Field evidence suggests that the Palaeoproterozoic Gowganda Formation in Canada is non-glacial in origin

Pubblicato online: 17 set 2021

Pagine: 73 - 91

Ricevuto: 21 apr 2021

Accettato: 14 lug 2021

DOI: https://doi.org/10.2478/logos-2021-0009

Parole chiave

Debris flow, lonestone dropstone, lamination varve, non-glacial diamictite tillite, Snowball Earth

© 2021 Mats O. Molén, published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.