Chemostratigraphy and detrital zircon geochronology of the Neoproterozoic Khorbusuonka Group, Olenek Uplift, Northeastern Siberian platform


статья в журнале
Авторы: Vishnevskaya I.A.   (ИГМ СО РАН)   Letnikova E.F.   (ИГМ СО РАН)   Vetrova N.I.   (ИГМ СО РАН)   Kochnev B.B.   (ИНГГ СО РАН)   Dril S.I.    
дата публикации: 2017
реферат:
This study provides 87Sr/86Sr, δ13C and δ18O data from the best-preserved limestone and dolomite of the Ediacaran carbonate-dominated Khorbusuonka Group of the Olenek Uplift, NE Siberian Craton, as well as detrital zircon geochronological data from both underlying and overlying sandstones. The Maastakh Formation is characterized by 87Sr/86Sr ratios of ca. 0.70822 and δ13C values between + 4.8 and + 6.0‰. 87Sr/86Sr ratios in limestones of the Khatyspyt Formation are fairly uniform, ranging from 0.70783 to 0.70806. The carbon isotopic composition slowly decreases from bottom (+ 3.7‰) to top (- 0.2‰) of section. The Sr isotopic composition of the Turkut Formation varies from 0.70824 to 0.70914, value of δ13C is about zero: - 0.7...+0.7 ‰. The youngest population of detrital zircons from Maastakh Formation indicates that these rocks were formed not later than 630 Ma. U-Pb detrital zircons data of Kessyusa Group has a single peak at about 543 Ma, which is almost identical to the earlier dating.
первоисточник: Gondwana Research
том:
страницы: 255-271
ISBN:
ISSN:
внешние ссылки:
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DOI  
РИНЦ SPIN  
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полный текст статьи

gr-2017-51-255