FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2037125485> ?p ?o ?g. }

• W2037125485 endingPage "206" @default.
• W2037125485 startingPage "190" @default.
• W2037125485 abstract "We describe the diagnostic lithological and chemical features of distal tephras from major Middle-Late Pleistocene (560–36 ka) explosive eruptions of the Colli Albani volcanic district, central Italy. In particular, we explore the time-dependent variability of the Sr and Nd isotope compositions as a tool for recognising and pinpointing individual Colli Albani tephra in distal settings. The distal tephras investigated are in lacustrine and fluvial sediments of central Apennine intermountain basins located 70 km–100 km east of Colli Albani. The recognition of the Colli Albani tephras is essentially based on the K-foiditic composition of their glass, which, within the Italian volcanological framework, is a distinctive character of the Colli Albani pyroclasts. In detail, these tephras are attributed to the following eruptive units: Tufo Pisolitico di Trigoria (561 ± 2 ka); Tufo del Palatino–Tufo di Bagni Albule (530 ± 2/527 ± 2 ka), Tufo di Bagni Albule–Pozzolane Rosse air-fall sequence (517 ± 1 to 500 ± 3 ka), Pozzolane Rosse (457 ± 4 ka), Villa Senni (365 ± 4 ka), and Albano 5–7 (41 ± 7 to 36 ± 1 ka). These correlations are supported by 40Ar/39Ar dating of the distal tephras correlated to the Pozzolane Rosse (457.4 ± 1.7 ka), Villa Senni (365 ± 2 ka) and Albano 5–7 (41 ± 9 ka) and by 87Sr/86Sr measured on clinopyroxene crystals and fresh glassy scoria from distal Colli Albani tephras that range from ∼0.711 to ∼0.709. These ratios are similar to those that characterise the individual proximal correlative units, and show the same decreasing trend over time. In contrast, the 143Nd/144Nd ratios for proximal and distal bulk samples and clinopyroxene increase from ∼0.51212 to ∼0.51215 from the oldest to the youngest tephra deposit. In summary, the study of Sr and Nd isotope compositions that is here applied on products from the Colli Albani volcanic district is a powerful, complementary tool to the more traditional tephrostratigraphic methods (e.g., componentry and electron microprobe analysis) for fingerprinting of distal tephras over a large region of the central Mediterranean, and over a large time interval, such as from 560 ka to 36 ka." @default.
• W2037125485 created "2016-06-24" @default.
• W2037125485 creator A5002008601 @default.
• W2037125485 creator A5005471074 @default.
• W2037125485 creator A5014473232 @default.
• W2037125485 creator A5036092583 @default.
• W2037125485 creator A5045010145 @default.
• W2037125485 creator A5052231993 @default.
• W2037125485 creator A5070696810 @default.
• W2037125485 creator A5088624526 @default.
• W2037125485 date "2013-05-01" @default.
• W2037125485 modified "2023-10-06" @default.
• W2037125485 title "Isotopic (Sr–Nd) and major element fingerprinting of distal tephras: an application to the Middle-Late Pleistocene markers from the Colli Albani volcano, central Italy" @default.
• W2037125485 cites W1521520101 @default.
• W2037125485 cites W1597239205 @default.
• W2037125485 cites W1965229619 @default.
• W2037125485 cites W1968588309 @default.
• W2037125485 cites W1969568624 @default.
• W2037125485 cites W1974626411 @default.
• W2037125485 cites W1975950635 @default.
• W2037125485 cites W1979873789 @default.
• W2037125485 cites W1979886846 @default.
• W2037125485 cites W1982103310 @default.
• W2037125485 cites W1982112763 @default.
• W2037125485 cites W1987281920 @default.
• W2037125485 cites W1988766028 @default.
• W2037125485 cites W1992996398 @default.
• W2037125485 cites W1997371892 @default.
• W2037125485 cites W201047755 @default.
• W2037125485 cites W2011311424 @default.
• W2037125485 cites W2012654922 @default.
• W2037125485 cites W2014433902 @default.
• W2037125485 cites W2015458523 @default.
• W2037125485 cites W2019427646 @default.
• W2037125485 cites W2026167320 @default.
• W2037125485 cites W2026632683 @default.
• W2037125485 cites W2030382982 @default.
• W2037125485 cites W2035329267 @default.
• W2037125485 cites W2039099919 @default.
• W2037125485 cites W2040235128 @default.
• W2037125485 cites W2040792553 @default.
• W2037125485 cites W2042400590 @default.
• W2037125485 cites W2048758565 @default.
• W2037125485 cites W2049425791 @default.
• W2037125485 cites W2057996409 @default.
• W2037125485 cites W2058259298 @default.
• W2037125485 cites W2062130555 @default.
• W2037125485 cites W2063091092 @default.
• W2037125485 cites W2063981631 @default.
• W2037125485 cites W2064481213 @default.
• W2037125485 cites W2065348283 @default.
• W2037125485 cites W2067344713 @default.
• W2037125485 cites W2068693734 @default.
• W2037125485 cites W2069629042 @default.
• W2037125485 cites W2069790122 @default.
• W2037125485 cites W2069830384 @default.
• W2037125485 cites W2070537236 @default.
• W2037125485 cites W2072981849 @default.
• W2037125485 cites W2073089862 @default.
• W2037125485 cites W2076081783 @default.
• W2037125485 cites W2076517688 @default.
• W2037125485 cites W2077039816 @default.
• W2037125485 cites W2085330842 @default.
• W2037125485 cites W2093041656 @default.
• W2037125485 cites W2093862012 @default.
• W2037125485 cites W2094300543 @default.
• W2037125485 cites W2098849316 @default.
• W2037125485 cites W2099797625 @default.
• W2037125485 cites W2104835438 @default.
• W2037125485 cites W2114481107 @default.
• W2037125485 cites W2123706788 @default.
• W2037125485 cites W2145604970 @default.
• W2037125485 cites W2150287538 @default.
• W2037125485 cites W2156727182 @default.
• W2037125485 cites W2157099954 @default.
• W2037125485 cites W2163308204 @default.
• W2037125485 cites W2312354977 @default.
• W2037125485 doi "https://doi.org/10.1016/j.quascirev.2013.01.028" @default.
• W2037125485 hasPublicationYear "2013" @default.
• W2037125485 type Work @default.
• W2037125485 sameAs 2037125485 @default.
• W2037125485 citedByCount "51" @default.
• W2037125485 countsByYear W20371254852013 @default.
• W2037125485 countsByYear W20371254852014 @default.
• W2037125485 countsByYear W20371254852015 @default.
• W2037125485 countsByYear W20371254852016 @default.
• W2037125485 countsByYear W20371254852017 @default.
• W2037125485 countsByYear W20371254852018 @default.
• W2037125485 countsByYear W20371254852019 @default.
• W2037125485 countsByYear W20371254852020 @default.
• W2037125485 countsByYear W20371254852021 @default.
• W2037125485 countsByYear W20371254852022 @default.
• W2037125485 countsByYear W20371254852023 @default.
• W2037125485 crossrefType "journal-article" @default.
• W2037125485 hasAuthorship W2037125485A5002008601 @default.
• W2037125485 hasAuthorship W2037125485A5005471074 @default.
• W2037125485 hasAuthorship W2037125485A5014473232 @default.
• W2037125485 hasAuthorship W2037125485A5036092583 @default.

• next