The First Finds of Glendonite in Permian Deposits of the North Okhotsk Region, Northeastern Asia

Authors

A. S. Biakov, Russian Academy of Sciences
N. A. Goryachev, Russian Academy of Sciences
V. I. Davydov, Boise State UniversityFollow
I. L. Vedernikov, Russian Academy of Sciences

Document Type

Article

Publication Date

7-2013

Abstract

Pseudomorphoses of calcite after ikàite are stellar rosette-like spheroid crystal nodules or clusters of up to 10 cm in cross size. These units are considered by many researchers as an indicator of low temperatures in a sedimentation basin (around 0̊C) [1—3]. They have repeatedly been found in Mesozoic and Cenozoic deposits of Siberia and the Russian Far East [1, 4, 5].

Publication Information

Biakov, A. S.; Goryachev, N. A.; Davydov, V. I.; and Vedernikov, I. L.. (2013). "The First Finds of Glendonite in Permian Deposits of the North Okhotsk Region, Northeastern Asia". Doklady Earth Sciences, 451(1), 716-718. https://doi.org/10.1134/S1028334X13070210