Explore: Lithostratigraphy

Lithostratigraphy is a sub-discipline of stratigraphy, the geological science associated with the study of strata or rock layers. Major focuses include

region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough

layered volcanic rocks. Stratigraphy has three related subfields: lithostratigraphy (lithologic stratigraphy), biostratigraphy (biologic stratigraphy)

In chronostratigraphy, a stage is a succession of rock strata laid down in a single age on the geologic timescale, which usually represents millions of

; Jahangir, H. (23 December 2022). "Ordovician of North Iran: New lithostratigraphy, palaeogeography and biogeographical links with South China and the

Series are subdivisions of rock layers based on the age of the rock and formally defined by international conventions of the geological timescale. A series

ago (Ma), which is preserved in Upper Jurassic strata. In European lithostratigraphy, the name "Malm" indicates rocks of Late Jurassic age. In the past

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In geology, a bed is a layer of sediment, sedimentary rock, or volcanic rock "bounded above and below by more or less well-defined bedding surfaces". A

The Sengsengebirge mountains are a folded mountain range in the Upper Austrian Pre-Alps and is part of the Northern Limestone Alps. The heavily karstified