
• W2220228056 hasConcept C17409809 @default.
• W2220228056 hasConcept C192241223 @default.
• W2220228056 hasConcept C192562407 @default.
• W2220228056 hasConcept C195845463 @default.
• W2220228056 hasConcept C199289684 @default.
• W2220228056 hasConcept C2777729578 @default.
• W2220228056 hasConcept C2778520076 @default.
• W2220228056 hasConcept C2779181077 @default.
• W2220228056 hasConcept C2779870107 @default.
• W2220228056 hasConcept C2780049196 @default.
• W2220228056 hasConcept C42787717 @default.
• W2220228056 hasConcept C49040817 @default.
• W2220228056 hasConceptScore W2220228056C120806208 @default.
• W2220228056 hasConceptScore W2220228056C127313418 @default.
• W2220228056 hasConceptScore W2220228056C139861200 @default.
• W2220228056 hasConceptScore W2220228056C148869448 @default.
• W2220228056 hasConceptScore W2220228056C151730666 @default.
• W2220228056 hasConceptScore W2220228056C17409809 @default.
• W2220228056 hasConceptScore W2220228056C192241223 @default.
• W2220228056 hasConceptScore W2220228056C192562407 @default.
• W2220228056 hasConceptScore W2220228056C195845463 @default.
• W2220228056 hasConceptScore W2220228056C199289684 @default.
• W2220228056 hasConceptScore W2220228056C2777729578 @default.
• W2220228056 hasConceptScore W2220228056C2778520076 @default.
• W2220228056 hasConceptScore W2220228056C2779181077 @default.
• W2220228056 hasConceptScore W2220228056C2779870107 @default.
• W2220228056 hasConceptScore W2220228056C2780049196 @default.
• W2220228056 hasConceptScore W2220228056C42787717 @default.

• next