PPT-Seismic Processing Lab Manual and Wiki

using Schlumbergers Vista Software Package AASPI Bryce Hutchinson Thang Ha and Kurt J Marfurt University of Oklahoma Overview and update from last time The purpose of this project is to provide a thorough set of instructions for seismic processing This guide will be utilized in a lab in concert with a course on seismic processing . Douglas Wiens. Department of Earth & Planetary Sciences. Washington University in Saint Louis. Gung & . Romanowicz. . [2004]. Pozgay. , Wiens, et al. . [2009]. Outline . What is seismic attenuation?. Seismic velocities – P & S. Relationship to elastic moduli. Seismic anisotropy. . -- directional variation in seismic velocity. Seismic Attenuation – 1/. Q. p. & 1/Q. s. . -- What is seismic attenuation?. Stephan . Husen. , Edi . Kissling. , Claudia . Ryser. , Martin . Lüthi. , Martin Funk, Ginny Catania, Lauren Andrews, . Katrin. . Plenkers. Fabian Walter. 1. , . Philippe Roux. 1. , Claudia Röösli. Muhammad Husni Mubarak Lubis. Geophysics Dept.. Colorado School of Mines. Picture was taken from . www.eoearth.org. 1. Do. you know that…?. 383 Cetaceans (whale and dolphins) were stranded in the Northern of Gulf of Mexico from November 3, 2010 – . Surveying: . Predicting . Earthquake. Hazard; Finding Geothermal Energy. John N. . Louie. Nevada . Seismological . Lab. oratory. Dept. of Geological Sciences & Engineering. www.seismo.unr.edu. Why do I care. Earthquake. – shaking and trebling that results from the movement of rock beneath Earth’s surface.. Plate movement causes earthquakes from stress and faults in Earth’s crust. When the rock breaks earthquakes happen. November 2012 Istanbul, Turkey. C. . Neagoe. , L.M. . Manea. and C. Ionescu. National Institute for Earth Physics, . Magurele-Ilfov. , Romania. . In . February 1977, the Department of Seismology from the Romanian Geophysical and Geological Institute (GGI) together with the Laboratory of Geodynamics of the Romanian Academy formed the Centre of the Earth Physics (CEP). In 1994, after a governmental decision, CEP was transformed in the National Institute for Earth Physics (NIEP). NIEP is coordinated by the Romanian Ministry of Education, Research, Youth and Sport. . 3D seismic reflection image of the . Nankai. Subduction zone, Japan. Seismic Sources: Land Surveys. Many options! Hammer, weight-drop, dynamite, . vibroseis. . What frequencies are needed?. What energy level is needed (what distances do you need to cover)?. Core Contractors are your trustworthy team of Seismic Retrofit Contractors Los Angeles and surrounding areas that comply with the Los Angeles retrofit requirements and other municipalities in the retrofitting of buildings just like yours. Earthquake Mechanisms. Brittle Mechanical Model: “stick-slip”. Focal point: 3D point inside the lithosphere where the seismic event occurs. Epicenter: projection of focal point to the map surface . Hints and TipsHints and TipsBuilder ToolsBuilder ToolsTracking Object RevTracking Object RevWeb GraphicsWeb GraphicsWorkflowWorkflowTroubleshootingTroubleshootingYou are in Best Practices fo Yichuan Wang. 1. Purpose of Seismic Processing. 2. Seismic Processing Sequence. 3. Summary. Outline. 1. Purpose of Seismic Processing. To suppress noise in the field data and enhance the reflection. s. infrasound data in Kazakhstan. Alexandr Smirnov, Natalya . Mikhailova. , Aidyn . Mukambaev. Institute of Geophysical Research, Almaty, Kazakhstan. P2.3-116. P2.3-116. ABSTRACT. The monitoring system of NNC RK comprises five seismic arrays, eight 3-component stations, and three infrasound arrays. Every year, the network in Central Asia registers and processes some 20,000 seismic events. Among the total bulk of such processed events, about 5,000 events are blasts of different characters. Mainly, they are industrial quarry blasts. The technique has been developed and technology has been generated for recognition of the character of the event based on the set of seismic and infrasound data, which can also increase the accuracy of blast localization significantly on account of reliable reference to the specific quarry. For twelve quarries, template seismic waveforms have been produced. It has been shown that a record of the . ¹Kadiri A. U. and ²Kijko A..  . ¹Centre for Geodesy and Geodynamics, PMB 11, Toro, Bauchi State, Nigeria. ²Natural Hazard Centre, University of Pretoria, Pretoria, Republic of South Africa. T5.2-033.