A. Ghosh, EAS, Georgia Tech Distribution of b-value in the Middle America Trench, near Nicoya Peninsula, Costa Rica Abhijit Ghosh A. V. Newman, A. M. Thomas,

Slides:



Advertisements
Similar presentations
Role of Space Geodesy In GEOSS Timothy H. Dixon University of Miami/RSMAS and Center for Southeastern Advanced Remote Sensing (CSTARS)
Advertisements

Mmax and the Maximum Catalog Magnitude Martin Chapman Department of Geosciences Virginia Tech Blacksburg, VA Mmax Workshop Golden, Colorado.
GPS & Seismic Studies of Episodic Tremor & Slip on the Nicoya Peninsula, Costa Rica Timothy H Dixon MARGINS Lecturer February/March 2009.
PLATE MOVEMENT POLLUTES ATMOSPHERE. X BECAUSE IT IS FURTHER EAST & THE EARTH ROTATES FROM WEST TO EAST. PLATE MOVEMENT THEY FIT TOGETHER LIKE A PUZZLE.
Spatial and Temporal Patterns of Deformation Through the Seismic Cycle Jeff Freymueller University of Alaska Fairbanks.
Lecture 6: Earth as a Planet 1.The Young Earth 2.Earth as a planet: interior 3.Plate tectonics 4.Atmosphere.
Plate Puzzle Plate Motions This PPT:
Yan Y. Kagan Dept. Earth and Space Sciences, UCLA, Los Angeles, CA , Statistical.
Class 1. Earth Structure and Plate Tectonics William Wilcock OCEAN/ESS 410.
CEE 437 Lecture 1 October 1, 2002 Thomas Doe. Outline Course Introduction Geology and Engineers Brief History of Geology Global Structure Plate Tectonics.
Remote Earthquake Triggering: (Fault) Failure is Not Always an Option Heather Savage and Emily Brodsky UC Santa Cruz.
Computer Aided Tomography Tomos: cut (Gr.) Extensively used to find 3D structure from surface measurements (X-ray, sound, seismic waves)
Yan Y. Kagan Dept. Earth and Space Sciences, UCLA, Los Angeles, CA , Global.
Seismicity around Lhasa Tsoja Wangmo 1), Norsang Gelsor 1) and Jens Havskov 2) 1) Jiangsu Road No 36 Lhasa, Tibet, PRC 2) University of Bergen, Department.
1 The Hydrologic Cycle Where is the water? The global cycle Groundwater –The myth of underground rivers.
The global seismic energy to moment ratio: a tool for basic research and real-time identification of “Tsunami Earthquakes” Jaime Andres Convers Dr. Andrew.
My objective is: To study the location and characteristics of tectonic activity I  Can describe the global distribution of volcanoes and earthquakes.
An Introduction to Seismic Eruption software and an associated classroom activity Michael Hubenthal, IRIS Educational Specialist.
Andrew V. Newman, Abhijit Ghosh, Amanda Thomas, Grant T. Farmer, Jaime Convers Georgia Institute of Technology, Atlanta, GA, USA Interface Locking: Seismic.
Continental Drift and Plate Tectonics. Global Problems in Geology Distribution of Continents Mid-ocean Ridges Trenches Orogenic Belts Deformation Metamorphism.
Research opportunities using IRIS and other seismic data resources John Taber, Incorporated Research Institutions for Seismology Michael Wysession, Washington.
INTERNAL TECTONIC STRUCTURE OF THE CENTRAL AMERICA WADATI-BENIOFF ZONE BASED ON ANALYSIS OF AFTERSHOCK SEQUENCES Aleš Špičák, Václav Hanuš, Jiří Vaněk.
Using IRIS and other seismic data resources in the classroom John Taber, Incorporated Research Institutions for Seismology.
Earth Science Notes Boundary Types. Plate Boundaries Plate boundaries are found at the edge of the lithospheric plates and are of three types, convergent,
Accessing and using event data in the classroom Michael Hubenthal, IRIS Educational Specialist.
Global seismic tomography and its CIDER applications Adam M. Dziewonski KITP, July 14, 2008.
Slow Slip Events v. Earthquakes Using geodetic data to estimate source parameters.
Andrew V. Newman, Grant. T. Farmer, Abhijit Ghosh, Amanda Thomas, Jaime Convers Georgia Institute of Technology, Atlanta, GA, USA Seismic and Geodetic.
Yan Y. Kagan Dept. Earth and Space Sciences, UCLA, Los Angeles, CA , Evaluation.
Plate Boundaries.
Earthquake size distribution: power-law with exponent ? Yan Y. Kagan Department of Earth and Space Sciences, University of California Los Angeles Abstract.
Chapter 12 Earthquakes.
Assessing the angle of subduction using GeoMapApp
Plate-tectonic analysis of shallow seismicity: Apparent boundary width, beta, corner magnitude, coupled lithosphere thickness, and coupling in 7 tectonic.
Along Strike Variations in Heat Flow 1.Shallow Thermal Structure of the Middle America Trench, Costa Rica Robert Harris, COAS Oregon State University Ingo.
EARTHQUAKE REPORT SOUTH AMERICA WEEK OF JANUARY 27 TH TO FEBRUARY 2 ND, 2016 OLIVIA HELPRIN.
Continental Drift and Plate Tectonics
EARTHQUAKE REPORT SOUTH AMERICA WEEK OF FEBRUARY 3 RD TO FEBRUARY 9 TH, 2016 OLIVIA HELPRIN.
Global Map Scripps Classroom Connection Finding volcanoes on the globe.
Science MONDAY, JAN 26 (A DAY) TUESDAY, JAN 27 (B DAY)
BREVIA Time-Variable Deformation in the New Madrid Seismic Zone Eric Calais 1 and Seth Stein 2 velocities relative to the rigid interior ofNorth Amer-
SEIZE Science Questions and Early Findings What controls the size of earthquakes on subduction thrusts? –What is the role of “asperities” – zones of high.
Earthquakes What are they?. Bellringer   Most of Hawaii’s earthquakes are directly related to volcanic activity and are caused by magma beneath the.
Potential SZO opportunities in Costa Rica Marino Protti Observatorio Vulcanológico y Sismológico de Costa Rica Universidad Nacional - OVSICORI-UNA.
Marino Protti and Víctor González OVSICORI-UNA. Marino Protti and Víctor González OVSICORI-UNA Do we know what’s the largest earthquake that could happen.
2010/11/01 Workshop on "Earthquake Forecast Systems Based on Seismicity of Japan: Toward Constructing Base-line Models of Earthquake Forecasting" Seismicity.
Evidence after wegener: distribution of earthquakes and volcanoes
Earthquakes and Seismic Waves
Motion of Bering Plate? Jeff Freymueller.
Plate Tectonics Movement of the Crust.
South America EQ Report, Week 2
Velocities in ITRF – not appropriate for interpretation
Yan Y. Kagan Dept. Earth, Planetary, and Space Sciences, UCLA, Los Angeles, CA , NEGATIVE.
The State of California: “Earthquake Country”
Earthquakes.
Maximum Earthquake Size for Subduction Zones
Plate Tectonics Evolution of the Earth.
Tip Meckel Ph.D. Candidate Geological Sciences
Tohoku earthquake: A surprise?
Earthquake report south America
SICHUAN EARTHQUAKE May 12, 2008
6.2 Notes Plate Boundaries
Seismic waves 4.6 Recall that seismic waves are generated by earthquakes or explosions 4.9 Recall that seismic waves can be longitudinal (P) waves and.
Notes Over 2.4 Writing an Equation Given the Slope and y-intercept
Types of Plate Boundaries
by Laura M. Wallace, Spahr C
Volcanoes 1 2 Volcanoes will form where the Earth’s structure allows a path for magma from the asthenosphere to rise. Subduction zones Hot spots 1 2.
Earth Science Notes Boundary Types.
by Naoki Uchida, Takeshi Iinuma, Robert M
Strain Release Along the Northern Costa Rica Seismogenic Zone
Presentation transcript:

