Sensitivity study of TEM data at La Bajada Fault Tobyn W. VanVeghten University of Missouri-Rolla July 11, 2004.

Slides:

Advertisements

Similar presentations

Nye data – nye muligheder? Esben Auken, Anders V. Christiansen, Nikolaj Foged and Kurt Sørensen HydroGeophysics Group Department of Earth Sciences, University.

Advertisements

Arbejdsgruppemøde - SkyTEM processering Esben Auken and Nikolaj Foged HydroGeophysics Group Department of Earth Sciences, University of Aarhus, Denmark.

Filtrering og LCI inversion Esben Auken HydroGeophysics Group Department of Earth Sciences, University of Aarhus, Denmark

Top left is avg Ch for 09Z during June Top right is same but using MYJSFC from WRFv3.0 Bottom left is same but using MYJSFC from WRFv3.1 Bottom right.

Large Scale Mapping of Groundwater Resources Using a Highly Integrated Set of Tools Verner H. Søndergaard Geological Survey of Denmark and Greenland, Denmark.

CSIR-NGRI, Aarhus University, CGWB Mapping groundwater resources in India – a pilot project covering six areas and more than 3000 km 2 of land.

Imaging a Fault with Magnetotellurics By Peter Winther.

Relative Dating The Law of Superposition

Continuous School Improvement Final Presentation School Name Date.

Nyeste erfaringer med processering af SkyTEM data Esben Auken GeoFysikSamarbejdet Geologisk Institut, Aarhus Universitet.

Airborne Resistivity Mapping with Helicopter TEM: An Oil Sands Case Study S. Walker and J. Rudd, Aeroquest International Ltd. KEGS Symposium: Geophysical.

Nancy Helen Natek The University of New Mexico SAGE 2001

Sensitivity kernels for finite-frequency signals: Applications in migration velocity updating and tomography Xiao-Bi Xie University of California at Santa.

Incorporation of Magnetic Resonance Sounding data into groundwater models through coupled and joint inversion 8th Annual Meeting of DWRIP 2014 JANUARY.

1 4 th International Symposium on Flood Defence: Managing Flood Risk, Reliability and Vulnerability, Toronto, Ontario, Canada, May 6-8, 2008 J. Chen, J.

Can We Determine Electric Fields and Poynting Fluxes from Vector Magnetograms and Doppler Shifts? by George Fisher, Brian Welsch, and Bill Abbett Space.

Comparison of NLFFF Extrapolations for Chromospheric and Photospheric Magnetograms of AR J. McTiernan SSL/UCB SHINE 2005 Workhsop.

1 EE 616 Computer Aided Analysis of Electronic Networks Lecture 11 Instructor: Dr. J. A. Starzyk, Professor School of EECS Ohio University Athens, OH,

Nikolaj Foged*, A.V. Christiansen**, and Esben Auken* *HydroGeophysics Group, Department of Earth Sciences, Aarhus University, Denmark **Geological Survey.

Workbench følgegruppemøde Esben Auken GeofysikSamarbejdet, Geologisk Institut, Aarhus Universitet.

Integrated planning on hydrogeophysical data on a national scale: From processing, interpretation and storage to visualisation Ingelise Møller, Flemming.

Atmospheric Mercury Deposition to the Great Lakes A Multi-Year Study Supported by the Great Lakes Restoration Initiative Principal Investigator: Dr. Mark.

Measures of Central Tendency Mode Median Mean. The Mode the value or property that occurs most frequently in the data.

Geology 5660/6660 Applied Geophysics 25 Apr 2014 Final Project © A.R. Lowry 2014 Final Project Assignment Due 5:00 pm May 1.

Scientific Method. Independent Variable (IV)  what you change in the experiment  this “change” needs to be measurable  examples  weight  mass  volume.

The Scientific Method. Steps of Scientific Method 1.Observation: notice and describe events or processes 2.Make a question 1.Relate to observation 2.Should.

Labs and write-ups Mrs. Kay. Scientific Law:  something that has been observed so many times by scientists that they are convinced that it will always.

