1 edition of Seismicity and seismotectonic study of the Kermit seismic zone, Texas found in the catalog.
Seismicity and seismotectonic study of the Kermit seismic zone, Texas
|Statement||by G.R. Keller ... [et al.] ; United States Department of the Interior, Geological Survey|
|Series||Open-file report -- 81-37, Open-file report (Geological Survey (U.S.)) -- 81-37|
|Contributions||Keller, G. Randy 1946-, Geological Survey (U.S.). Office of Earthquake Studies|
|The Physical Object|
|Pagination||iv, 383 p. :|
|Number of Pages||383|
This book represents a significant contribution to the area of earthquake data processing and to the development of region-specific magnitude correlations to create an up-to-date homogeneous earthquake catalogue that is uniform in magnitude scale. The book discusses seismicity analysis and estimation of seismicity parameters of a region at both finer and broader levels using different. Seismic Design Categories. The NEHRP Recommended Seismic Provisions. recognizes that, independent of the quality of their design and construction, not all buildings pose the same seis-mic risk. Factors that affect a structure’s seismic risk include: • The intensity of ground shaking and other earthquake effects the structureFile Size: 1MB.
Seismic energy is defined as the area under the curve of the velocity spectrum of a triaxial waveform. The seismic moment is a quantity to measure the strength of a seismic event by considering the double couple, shear dislocation source model parameters. The concept behind the Energy-Moment relation is for an event with larger seismic moment. B.F. Howell Jr., in International Geophysics, Bock, Günter (–) German geophysicist who died prematurely in a plane crash on Nov. 6, He listed his seismological interests as (1) development of models on reservoir-induced seismicity, (2) investigation of the effect of subducting lithosphere on travel times of body waves, (3) study of the Earth's mantle using body waves and.
TexasEQ Reference List. Abe, K., , Magnitudes of large shallow earthquakes from to , Phys. Earth , 27, Aguilera, J. G., , The. Development of a seismotectonic map for India Seismic source models Summary. 3 Deterministic seismic hazard assessment Introduction Methodology Estimation of hazard for Indian subcontinent Discussions. 4 Seismicity analysis and characterization of source zones Introduction Seismicity analysis.
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A Seismicity and seismotectonic study of the Kermit seismic zone, Texas Open-File Report By: Gordon R. Keller, A.M.
Rogers, and R.J. Texas book. This work presents and summarizes all data that were collected during the operation of a station seismograph network in the vicinity of Kermit, Texas, during the period December to September The results of this study have several implications relating to the seismic hazard at the Waste.
Get this from a library. A Seismicity and seismotectonic study of the Kermit seismic zone, Texas. [G Randy Keller; Geological Survey (U.S.). Office of Earthquake Studies.;].
Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more. Two distinct areas of seismic activity were delineated during the course of the earthquake monitoring and were named the Kermit seismic zone because of their proximity to the town of Kermit, Texas.
One area of pronounced seismic activity was located in the Delaware basin in the vicinity of the War-Wink South gas field. A second area of seismic activity occurred on the Central Basin platform in the vicinity of the Keystone field Author: Cynthia Dolores Orr.
The purpose of this study was to investigate the seismicity and contemporary stress regime (seismotectonics) of the Delaware basin and the Central Basin platform of west Texas and southeastern New.
A SEISMOTECTONIC STUDY AND STRESS ANALYSIS OF THE KERMIT SEISMIC ZONE, TEXAS (SEISMOTECTONIC, WEST, FINITE ELEMENT ANALYSIS, HYDRAULIC FRACTURING, EARTHQUAKE) By CYNTHIA DOLORES ORR. Abstract. The purpose of this study was to investigate the seismicity and contemporary stress regime (seismotectonics) of the Delaware basin and the Author: CYNTHIA DOLORES ORR.
Seismicity of the Intermountain Seismic Belt Author(s) (Engdahl and Rinehart, ). The ISB is a prominent northerly-trending zone of mostly shallow (earthquakes, about to km wide, that extends in a curvilinear, branching pattern at least km from southern Nevada and northern Arizona to northwestern Montana (Fig.
We have relocated seismicity occurring in the Permian Basin of west Texas between and using three-dimensional velocity models constructed from well log information and compared the locations to detailed geological and geophysical models of specific oil fields.
The seismicity appears to be related to a variety of causes including migration of naturally occurring overpressured fluids, tectonic activity, reservoir production, and enhanced recovery by: SEISMICITY AND SEISMOTECTONIC STUDY FOR ALTUNKOPRI DAM SITE NORTH IRAQ N.
Alridha, R. Baqir, A.R. Hamid Department of Geology, College of Science, University of Baghdad. Baghdad-Iraq Abstract A seismicity and seismotectonicstudy for a. The workshop is devoted to the seismicity and seismological observations of the Baltic Sea region and adjacent territories: historical and present situation, installation of new seismic stations, processing and analysis of seismic data, seismic hazard assessment and risk mitigation.
The ability to predict the magnitude of an earthquake caused by deep fluid injections is an important factor for assessing the safety of the reservoir storage and the seismic hazard.
Here, we Cited by: 4. Apply Filter. © Katalyst Data Management LP. A seismicity and seismotectonic study of the Kermit seismic zone, Texas, by G. Keller, A. Rogers, and R. Lund, p. Geologic data for borehole ERDA-6, Eddy County, New Mexico, by C.
Jones, 59 p. Geologic data for borehole ERDA Author: V.M. Glanzman. Colorado Law and Induced Seismicity. located over a ver y active seismic zone in the Aleutian Islands. the seismotectonic study concluded that the Ridgway Fault and the branch faults were. Understanding Seismic Zones Rebecca South • Published Aug pm • The President’s Sphere To understand the Seismic Zoning method and how it pertains to the Monolithic Dome, we must first understand what effective peak ground acceleration means and how it .Who's who in Texas today: a new biographical survey of Texas / researched, compiled and edited by International Biographical Research Corporation.
Wikipedia Citation. Please see Wikipedia's template documentation for further citation fields that may be required. University of Liverpool researchers undertook a study in response to a request from the Department of Business, Energy and Industrial Strategy (BEIS) to assess induced seismicity and the.
Orr, Cynthia D.,A seismotectonic study and stress analysis of the Kermit Seismic zone, Texas; p. Simpson, Ronald D.,Permian brachiopoda from far west Texas. Seismicity. Seismicity is defined by a number of seismic events occurring within a given volume of rock over a certain period of time and is quantified using mainly the four largely independent quantities: (1) average time between events, (2) average distance between consecutive events, (3) cumulative seismic potency or seismic moment, and (4) cumulative radiated energies.
Although you may hear the terms “seismic zone” and “seismic hazard zone” used interchangeably, they really describe two slightly different things. A seismic zone is used to describe an area where earthquakes tend to focus; for example, the New Madrid Seismic Zone in the Central United States.
A seismic hazard zone describes an area with a particular level of hazard due to.Zone 0 = g Zone 1 = g Zone 2A = g Zone 2B = g Zone 3 = g Zone 4 = g Source: Edition UBC Seismic Zones (Ground Acceleration) Kaua‘i O‘ahu Maui Honolulu Seattle Portland Rexburg Reno Los Angeles Las Vegas San Francisco San Jose San Diego Fort Worth Dallas Houston Kansas City Wichita Norman White Plains Miami.Abstract.
This chapter examines seismicity in Oregon and Washington, and combines historical accounts of damaging earthquakes with the detail of recent seismic.