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• W2016346688 abstract "Titanite, apatite, and in one case rutile, from a suite of twenty-seven samples representing the major phases of an extensive and well dated Archean plutonic domain of the northwestern Superior Province, have been dated by U-Pb to determine the temporal progress of thermal and hydrothermal events accompanying and following major plutonism and to assess the isotopic behaviour of these geochronometers. Most samples contain: (1) dark-brown titanite with 350–20 ppm U, showing shapes and textural relationships indicative of a primary magmatic origin and yielding ages corresponding either to the time of magmatic crystallization or to that of secondary metamorphic or magmatic events known in the area; (2) pale titanite with 30–2 ppm U, showing textural evidence for a secondary origin by breakdown of biotite, hornblende, oxide, or older titanite and yielding ages that in general post-date the major plutonic and metamorphic events in the area; (3) apatite containing 30–5 ppm U (occasionally up to 150 ppm U), showing igneous shapes and textural relationships, but yielding post-magmatic ages similar to those of coexisting pale titanite; (4) rutile (in one sample) postdating the ages of coexisting titanite and apatite. The common coexistence of two noncoeval titanite generations demonstrates that the often invoked mechanism of Pb diffusion during slow cooling in this case has no general validity. The distribution of primary dark titanite ages, however, could be explained by late closure to diffusion or, alternatively, as the result of resetting by the thermal or hydrothermal effects caused by younger plutonic activity. The ages of the secondary pale titanites probably reflect crystallization during discrete retrogressive events promoted by moderate heating or enhanced fluid activity. The correspondence between pale titanite and apatite ages suggests that the same processes also caused the isotopic resetting of apatite. On a regional scale the data pattern permits the identification of domains characterized by differences in the length and intensity of the thermal and hydrothermal processes. The most protracted activity is recorded in northern domains of the Berens River area, whereas the gold-mineralized Red Lake area in the south underwent a very rapid decline of the thermal/hydrothermal activity. These data also highlight important differences between the Red Lake and other gold camps of the Superior Province such as Hemlo and Val d’Or where hydrothermal activity, locally associated with mineralization, occurred as much as 30–80 m.y. after the major orogenic developments." @default.
• W2016346688 created "2016-06-24" @default.
• W2016346688 creator A5011213490 @default.
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• W2016346688 date "1998-09-01" @default.
• W2016346688 modified "2023-10-14" @default.
• W2016346688 title "The significance of titanite and apatite U-Pb ages: constraints for the post-magmatic thermal-hydrothermal evolution of a batholithic complex, Berens River area, northwestern Superior Province, Canada" @default.
• W2016346688 cites W1963779558 @default.
• W2016346688 cites W1965858395 @default.
• W2016346688 cites W1966256034 @default.
• W2016346688 cites W1968224497 @default.
• W2016346688 cites W1973207778 @default.
• W2016346688 cites W1973507208 @default.
• W2016346688 cites W1976876390 @default.
• W2016346688 cites W1978241751 @default.
• W2016346688 cites W1983558505 @default.
• W2016346688 cites W1984414126 @default.
• W2016346688 cites W1986509396 @default.
• W2016346688 cites W1989098814 @default.
• W2016346688 cites W1991233570 @default.
• W2016346688 cites W1991332592 @default.
• W2016346688 cites W1994320114 @default.
• W2016346688 cites W1994452277 @default.
• W2016346688 cites W1994857564 @default.
• W2016346688 cites W1999142835 @default.
• W2016346688 cites W2000700397 @default.
• W2016346688 cites W2003919078 @default.
• W2016346688 cites W2005356053 @default.
• W2016346688 cites W2007105153 @default.
• W2016346688 cites W2009416250 @default.
• W2016346688 cites W2016050505 @default.
• W2016346688 cites W2019239270 @default.
• W2016346688 cites W2023841314 @default.
• W2016346688 cites W2023902466 @default.
• W2016346688 cites W2025772790 @default.
• W2016346688 cites W2026559043 @default.
• W2016346688 cites W2033540463 @default.
• W2016346688 cites W2036889638 @default.
• W2016346688 cites W2043335427 @default.
• W2016346688 cites W2045916683 @default.
• W2016346688 cites W2046459821 @default.
• W2016346688 cites W2053204413 @default.
• W2016346688 cites W2054018939 @default.
• W2016346688 cites W2055357687 @default.
• W2016346688 cites W2060094561 @default.
• W2016346688 cites W2067703696 @default.
• W2016346688 cites W2068928600 @default.
• W2016346688 cites W2070732410 @default.
• W2016346688 cites W2071633582 @default.
• W2016346688 cites W2074783352 @default.
• W2016346688 cites W2075941297 @default.
• W2016346688 cites W2076774944 @default.
• W2016346688 cites W2078416236 @default.
• W2016346688 cites W2081886238 @default.
• W2016346688 cites W2082844473 @default.
• W2016346688 cites W2083774164 @default.
• W2016346688 cites W2086982406 @default.
• W2016346688 cites W2089013154 @default.
• W2016346688 cites W2092660030 @default.
• W2016346688 cites W2092742668 @default.
• W2016346688 cites W2098235917 @default.
• W2016346688 cites W2105662998 @default.
• W2016346688 cites W2112743924 @default.
• W2016346688 cites W2119661400 @default.
• W2016346688 cites W2119892892 @default.
• W2016346688 cites W2135960851 @default.
• W2016346688 cites W2154745839 @default.
• W2016346688 cites W2171410068 @default.
• W2016346688 cites W2314757460 @default.
• W2016346688 cites W2328023021 @default.
• W2016346688 cites W2331949527 @default.
• W2016346688 cites W2910017513 @default.
• W2016346688 cites W4249133946 @default.
• W2016346688 doi "https://doi.org/10.1016/s0016-7037(98)00225-7" @default.
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