The isotopic-geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise

Alekseeva K. S.; Popova L. P.; Postnikov A. V.; Postnikova O. V.

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The isotopic-geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise

机译：拜吉特山沉积区圈闭形成岩的同位素-地球年代学年龄

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The Lower Cambrian Usol'e Formation in the Kamov arch of the Baikit anteclise includes stratiform intrusions confined to several levels. According to isotopicaEuro'geochronological investigations, the age of stratiform intrusions composed of olivine dolerites is estimated to be 256.0 +/- 3.2 Ma.

机译：拜基特河前缘的卡莫夫拱门中的下寒武统乌索尔地层包括层状侵入体，其范围仅限于几个层次。根据同位素欧洲地质年代学调查，由橄榄石白云石构成的层状侵入体的年龄估计为256.0 +/- 3.2 Ma。

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《Doklady Earth Sciences》 |2016年第2期|1014-1018|共5页
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Alekseeva K. S.; Popova L. P.; Postnikov A. V.; Postnikova O. V.;
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Gubkin Russian State Univ Oil & Gas, Leninskii Pr 65, Moscow 119991, Russia;

Gubkin Russian State Univ Oil & Gas, Leninskii Pr 65, Moscow 119991, Russia;

Gubkin Russian State Univ Oil & Gas, Leninskii Pr 65, Moscow 119991, Russia;

Gubkin Russian State Univ Oil & Gas, Leninskii Pr 65, Moscow 119991, Russia;

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The isotopic-geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise

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