Real-time Monitoring of Slip Triangles: Tremor Activity –Average envelope seismogram amplitudes in tremor passband –Active Tremor = black triangles Arrows:

Slides:



Advertisements
Similar presentations
Cascadia Ken Creager, Steve Malone, Geoff Abers, Stephane Rondenay, Brad Hacker and Tim Melbourne Earth and Space Sciences University of Washington.
Advertisements

Group Velocity Dispersion Curves from Wigner-Ville Distributions Simon Lloyd 1, Goetz Bokelmann 1, Victor Sucic 2 1 University of Vienna 2 University of.
Subduuction Zone Observatory: Faulting and Deformation Jeff Freymueller Geophysical Institute and Dept. of Geology and Geophysics University of Alaska.
Body and Surface Wave Seismic Tomography for Regional Geothermal Assessment of the Western Great Basin Glenn Biasi 1, Leiph Preston 2, and Ileana Tibuleac.
Lessons we have learned from seismological observations in the Taiwan region Jer-Ming Chiu CERI/Dept. of Earth Sciences University of Memphis March 19,
Subduction Zone Geodynamics:
Seismic tomography Tomography attempts to determine anomalous structures within the Earth as revealed by deviations from “average” seismic properties at.
Spatial and Temporal Patterns of Deformation Through the Seismic Cycle Jeff Freymueller University of Alaska Fairbanks.
“Real-time” Transient Detection Algorithms Dr. Kang Hyeun Ji, Thomas Herring MIT.
Earthquake Predictibility, Forcasting and Early Warning Bill Menke October 18, 2005.
Very-Low-Frequency Earthquakes (VLFE) in SVI and Grid Moment-Tensor Inversion For details on GCMT inversion method, see Ito et al., GJI, 2006.
Observing an Earthquake Cycle Within a Decade
Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip Garry Rogers and Herb Dragert, Science 300, Shaji Nair Earthscope.
2-3 March 2009 Cascadia 2007 and Beyond Workshop, Seattle Results from Strainmeter Recordings of Cascadia “ETS” events Work by Evelyn Roeloffs, Wendy McCausland,
Subduction Fluids Channelled to Forearc Mantle Corner:
The RSNI Seismic Network Laboratory of seismology, DISTAV - University of Genoa (Italy) RSNI STAFF RSNI STAFF : Spallarossa D.,
Earthquakes.
Earthquake Location The basic principles Relocation methods
Locating Earthquakes Earthquake occurs when there is a rupture in the rock or when the strain builds up enough to cause movement along a fault. 3 waves.
Volcanoes and Plate Tectonics
New earthquake category Nature 447, (3 May 2007) | doi: /nature05780; Received 8 December 2006; Accepted 26 March A scaling law for slow.
Tectonic boundaries and hot spots. A useful reference dynamicearth/sitemap.html
Surface wave tomography : 1. dispersion or phase based approaches (part A) Huajian Yao USTC April 19, 2013.
Crust and upper mantle structure of Tien Shan Orogen and its surroundings by ambient noise tomography and earthquake tomography Yong Zheng a, Yingjie Yang.
CHAPTER Plate Tectonics 18
U.S. Department of the Interior U.S. Geological Survey Earthquake Location by Annabel Kelly.
Section 19.2– Seismic Waves and the Earth’s Interior
Episodic Tremor in the Alaska/Aleutian Subduction Zone Chloe Peterson, Douglas Christensen, and Steve McNutt Geophysical Institute, University of Alaska.
Last week’s problems a) Mass excess = 1/2πG × Area under curve 1/2πG = × in kgs 2 m -3 Area under curve = -1.8 ×10-6 x 100 m 2 s -2 So Mass.
Disputable non-DC components of several strong earthquakes Petra Adamová Jan Šílený.
Borehole Strainmeters: Instruments for Measuring Aseismic Deformation in Subduction Zones Evelyn Roeloffs U.S. Geological Survey, Vancouver, WA.
Integrated Coordinated Science End of Year Review.
Large Earthquake Rapid Finite Rupture Model Products Thorne Lay (UCSC) USGS/IRIS/NSF International Workshop on the Utilization of Seismographic Networks.
Formation of the Universe and Earth’s Interior 1.
SPICE Research and Training Workshop III, July 22-28, Kinsale, Ireland Seismic wave Propagation and Imaging in Complex media: a European.
