AN ACTIVE NEOPROTEROZOIC CONTINENTAL MARGIN OF THE ZAVKHAN MICROCONTINENT (MONGOLIA): ISOTOPIC-GEOCHRONOLOGICAL EVIDENCE

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AN ACTIVE NEOPROTEROZOIC CONTINENTAL MARGIN OF THE ZAVKHAN MICROCONTINENT (MONGOLIA): ISOTOPIC-GEOCHRONOLOGICAL EVIDENCE

There have been presented the results of the study of a thick (no less than 2–3 km), extended (for more than 200 km) volcanogenic formation (Tsetsen-Uul or Yargait) in the south of the Zavkhan terrane of the Central Asian fold belt. The formation is an assemblage of frequently intercalating effusive...

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Bibliographic Details
Main Authors:	S. I. Shkolnik, E. F. Letnikova, L. Z. Reznitsky
Format:	Article
Language:	English
Published:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2022-12-01
Series:	Геодинамика и тектонофизика
Subjects:	central asian fold belt neoproterozoic zavkhan terrane volcanic rocks magmatic zircons u-pb-geochronology nd-isotopy petrogeochemistry active continental margin
Online Access:	https://www.gt-crust.ru/jour/article/view/1579
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