https://vital.lib.tsu.ru/vital/access/manager/Index ${session.getAttribute("locale")} 5 https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996549 Tue 21 Feb 2023 10:04:44 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996548 Tue 21 Feb 2023 10:04:39 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996550 Tue 21 Feb 2023 10:04:33 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000997760 Tue 14 Mar 2023 14:48:16 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000997761 Tue 14 Mar 2023 14:48:15 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001010827 Thu 30 Nov 2023 09:40:47 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000926794 1 Mkm3) to other LIPs (e.g., Deccan, Emeishan and Siberian Traps), it remains controversial why this LIP did not contribute to a mass extinction and whether it is associated with the Weissert Event. This work presents new 40Ar/39Ar dating over a 425-m vertical stratigraphic profile (out of 1,000 m) that spans three formations of the PE-LIP in southern Brazil (low-Ti Vale do Sol, high-Ti Urubici, and high-Ti Palmas). Our data demonstrate that this mafic lava pile was emplaced in c. 2.0 m.y., from c. 135.5 Ma to c. 133.5 Ma, and endorse the hypothesis that the basaltic and andesitic flows of the Vale do Sol Formation (peak of mafic magmatism) contributed to the Weissert Event.]]> Mon 23 Jan 2023 10:02:20 KRAT ]]>