Media Summary: Strain in the lithosphere localizes into tabular zones known as Riedalshear Simple explanation of development of Riedal and Conjugate Riedal The difference in how force/stress/pressure deforms rocks/rock layers depending on temperature.
Shear Faults In A Model Brittle Solid - Detailed Analysis & Overview
Strain in the lithosphere localizes into tabular zones known as Riedalshear Simple explanation of development of Riedal and Conjugate Riedal The difference in how force/stress/pressure deforms rocks/rock layers depending on temperature. Table of Contents: 00:13 - Objectives 08:40 - Hanging Wall (HW) vs. Foot Wall (FW) So I just want to take a moment here to explain where we're going to find Mini-lecture 11.1 - Rock deformation, part of the topic
This video is a continuation of the video discussing how rocks behave under different types of stress. Dr. Robert Butler, University of Portland, discusses Quartz-filled tension gashes are common features associated with semi-
![IITK NPTEL Structural Geology_Lecture 29: Faults & Faulting I [Prof. Santanu Misra]](https://i.ytimg.com/vi/BLvO-XQyg_U/mqdefault.jpg)
![IITK NPTEL Structural Geology_Lecture 31: Ductile Shear Zones I [Prof. Santanu Misra]](https://i.ytimg.com/vi/R3qFxu1PVmY/mqdefault.jpg)
