1996
DOI: 10.1086/629851
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Chemostratigraphic and Sequence Stratigraphic Constraints on Vendian-Cambrian Basin Dynamics, Northeast Siberian Craton

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Cited by 71 publications
(40 citation statements)
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“…10), but the absence of unique features at this boundary or independent means of correlation do not presently permit precise correlation between boundaries. There does not appear to be a sequence boundary at this level on the Siberian Platform Pelechaty et al, 1996;Pelechaty, 1998).…”
Section: Global Correlationsmentioning
confidence: 83%
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“…10), but the absence of unique features at this boundary or independent means of correlation do not presently permit precise correlation between boundaries. There does not appear to be a sequence boundary at this level on the Siberian Platform Pelechaty et al, 1996;Pelechaty, 1998).…”
Section: Global Correlationsmentioning
confidence: 83%
“…10. Global correlation of terminal Neoproterozoic mixed siliciclastic-carbonate successions within a chemostratigraphic framework of carbon-isotopic intervals based on a synthesized profile (after Pelechaty et al, 1996;Pelechaty, 1998;Saylor et al, 1998). Synthesized curve is based on the Mackenzie Mountains (after Kaufman et al, 1997;James et al, 2001).…”
Section: Intrabasinal Sequence Stratigraphic Correlationmentioning
confidence: 99%
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“…According to the zircon-based U-Pb datings [Bowring et al, 1993], the age of explosive basite breccias samples from the Olenek uplift (543.9±0.24 Ma) correlates with the age of potash-rhyolites (534.6±0.5 Ma) from the basal Lower Cambrian conglomerates in the Kharaulakh uplift section. The geodynamic evolution of the northeastern margin of the Siberian craton at the end of the Vendian and the beginning of the Cambrian periods is reflected not only in the magmatism, but also in the thicknesses and facial characteristics of the correlating sediments of the regional passive sea basins [Pelechaty et al, 1996]. The northern and eastern margins of the craton were subject to progressive uplifting at the end of the Vendian, which resulted in dewatering and paleokarsting.…”
Section: Introductionmentioning
confidence: 99%
“…Возраст эксплозивных брекчий Оленекского поднятия, определен-ный U-Pb методом по цирконам [Bowring et al, 1993], имеет значение 543.9±0.24 млн лет и коррелируется с возрастом гальки калиевых риолитов (534.6±0.5 млн лет) из базальных нижнекембрийских конгломератов в разрезе Хараулахского поднятия. Геодинамическая эволюция северо-восточной окраины Сибирского кратона в конце венда и начале кембрия отражена не только в магматизме, но и в мощностях и фациальных характе-ристиках коррелятных отложений региональных пассивных морских бассейнов [Pelechaty et al, 1996]. В конце венда обращенные к северу и востоку внешние части окраины кратона испытали прогрессивное воздымание, приведшее к осушению и образованию палеокарста.…”
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