Models for Fault Behavior
The seismogram U = Source * Propagation * Site.
David Schmidt Ray Weldon Reed Burgette Randy Krogstad Haiying Gao
Causes and Effects of Plate Movement
P079: Crustal Structure using the tomography method, in the central part of Itoigawa-Shizuoka Tectonic Line (ISTL). Panayotopoulos Yannis 1, Hirata Naoshi.
2002/05/07ACES Workshop Spatio-temporal slip distribution around the Japanese Islands deduced from Geodetic Data Takeshi Sagiya Geographical Survey Institute.
The theory of plate tectonics states that the lithosphere is divided into 12 large sections (plates) and about 20 smaller ones. These plates ‘float’ on.
Earthquakes. earthquakes Earthquakes are natural vibrations of the ground caused by movement along gigantic fractures in Earth’s crust or by volcanic.
The geometry of a subduction zone. Geometry of subducting slab Syracuse and Abers (2006) Compiled subduction parameters along 33,000 km length of volcanic.
Volcanoes are produced over lithosphere cracks and mantle hot spots. Hot spots are rising plumes of hot mantle magma. As tectonic plates move over the.
Causes and Effects of Plate Movement
Earthquake Notes Warm up:
Susan L. Beck George Zandt Kevin M. Ward Jonathan R. Delph.
Douglas A. Wiens & James Conder
學生: 花翊筑 Alice Hua 指導老師: 陳卉瑄 教授 Kate Huihsuan Chen
Compilations of earthquake locations indicate
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
The Theory of Plate Tectonics
Lithosphere Delamination and Small-Scale Convection Beneath California Imaged with High Resolution Rayleigh Wave Tomography Donald W. Forsyth and Yingjie.
CHAPTER Plate Tectonics 18
1-D Mississippi embayment sediment velocity structure and anisotropy: constraint from ambient noise analysis on a dense array Chunyu,Liu1; Charles A. Langston1.
CERI/Dept. of Earth Sciences
Creager, Wech, Vidale, Melbourne
Archean continental terranes commonly have deep keels, but the whole upper mantle of western North America shows very slow seismic velocities.
Seismic tomography Tomography attempts to determine anomalous structures within the Earth as revealed by deviations from “average” seismic properties at.
8.2 Measuring Earthquakes
Seismic tomography Tomography attempts to determine anomalous structures within the Earth as revealed by deviations from “average” seismic properties at.
The Theory of Plate Tectonics
A numerical scale used to measure the magnitude or energy released
Plate Tectonics Chapter 12.2.
Creager, Wech, Vidale, Melbourne
Creager, Wech, Vidale, Melbourne
Terms/Phrases to Investigate
Ken Creager, Wendy McClausland and Steve Malone
by Satoshi Ide, Annemarie Baltay, and Gregory C. Beroza
Presentation transcript:

Real-time Monitoring of Slip Triangles: Tremor Activity –Average envelope seismogram amplitudes in tremor passband –Active Tremor = black triangles Arrows: GPS Short-term Velocity –50-day GPS site velocities after long-term velocity is removed –Slow Slip = large arrows pointing towards trench

January-February 2007

June-July-August 2007

April-May-June 2008

NVT Location Approach Filtered envelope waveforms STA/LTA to find NVT bursts Pick relative times of good S/N arrivals –By hand and/or automated 1D inversion for locations Analyze for patterns in space and time

NVT Migration in Southern Cascadia : Hand-picked vs. Automated

NVT Migration Along All of Cascadia (Automated) Still preliminary, but find long migrating episodes that overlap in time despite being separated by >100 km Three events are more interrelated along- strike than all events in previous few years

NVT Locations So Far Still plenty of work for us to do in the northern half Beginning to see a persistent gap at OR-CA border NVT band primarily between km slab contours Matches some aspects of slab curvature

Integrating ETS with Earth Structure and Geology ETS Periodicity Surface Wave Crust Structure Body Wave Mantle Structure Brudzinski & Allen, 2007 Arc volcanism Schmidt et al., 2008