FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2171527602> ?p ?o ?g. }

• W2171527602 endingPage "298" @default.
• W2171527602 startingPage "284" @default.
• W2171527602 abstract "Abstract Quartz, the most common mineral in most sandstones, rarely is used in provenance studies. This study demonstrates the provenance-discriminatory potential of combining cathodoluminescence (CL) color wavelength spectra of quartz with morphology and in situ U-Pb ages of zircon. The Cambrian Meson Group in northwestern Argentina is used for the test of this combined methodology, because it is composed of nonmetamorphosed sandstones with > 90% quartz and a dominance of zircon among the heavy minerals. Correlation of the results from the two methods is evident: (1) both CL spectra typical for bright-luminescent quartz (red to blue; > 90%) and oscillatory zircon growth zoning (80–90%) indicate a dominance of magmatic detritus. (2) Upsection, diminishing input from euhedral 510–600 Ma zircons (70% at the base) correlates with lower amounts of volcanic quartz (40% red and violet grains at the base). Instead, plutonic quartz and abraded zircons of 550–700 Ma age prevail. The data point to the occurrence of a (nearly) synsedimentary volcanic phase, which has not been known previously. Furthermore, initial short transportation paths from nearby magmatic bodies (100–200 km) can be assumed, because of the low degree of grain abrasion and an age correlation with magmatic bodies in the region, such as the Santa Rosa de Tastil batholith, here dated at 513 +4/−5 Ma. The proximity to the source area at an initial stage indicates first-cycle sand. The maturity was probably reached by intense chemical weathering. The upsection-diminishing young, volcanic input indicates erosion of the volcanic source within a time period of millions of years. At that stage, mainly up to 1000-km-long coast-parallel transport from the Sierras Pampeanas in the south fed the depositional basin. The change in—and expansion of—the main source areas record a change to production of multicycle sand. Hence, the maturity was partly caused by sedimentary recycling. More generally, the provenance-discriminative effect of the CL of quartz, which has been doubted by some researches, can be confirmed. Therefore, the results imply that both quartz and zircon should be taken into account in provenance studies of quartz arenites." @default.
• W2171527602 created "2016-06-24" @default.
• W2171527602 creator A5024775226 @default.
• W2171527602 creator A5026172972 @default.
• W2171527602 creator A5033533452 @default.
• W2171527602 creator A5035681463 @default.
• W2171527602 creator A5071247100 @default.
• W2171527602 creator A5071533916 @default.
• W2171527602 creator A5076650405 @default.
• W2171527602 creator A5078046841 @default.
• W2171527602 creator A5079566558 @default.
• W2171527602 date "2011-04-01" @default.
• W2171527602 modified "2023-10-18" @default.
• W2171527602 title "Detrital Quartz and Zircon Combined: The Production of Mature Sand with Short Transportation Paths Along the Cambrian West Gondwana Margin, Northwestern Argentina" @default.
• W2171527602 cites W1491773648 @default.
• W2171527602 cites W1497248863 @default.
• W2171527602 cites W1518758285 @default.
• W2171527602 cites W1645227000 @default.
• W2171527602 cites W1774400765 @default.
• W2171527602 cites W1848401775 @default.
• W2171527602 cites W1980025974 @default.
• W2171527602 cites W1989194022 @default.
• W2171527602 cites W1989607362 @default.
• W2171527602 cites W1990466922 @default.
• W2171527602 cites W1991996087 @default.
• W2171527602 cites W1994072628 @default.
• W2171527602 cites W1994721399 @default.
• W2171527602 cites W1994816293 @default.
• W2171527602 cites W2002606625 @default.
• W2171527602 cites W2004684606 @default.
• W2171527602 cites W2008929168 @default.
• W2171527602 cites W2014601005 @default.
• W2171527602 cites W2015876559 @default.
• W2171527602 cites W2016848487 @default.
• W2171527602 cites W2017227039 @default.
• W2171527602 cites W2017950482 @default.
• W2171527602 cites W2023538324 @default.
• W2171527602 cites W2023601146 @default.
• W2171527602 cites W2023936068 @default.
• W2171527602 cites W2025247012 @default.
• W2171527602 cites W2035154010 @default.
• W2171527602 cites W2036174339 @default.
• W2171527602 cites W2039269540 @default.
• W2171527602 cites W2040280254 @default.
• W2171527602 cites W2043238774 @default.
• W2171527602 cites W2057695611 @default.
• W2171527602 cites W2060663380 @default.
• W2171527602 cites W2060695810 @default.
• W2171527602 cites W2066756809 @default.
• W2171527602 cites W2067143430 @default.
• W2171527602 cites W2070038511 @default.
• W2171527602 cites W2072933753 @default.
• W2171527602 cites W2077413291 @default.
• W2171527602 cites W2079002288 @default.
• W2171527602 cites W2088310768 @default.
• W2171527602 cites W2098839023 @default.
• W2171527602 cites W2099933884 @default.
• W2171527602 cites W2106297671 @default.
• W2171527602 cites W2108844550 @default.
• W2171527602 cites W2112168154 @default.
• W2171527602 cites W2116197973 @default.
• W2171527602 cites W2120006837 @default.
• W2171527602 cites W2129660904 @default.
• W2171527602 cites W2129945893 @default.
• W2171527602 cites W2136615364 @default.
• W2171527602 cites W2138217183 @default.
• W2171527602 cites W2138220934 @default.
• W2171527602 cites W2138335766 @default.
• W2171527602 cites W2139498789 @default.
• W2171527602 cites W2152210738 @default.
• W2171527602 cites W2157472312 @default.
• W2171527602 cites W2159557178 @default.
• W2171527602 cites W2161200139 @default.
• W2171527602 cites W2162245896 @default.
• W2171527602 cites W2167383433 @default.
• W2171527602 cites W2264388295 @default.
• W2171527602 cites W2313236783 @default.
• W2171527602 cites W2336738242 @default.
• W2171527602 cites W2493502679 @default.
• W2171527602 cites W2948581991 @default.
• W2171527602 cites W3162243377 @default.
• W2171527602 cites W373992856 @default.
• W2171527602 cites W2337202454 @default.
• W2171527602 doi "https://doi.org/10.2110/jsr.2011.23" @default.
• W2171527602 hasPublicationYear "2011" @default.
• W2171527602 type Work @default.
• W2171527602 sameAs 2171527602 @default.
• W2171527602 citedByCount "50" @default.
• W2171527602 countsByYear W21715276022012 @default.
• W2171527602 countsByYear W21715276022013 @default.
• W2171527602 countsByYear W21715276022014 @default.
• W2171527602 countsByYear W21715276022015 @default.
• W2171527602 countsByYear W21715276022016 @default.
• W2171527602 countsByYear W21715276022017 @default.
• W2171527602 countsByYear W21715276022018 @default.
• W2171527602 countsByYear W21715276022019 @default.
• W2171527602 countsByYear W21715276022020 @default.
• W2171527602 countsByYear W21715276022021 @default.

• next