PPT-Faults and Faulting

Regional Strain Types of Fault and the Principal Stresses Fault Rocks Gouge noncohesive fine grained Breccia coarse angular fragments Cataclasite cohesive fragments Fault Melt pseudotachylite. Dr. . Chuck . Neufeld. Lander University. Phonation Faults. Hypofunctional (Breathy) Phonation. Forced Breathiness. Hyperfunctional Phonation. Phonation Faults. Hypofunctional. (Breathy) Phonation. Failure to demand enough appropriate activity from the vocal mechanism. Chapter 6. Folding. Faulting. The buckling of a rock layer that was once horizontal. Buckles or folds appear on the landscape.. The main type of folds are:. Anticlines. Synclines. Faulting is the result of the movement of the earths plates. Faults occur where there is stress along a weak point in the earths crust.. Dr. . Chuck . Neufeld. Lander University. Resonance Faults. Faults Related to Nasal Resonance. Faults Related to Tone Color. Nasal Resonance Faults. Excessive Nasality. Insufficient Nasal Resonance. Nasal Resonance Faults. Abhilash Thekkilakattil. , Alan Burns, Radu Dobrin and Sasikumar Punnekkat. Motivation and Contribution. State of the art of mixed criticality scheduling . mainly . focuses . on. WCET overruns. WCET overruns are . Folding. When Earth’s crust bends, folds occur. Folding occurs under compression when forces act towards each other, such as when plates collide. . Folding & Faulting. Definitions. Compression. A – S55E. B – N25W. C – 305. D – 355. 1. The strike of the plane represented by the great circle trace on the equal area plot at left is:. A – S55E. B – N25W. C – 305. D – 355. 305 or N55W. Lemuel Jhon S. Libres. Janice Putian. Sta. Fe Lopez. If your pocket gets empty your faults will be many.. FAULT. FAULT. FAULT. FAULT. FAULT. A fracture along which there has been displacement of the sides relative to one another.. Faults form in rocks when the stresses overcome the internal strength of the rock resulting in a fracture. A fault can be defined as the displacement of once connected blocks of rock along a fault plane. This can occur in any direction with the blocks moving away from each other. Faults occur from both tensional and compressional forces. Lecture 11 – Brittle faulting. Geol 244 – structural geology. Lecture 11 – Brittle faulting. Types of Faults – Anderson’s theory. Explains conjugate . fault . systems. Fault planes inclined ~30° either side of . Move it, move it !!. What are they?. Fault: a break or fracture in the crust of Earth.. Earthquakes: shaking or trembling of the earth caused by movement along a fault.. Uplift: upward movement of Earth’s crust.. Chidambaram Alagappan. Vishwani. D. . Agrawal. Department of Electrical and Computer Engineering. Auburn University, AL 36849 USA. 5/9/2013. 2. Presentation Outline. Purpose. Introduction to Fault. Diagnosis. François . Renard, Jessica McBeck, Benoît . Cordonnier. The Njord Centre, Department . of. . Geosciences. , . University. . of. Oslo, Norway. ISTerre. , . University. Grenoble . Alpes. & CNRS, France. When stresses in the earth crust act on soft plastic rocks, they bend or fold the rocks. But when stresses act on hard, brittle rocks, they fracture or break the rocks. . A . fault is a type of fracture along which there has been relative movement displacing the wall rocks on either side of the fault.. During: Fault notes. After: Exit slip 4 questions. Day 1: Faults. Fault-. a breaks . in the earth’s surface along which rocks can . move.. Three . kinds of faults – determined by how the rocks move against each .