PPT-FAULTS AND FAULTING

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. 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.. and Folds. The illustration shows an east-west cross section between the Allegheny Structural Front and North Fork Mountain. The topographic feature called Germany Valley sits atop the geologic structure called the Wills Mountain Anticline. Westward directed compressive forces associated with the . Faults of the Los Angels Field trip. How were the San Gabriel Mountains uplifted? –Kim . Gloersen. . How the Raymond, Hollywood, and Santa Monica faults are related? –Diego Furtado. How are we “blind” to some of our faults? – Hannah . 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. Lecture 29. Gly. 326. Compression and deformation. In areas of compression, we have several options for deformation. Dependent on lithology, rock strength, confinement, fluid occurrence, etc.. Reverse/Thrust faults. 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.. Craig . Hyslop. Robert Stewart. Outline. Purpose. Process. Synthetics. Field . d. ata. Conclusions. 2. Purpose. 3. (. Engelkemeir. , 2006). Identification of blind faults. Depth: . 0-50m. Exploration. OROGENY. LED BY PROFESSOR DONNY HUTTON The North Cornwall/Bude coastal section contains probably the best exposed, most accessible and spectacular fold structures seen in western Europe. They, alon 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. Presented by. Kelly Benson. Mouiad Al-Wahah. 1. Definitions we agreed upon... Def 1. . Diagnosis is the problem of trying to find what is wrong with some system based on knowledge about the design/structure of the system, possible malfunctions that can occur in the system and observations made of the behavior of the system..