FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022272478> ?p ?o ?g. }

• W2022272478 endingPage "321" @default.
• W2022272478 startingPage "305" @default.
• W2022272478 abstract "Convergent continental margins are the primary host of both growth and loss of continental crust. Continental growth largely occurs via subduction-driven magmatism, whereas continental loss largely occurs via subduction erosion and sediment subduction. Because the latter typically involves partial recycling into magmas, both growth and loss of continental crust can be represented in the magmatic record. The degree of crustal recycling can be estimated from the initial Hf isotope signatures in both magmatic and detrital zircon grains. Recent insights into the geodynamic evolution of the Peruvian margin, in combination with a new dataset of Hf isotopic data on zircon from the Carboniferous to Early Cretaceous, enable us to (1) compare the geodynamic history of the southern Peruvian margin with its Hf isotopic evolution, and (2) quantify the crustal growth between 500 and 135 Ma. The data exhibit a correlation with trends in isotope composition v. time and reflect the dominantly extensional regime that prevailed from the onset of subduction from 530 Ma to c. 135 Ma. This study demonstrates that the Peruvian margin experienced continental growth with juvenile input to arc magmatism of 30–45% on average, and illustrates the use of U–Pb and Hf isotopes in zircon as a tool to trace episodes of crustal growth through time. Supplementary material: Hf istopic analyses on zircon (A1 and A2) and new U–Pb zircon ages (A3) are available at http://www.geolsoc.org.uk/SUP18661." @default.
• W2022272478 created "2016-06-24" @default.
• W2022272478 creator A5030081327 @default.
• W2022272478 creator A5031387958 @default.
• W2022272478 creator A5071532638 @default.
• W2022272478 creator A5077316743 @default.
• W2022272478 date "2013-09-09" @default.
• W2022272478 modified "2023-10-17" @default.
• W2022272478 title "A Hf-isotope perspective on continent formation in the south Peruvian Andes" @default.
• W2022272478 cites W150149165 @default.
• W2022272478 cites W1534749586 @default.
• W2022272478 cites W1674500046 @default.
• W2022272478 cites W1932261477 @default.
• W2022272478 cites W1967028244 @default.
• W2022272478 cites W1969083832 @default.
• W2022272478 cites W1970197610 @default.
• W2022272478 cites W1970752910 @default.
• W2022272478 cites W1978465122 @default.
• W2022272478 cites W1978488084 @default.
• W2022272478 cites W1980745168 @default.
• W2022272478 cites W1994048706 @default.
• W2022272478 cites W1996562355 @default.
• W2022272478 cites W2004934899 @default.
• W2022272478 cites W2008087815 @default.
• W2022272478 cites W2011305958 @default.
• W2022272478 cites W2013066991 @default.
• W2022272478 cites W2016855401 @default.
• W2022272478 cites W2017512729 @default.
• W2022272478 cites W2018626452 @default.
• W2022272478 cites W2019310190 @default.
• W2022272478 cites W2020973699 @default.
• W2022272478 cites W2024861829 @default.
• W2022272478 cites W2025432102 @default.
• W2022272478 cites W2029013584 @default.
• W2022272478 cites W2037717521 @default.
• W2022272478 cites W2039195953 @default.
• W2022272478 cites W2039848826 @default.
• W2022272478 cites W2040187777 @default.
• W2022272478 cites W2044175358 @default.
• W2022272478 cites W2050120676 @default.
• W2022272478 cites W2051164400 @default.
• W2022272478 cites W2059356468 @default.
• W2022272478 cites W2062965671 @default.
• W2022272478 cites W2064167853 @default.
• W2022272478 cites W2064531217 @default.
• W2022272478 cites W2067218810 @default.
• W2022272478 cites W2071646395 @default.
• W2022272478 cites W2071782561 @default.
• W2022272478 cites W2074674283 @default.
• W2022272478 cites W2077421659 @default.
• W2022272478 cites W2080325016 @default.
• W2022272478 cites W2081823548 @default.
• W2022272478 cites W2087112906 @default.
• W2022272478 cites W2090206242 @default.
• W2022272478 cites W2094194853 @default.
• W2022272478 cites W2095352961 @default.
• W2022272478 cites W2097502986 @default.
• W2022272478 cites W2099932450 @default.
• W2022272478 cites W2108390090 @default.
• W2022272478 cites W2109946900 @default.
• W2022272478 cites W2111835129 @default.
• W2022272478 cites W2112292068 @default.
• W2022272478 cites W2113626510 @default.
• W2022272478 cites W2115393563 @default.
• W2022272478 cites W2116197973 @default.
• W2022272478 cites W2118658585 @default.
• W2022272478 cites W2122005119 @default.
• W2022272478 cites W2124559878 @default.
• W2022272478 cites W2135538698 @default.
• W2022272478 cites W2137237427 @default.
• W2022272478 cites W2146004550 @default.
• W2022272478 cites W2146941374 @default.
• W2022272478 cites W2154635232 @default.
• W2022272478 cites W2156985625 @default.
• W2022272478 cites W2161200139 @default.
• W2022272478 cites W2169061213 @default.
• W2022272478 cites W2169426782 @default.
• W2022272478 cites W2169766597 @default.
• W2022272478 cites W2336838457 @default.
• W2022272478 cites W2615048764 @default.
• W2022272478 cites W3207805732 @default.
• W2022272478 cites W4232157889 @default.
• W2022272478 doi "https://doi.org/10.1144/sp389.6" @default.
• W2022272478 hasPublicationYear "2013" @default.
• W2022272478 type Work @default.
• W2022272478 sameAs 2022272478 @default.
• W2022272478 citedByCount "24" @default.
• W2022272478 countsByYear W20222724782017 @default.
• W2022272478 countsByYear W20222724782018 @default.
• W2022272478 countsByYear W20222724782019 @default.
• W2022272478 countsByYear W20222724782020 @default.
• W2022272478 countsByYear W20222724782021 @default.
• W2022272478 countsByYear W20222724782022 @default.
• W2022272478 countsByYear W20222724782023 @default.
• W2022272478 crossrefType "journal-article" @default.
• W2022272478 hasAuthorship W2022272478A5030081327 @default.
• W2022272478 hasAuthorship W2022272478A5031387958 @default.
• W2022272478 hasAuthorship W2022272478A5071532638 @default.

• next