PPT-Faults FAULTS Introduction

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. 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. Regional Strain. Types of Fault and the Principal Stresses. Fault Rocks. Gouge: non-cohesive, fine grained. Breccia: coarse angular fragments. Cataclasite: cohesive fragments. Fault Melt (pseudotachylite):. 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.. 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 . 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. Layali Rashid. Errors that occur in bursts, at the same location, when the fault is activated . [WDSN07]. .. Faults which occur frequently and irregularly for a period of time . [ASPLOS08]. .. A persistent defect that causes zero or more failures, such as a speck of conductive dust partially bridging two traces . 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 . 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 . 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. 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.. lithosphere,. where movement occurs.. Stress. A force that presses on, pulls on, or pushes against another object.. Earthquake. The ground shaking caused by the sudden movement of large blocks of rock around a fault.. 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. 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 . 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..