PPT-Altay- Sayan Regional Seismic Network

Altai Sayan Branch of Geophysical Survey Siberian Branch of the RAS Geophysical Survey of Siberian Branch of the RAS Three seismological branches with regional scale seismic networks Altay. 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. Peter Novotny. 1. st. PACMAN workshop. 3. rd. February 2015, CERN. Seismic sensors in PACMAN - . Peter NOVOTNY - 3. rd. February 2015. 2. Outline. Why seismic sensors in PACMAN. How seismic sensors work. Seismic Instruments. and Data Acquisition Systems at MSSP. Waqas. Ali, Jr. Engineer. Micro Seismic Studies Programme. . . Government of Pakistan. Contents. Introduction. MSSP Seismic Network—Map. 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. What we can learn from. what we can’t feel. Celeste Labedz. Massachusetts Institute of Technology. Incorporated Research Institutions for Seismology. Summer Internship 2014. What can ambient seismic. ITET G. . MAGGIOLINI . & . “The green . school. network. ” . present. . What. . is. an . earthquake. ?. An earthquake (also known as a quake, . tremor) . is the . shaking of the surface. of the Earth, resulting from the sudden release of energy in the Earth's lithosphere that creates seismic waves. . Birhanu. . Abera. Managing . Data from . Seismic Networks. Pretoria. , . South Africa. 20 Aug . 2017. Outline. Introduction. M. ap of the current . ESSN . network. Data Acquisition and processing. D. Seismic . Waves. . are shock . waves . given off by earthquakes. . There are 2 types:. 1. . Body Waves. . originate from the . focus. (. F. ). travel . through. . the earth. . They’re used to locate . WELCOME . TO THE PRESENTATION ON THE CAMEROON SEISMIC NETWORK. PRESENTATION OF THE CAMEROON SEISMIC NETWORK . . MOUZONG PEMI MARCELIN. Department. of . Physics. , . University. of . Yaounde. 1. 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. Part 1. Seismic Waves and Interior of the Earth. The behaviour of seismic waves in the different layers of the earth provides the most authentic evidence about the composition and structure of the earth. The different types of waves, generated during the occurrence of an earthquake, are generally divided into three broad categories: . Alhakeem A . 1. , . Almubarak. H . 1. , Liu K . 1. , Al-. Bazzaz. W . 2 . 1. Missouri University of Science and Technology, Rolla, Missouri, United States, . . 2. Kuwait Institute for Scientific Research, Ahmadi, Kuwait. Siddharth Garia. 1. , . Arnab Kumar Pal. 1. , . Karangat. Ravi. 2. , Archana M Nair. 2. 1. Research Scholar, Department of Civil Engineering, Indian Institute of Technology, Guwahati, 781039, . India.