Year: 2024
Type: article
Abstract: The Middle Jurassic (Aalenian-Bajocian) terrigenous deposits in the southeastern part of the Inyali-Debin synclinorium, in which glendonites were found, were studied. Glendonites are most characteristic of the Bajocian; they are often found in the Upper Morzhovka subformation and are rarer in the Lower Debin subformation. These pseudomorphs are small in size and are represented by a single rosette-shaped morphotype. The presence of glendonites in these sedimentary rocks is an indicator of low bottom water temperature, which could be partly related to the great depth of the basin.
Author: I. V. Brynko
Language: English
Subfield: Paleontology
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: bronze
OpenAlex ID: W4405747805
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