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Дата публикации статьи в журнале: 2019/10/11
Название журнала: Восточно Европейский Научный Журнал, Выпуск:
49, Том: 3,
Страницы в выпуске: 18-30
Автор: Dorjnamjaa D.
Ulaanbaatar, Institute of Paleontology and Geology, Mongolian Academy of Sciences,
Ulaanbaatar, Institute of Paleontology and Geology, Mongolian Academy of Sciences,
Автор: Altanshagai G.
Ulaanbaatar, Institute of Paleontology and Geology, Mongolian Academy of Sciences,
Ulaanbaatar, Institute of Paleontology and Geology, Mongolian Academy of Sciences,
Анотация: This presentation considers deals with biostratigraphic peculiarities of the Zavkhan phosphate basin by example of the Tsagaanolom shelfy trough. The Tsagaanolom trough was formed a large shelfy basin that is located in the western part of the Khangai intraplate orocline geostructure and existed during Late Neoproterozoic to Early Cambrian times.This phosphate shelfy trough is important to Late Precambrian -
Cambrian geology and paleontology because the stratigraphic sections of the Maikhanuul (diamictite), Tsagaanolom (carbonate), Bayangol (terrigenous) and Salanygol (carbonate-terrigenous) formations are thick, relatively complete, well exposed and particularly correlatable with classical sections of the Siberian platform. Also important is the fact that the sections contain a combination of stratigraphic features seldom found elsewhere over this interval in a single region: diamictites, bacterial fossils, trace fossils, small shelly fossils, soft-bodied fossils, sponge spicules, archaeocyaths and calcimicrobes, abundant carbonates for carbon and strontium isotope stratigraphy, and good potential for sequence stratigraphy
Ключевые слова:
Bayangol section
Ediacarian-Lower Cambrian boundary
Bacterial fossils
Trace fossils
Softbodied fossils
Small shelly fossils
Данные для цитирования:
Dorjnamjaa D.,
Voinkov D.M.,
Altanshagai G. .
ON THE LOWER CAMBRIAN KHASAGTIAN GROUP OF THE ICHNOFOSSILS AND SOFT- BODIED FAUNA OF THE ZAVKHAN PHOSPHATE BASIN IN WEST MONGOLIA (18-30). Восточно Европейский Научный Журнал. Науки о Земле. 2019/10/11;
49(3):18-30.