Tectonics and Structural Geology

Fault rocks

Features from the Field: Shear Zones and Mylonites

Samuele Papeschi, Sandra McLaren and Hannah Davies January 25, 2021

The San Andreas Fault in California, the Alpine Fault in New Zealand, or the Main Frontal Thrust in the Himalayas are some of the most famous and largest fault zones that accommodate the relative displacement between two adjacent crustal blocks. Such faults, however, represent only the shallower expression of something much bigger: a crustal shear …[Read More]

TS Must-Read – Sibson (1977) Fault Rocks and Fault Mechanism

The Must-read team December 28, 2020

The paper “Fault Rocks and Fault Mechanisms” by R. H. Sibson (1977), was one of the first studies that established major connections between the rocks that form in faults, and their conditions and mechanics during formation at crustal scale. Concretely, Sibson (1977) established: 1.) links among the textures and lithologies that develop along fault zones …[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.