Strawperson Design II TA-type array 45 $75K Intermediate band

Slides:



Advertisements
Similar presentations
OBSIP Overview Instrumentation Centers: Lamont-Doherty Earth Observatory A. Barclay, J. Gaherty, M. Tolstoy Scripps Institution of Oceanography J. Babcock,
Advertisements

We know the Earth is broken into 8 major lithospheric plates …. We know these plates move …. We know there are boundaries between the plates …. Now, let’s.
Instrumentation Centers: Lamont-Doherty Earth Observatory A. Barclay, J. Gaherty, M. Tolstoy Scripps Institution of Oceanography J. Babcock, A. Harding,
Continental Drift Theory Plate Tectonics How the crust.
 Earthquake: the shaking of the Earth’s crust caused by a release of energy.  Common cause: movement of the Earth’s plates.
More Stuff About Earthquakes. Faults Any stress on the plates can cause an earthquake if the elastic limit is reached. Each type of stress results in.
Earthquakes An earthquake is the shaking or trembling of the earth caused by the _Sudden_ movement of the earth’s crust. They usually occur where rocks.
Chapter 6 Earthquakes Ch. 6.1 Earthquakes and Plate Tectonics.
Geophysical study of the crust and upper mantle in the Qinghai-Tibet Plateau, China: Broadband seismic observations and tomography imaging of the lithosphere.
From Word Embeddings To Document Distances
Choosing a Dental Plan Student Name
D. Phát triển thương hiệu
NHỮNG VẤN ĐỀ NỔI BẬT CỦA NỀN KINH TẾ VIỆT NAM GIAI ĐOẠN
Nasal Cannula X particulate mask
HF NOISE FILTERS PERFORMANCE
实习总结 (Internship Summary)
Current State of Japanese Economy under Negative Interest Rate and Proposed Remedies Naoyuki Yoshino Dean Asian Development Bank Institute Professor Emeritus,
Front End Electronics for SOI Monolithic Pixel Sensor
Solving Rubik's Cube By: Etai Nativ.
CS284 Paper Presentation Arpad Kovacs
Theoretical Results on Neutrinos
Creating Synthetic Microdata for Higher Educational Use in Japan: Reproduction of Distribution Type based on the Descriptive Statistics Kiyomi Shirakawa.
MOCLA02 Design of a Compact L-­band Transverse Deflecting Cavity with Arbitrary Polarizations for the SACLA Injector Sep. 14th, 2015 H. Maesaka, T. Asaka,
Fuel cell development program for electric vehicle
Overview of TST-2 Experiment
Inter-system biases estimation in multi-GNSS relative positioning with GPS and Galileo Cecile Deprez and Rene Warnant University of Liege, Belgium  
10. predavanje Novac i financijski sustav
Wissenschaftliche Aussprache zur Dissertation
Advisor: Chiuyuan Chen Student: Shao-Chun Lin
Widow Rockfish Assessment
On Robust Neighbor Discovery in Mobile Wireless Networks
Y V =0 a V =V0 x b b V =0 z
Fairness-oriented Scheduling Support for Multicore Systems
Climate-Energy-Policy Interaction
Ch48 Statistics by Chtan FYHSKulai
The ABCD matrix for parabolic reflectors and its application to astigmatism free four-mirror cavities.
Measure Twice and Cut Once: Robust Dynamic Voltage Scaling for FPGAs
Online Learning: An Introduction
The Toroidal Sporadic Source: Understanding Temporal Variations
Howard Wiseman1 and Geoff Pryde1
C3q Measurement Using Polarized e+/e- Beams at JLab
Solar Astronomy with LOFAR - First Steps
Topic 5: Sequences and Series
Free Cooling Application for Energy Savings at Purdue
Topic 1 Applications of Physics
Calibration: more background
Small-Sample Methods for Cluster-Robust Inference in School-Based Experiments James E. Pustejovsky UT Austin Educational Psychology Department Quantitative.
Introduction to Scientific Computing
Gas-Electric Co-Optimization (GECO)
Gil Kalai Einstein Institute of Mathematics
Gravitation and Cosmology I Introduction to Cosmology
Emmanuel Mouche, Marie Alice Harel (LSCE)
Richard Anantua (UC Berkeley)
Wednesday 9/6 Welcome back!
Atmospheric Thermodynamics
Conformational Sampling to Interpret SAXS Profiles
Chapter 3. Data Processing
Summary.
Basic Regression Analysis with Time Series Data
2National Institute of Standards and Technology, Boulder, CO 80305
Chapter 11 Plate Tectonics.
Squeezing the Slab: future directions for metamorphic petrology in the SZO Andrew Smye Sentence about metamorphic petrology and need to link observations.
Compilations of earthquake locations indicate
Archean continental terranes commonly have deep keels, but the whole upper mantle of western North America shows very slow seismic velocities.
Mantle wedge processes
(Fig ).
Mantle wedge processes
Logistics Wine bill ($12 per person, for drinkers)
Cascadia Facility Purpose
The Theory of Plate Tectonics
Presentation transcript:

Strawperson Design II TA-type array 45 OBSs @ $75K Intermediate band + DPG or APG 15 shallow water 30 deep water Redeploy 30 deep Flex-type array 5 OBS @ $75K 30-35 Short-period @ $35 -40K Total $5M

Whole plate Flex array for detailed studies Greater density near trench Multiple deployments Absolute pressure gauges Shallow water - facility for future Deploy first instruments in 2010 near N. ETS site 2 summers for each deployment to study structure Accelerometers at some sites Balance of “broadband” vs shortperiod in flex array?

Strawperson Design TA-type array 45 OBSs @ $75K Intermediate band + DPG or APG 15 shallow water 30 deep water Flex-type array 5 OBS @ $75K 50 Short-period @ $25K or ~ 30 @ $40K Total $5M

Rupke et al., EPSL 2004

Ranero et al., Nature, 2003 Normal faults extend 20 km+ into lithosphere while bending before subduction

Contreras-Reyes et al., G3, 2007

Contreras-Reyes et al., G3, 2007

Contreras-Reyes et al., G3, 2007

Contreras-Reyes et al., GJI, 2008