A. Ghosh, EAS, Georgia Tech Distribution of b-value in the Middle America Trench, near Nicoya Peninsula, Costa Rica Abhijit Ghosh A. V. Newman, A. M. Thomas, G. T. Farmer School of Earth & Atmospheric Sciences Georgia Tech

A. Ghosh, EAS, Georgia Tech Outline of the talk Basics of plate tectonics Why this study is important What is b-value… Data processing and results Discussions Summary

A. Ghosh, EAS, Georgia Tech Plate tectonic map

A. Ghosh, EAS, Georgia Tech Plate boundaries

A. Ghosh, EAS, Georgia Tech Why this study is important Lowman and Montgomery, 1998

A. Ghosh, EAS, Georgia Tech Study area: Middle America Trench

A. Ghosh, EAS, Georgia Tech Earthquake catalog

A. Ghosh, EAS, Georgia Tech Seismic network and earthquake location 1-D global velocity model3-D local velocity model

A. Ghosh, EAS, Georgia Tech What is ‘b-value’… : frequency- magnitude distribution log 10 N = a – b. M M = Magnitude of earthquakes N = number of earthquakes equal or greater than M b = slope of the line a = intercept of the line (seismicity rate)

A. Ghosh, EAS, Georgia Tech b-value in the study area b = 1.29±0.03 a = 6.19±0.1

A. Ghosh, EAS, Georgia Tech Spatial variation of Mc

A. Ghosh, EAS, Georgia Tech Spatial variation of b-value

A. Ghosh, EAS, Georgia Tech b-value error

A. Ghosh, EAS, Georgia Tech Interpretation Norabuena et al., 2004

A. Ghosh, EAS, Georgia Tech Summary b-value varies spatially in the Middle America Trench (MAT), near Nicoya Peninsula Anomalously low b-value zone detected May indicate locked part of MAT Supported by independent geodetic model b-value mapping may be used to identify locked portion of subduction zone

A. Ghosh, EAS, Georgia Tech