Tectonics and Structural Geology

folding

Features from the Field: Sheath Folds

Samuele Papeschi and Hannah Davies October 4, 2021

Shear zones are areas of intense deformation that localize the movement of one block of the crust with respect to another. In previous posts, we have seen that shear zones contain some very deformed rocks called mylonites, lineations that tell us the direction of movement, and useful kinematic indicators, such as S-C fabrics, that allow …[Read More]

Features from the Field: Chevron Folds

Samuele Papeschi June 12, 2020

Folds are among the most strikingly beautiful structures we can observe in rocks. There are several ways folds may form in rocks. For instance, folds in sedimentary rocks may develop by liquefaction of soft sediments, but the most common way to produce folds – and also my favorite – is by deformation. When rocks are …[Read More]

About

Welcome to the blog of the Tectonics and Structural Geology (TS) Division of the European Geosciences Union (EGU). Here you can find a whole range of fun and informative posts related to tectonics and structural geology, such as interviews with established scientists, descriptions of common features in the field, as well as updates on the latest research being carried in these scientific areas. This blog is run with great enthusiasm by Hannah Davies, David Fernández-Blanco, Derya Gürer, Samuele Papeschi, Elenora van Rijsingen, Silvia Brizzi and Anne Pluymakers. Everybody is invited to contribute to the blog and submit posts to the editor-in-chief Hannah Davies.