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Stratigraphic chart of Cambrian deposits in the Turukhansk-Irkutsk-Olekma region, Siberian Platform

机译:西伯利亚平台Turukhansk-Irkutsk-Olekma地区的寒武纪沉积物地层图

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The former stratigraphic chart of the Cambrian in the Turukhansk-Irkutsk-Olekma region of the Siberian Platform was compiled in 1986 and approved in 1988. Large amounts of data were obtained from new wells drilled in the western and northern parts of the region during the preceding 20 years. Modifications necessitated by new data entail an indefinitely continuous series of revised facies zonation, recognition of new facies areas, regions and zone, as well as definition of a regional early Mayan stratigraphic hiatus. A new local stratigraphic division is the Olenchima Member (base of the Evenk Formation) underlain by a hiatus. The term Kochumdek Formation is no longer used in the Bakhta region and its lithologically distinct subformations (Yasenga, Moktakon, Mara, and Abakun) were raised to formation rank. The Olenchima Formation is no longer used in the Baikit zone; but instead, the Litvintsevo Formation was established here by correlation.
机译:西伯利亚平台Turukhansk-Irkutsk-Olekma地区寒武纪的前地层图于1986年编制,并于1988年获得批准。 20年。新数据需要进行的修改需要无限连续地进行一系列修订后的相带划分,新相区,地区和地带的识别以及区域玛雅早期地层裂隙的定义。一个新的局部地层划分是Olechima成员(Evenk地层的基础),其下有一个裂隙。在巴赫塔地区不再使用Kochumdek地层一词,其岩性上不同的亚型(Yasenga,Moktakon,Mara和Abakun)被提升到地层等级。拜基特地区不再使用Olenchima组;但是,通过相关性在这里建立了Litvintsevo组。

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