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Cited by 43 publications
(47 citation statements)
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“…Although their geometric relations with the San Juan terrane are not visible, these deposits are interpreted as postdating the accretion of the San Juan terrane to the Andean margin, which occurred therefore, in Late Campanian times (Hughes & Pilatasig 2002;Kerr et al 2002;Jaillard et al 2004;. This tectonic event is further documented on the continental margin of southern Ecuador and northern Peru, by the widespread deposition of a coarsening and shallowing upward sequence of conglomerates of Late Campanian age, unconformably overlain by transgressive marine shales of Early Maastrichtian age (Taipe et al 2004;Jaillard et al 1999; …”
Section: San Juan Terranementioning
confidence: 92%
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“…Although their geometric relations with the San Juan terrane are not visible, these deposits are interpreted as postdating the accretion of the San Juan terrane to the Andean margin, which occurred therefore, in Late Campanian times (Hughes & Pilatasig 2002;Kerr et al 2002;Jaillard et al 2004;. This tectonic event is further documented on the continental margin of southern Ecuador and northern Peru, by the widespread deposition of a coarsening and shallowing upward sequence of conglomerates of Late Campanian age, unconformably overlain by transgressive marine shales of Early Maastrichtian age (Taipe et al 2004;Jaillard et al 1999; …”
Section: San Juan Terranementioning
confidence: 92%
“…The age of accretion is assumed to be the same as in central Ecuador. Jaillard et al 1999;. Location Fig.…”
Section: Fig 6: Rare Earth Element (Left) and Multi-element (Right) mentioning
confidence: 99%
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“…Also outcropping in northern Peru-southern Ecuador, is the Cretaceous Lancones basin (Figure 1), which comprises a broadly folded, metalliferous volcanic section ranging in age from ~105-90 Ma, just younger than most of the Huarmey basin; hosts Late Cretaceous plutons correlated with those of the Coastal batholith; and sits structurally between the Amotape and Olmos massifs (Jaillard et al 1999;Winter et al 2010). The earliest magmatism, ~105-100 Ma, was a bimodal, tholeiitic to calc-alkaline basalt-dominated sequence of pillow basalt with associated volcanic massive sulphide deposits and low Nb and Y siliceous rocks; whereas younger 99-90 Ma magmatism involved both tholeiitic and calc-alkaline basalt, andesite and more siliceous lava (Winter 2008).…”
Section: Other Considerationsmentioning
confidence: 99%
“…Note locations of Figs. 4-6. ceous succession rests unconformably on Paleozoic-middle Cretaceous rocks of the forearc zones of southern Ecuador and northwestern Peru (Olsson, 1944;Jaillard et al, 1998Jaillard et al, , 1999.…”
Section: Geological Settingmentioning
confidence: 99%