El Criogénico terminal, el Ediacárico y el Cámbrico temprano en la Plataforma Siberiana sudoccidental: estratotipos y limitotipos

Autores/as

DOI:

https://doi.org/10.3989/egeol.43595.570

Palabras clave:

Litoestratigrafía, Criogénico, Ediacárico, Cámbrico, Plataforma Siberiana

Resumen


Se propone a continuación una revisión estratigráfica del Criogénico terminal, el Ediacárico y el Cámbrico temprano en la Platafora Siberiana. Todas las unidades estratigráficas neoproterozoicas tardías llenan la cuenca remanente de Sayan. El registro sedimentario se adscribe al grupo Criogénico terminal y Ediacárico de Oselok y a la formación inferior cámbrica Ust’-Tagul. Se pueden subdividir en miembros a partir de su característico contenido en Dickinsonia.

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Citas

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Publicado

2019-12-30

Cómo citar

Sovetov, J. K., & Solovetskaya, L. V. (2019). El Criogénico terminal, el Ediacárico y el Cámbrico temprano en la Plataforma Siberiana sudoccidental: estratotipos y limitotipos. Estudios Geológicos, 75(2), e115. https://doi.org/10.3989/egeol.43595.570

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