Seismic refraction along a profile across the La Bajada fault Max Moorkamp.

1 Assimilation of EPS tropospheric ozone for air quality forecast B. Sportisse, M. Bocquet, V. Mallet, I. Herlin, JP. Berroir, H. Boisgontier ESA EUMETSAT.

How to extract Neutrino Factory flux from IMD and neutrino elastic scattering? Near Detector Workshop, CERN, 30 July 2011 Paul Soler.

Magnetotelluric Interpretation of La Bajada Canyon Jeremy Gunter SDSU SAGE 2004.

Institutional Discrimination in Marginalised Communities: The Case of People Living with HIV in Nepal By RAM ARYAL.

An E-W gravity profile across the La Bajada fault Zone in the Rio Grande Rift, North Central New Mexico Rajesh Goteti University of Rochester SAGE 2007.

 Content area: Integrated Language Arts  Grade Area: 7-12 Next slide.

Nikolaj Foged, and Esben Auken HydroGeophysics Group, Department of Earth Sciences, Aarhus University, Denmark Coil response inversion in Aarhus Workbench,

+ EXPERIMENTAL INVESTIGATIONS An experimental investigation is one in which a control is identified. The variables are measured in an effort to gather.

The IB Way.  Title  Background Information -enhances the understanding of the investigation and… - demonstrates personal significance, interest or curiosity.

Designing an Experiment. Think of a Question  What do you want to know? (1)  “What is the effect of the____on the _____?”  Change the question into.

REPENTURN July 5, 2015 REPENTURN REPENTURN REPENTURN.

日期：指導老師：林克默博士黃文勇博士學生：郭怡彣 T. Trupke and R. A. Bardos Centre of Excellence for Advanced Silicon Photovoltaics and Photonics, University.

Click me for movie Get a 100% before moving on to next slide Screenshot here.

Step 1 – Melody 2 (synth lead/violin/flute)

WP 4.1 Source Mechanisms and fault dimensions of the

(a) (b) Up-regulated in R Down-regulated in R Up-regulated in S

Comparing AEM with lithological data using a comprehensive database system for geological and downhole geophysical information Esben Auken, Professor HydroGeophysics.

METALLURGICAL PROPERTIES PREDICTION

DIAL: HP PRINTER TECHNICAL SUPPORT. Hp Printer For Technical Error: Visit our site :

قراءة القوائم المالية وفـاء شـريف علي. محلل مالي

Designing a Research Project

Package 2100 Boreholes – Groenholland

تحليل الحساسية Sensitive Analysis.

When is a fit good??? Ulrich Becker 3/4/2009 Repeat from last Mini lecture Fit exercises 1,2, and 2008 Likelihood and goodness of fit.

MagnetoTelluric in combination with seismic data for geothermal exploration A. Manzella1 V. Spichak2 1National Research Council – Institute of Geosciences.

Solar Cell Fabrication Process Comparison

INFLUX: Comparisons of modeled and observed surface energy dynamics over varying urban landscapes in Indianapolis, IN Daniel P. Sarmiento, Kenneth Davis,

بسم الله الرحمن الرحیم.

Designing a Research Project

Observing Forming Hypothesis Testing Hypothesis Analyzing Data

The Laws of Stratigraphy

Converting from Base-n to Base-10

First and Last name homeroom

3 Week A: May 1 – 19 3 Week B: May 22 – June 9

ADVANCES IN MAGNETOTELLURIC STUDY OF GEOTHERMAL AREAS Viacheslav Spichak Geoelectromagnetic Research Center IPE RAS.

Types of Errors And Error Analysis.

This is a timeline of the RDA interest and working groups launched from the beginning through November. At the bottom are the earliest groups, at the top.

Comparison of model estimates of p (the exponent of the contrast response function) across psychophysical and fMRI data. Comparison of model estimates.

Fig. 2 Large-area and high-density assembly of AuNPs.

Building pattern  Complete the following tables and write the rule 

Presentation transcript:

Sensitivity study of TEM data at La Bajada Fault Tobyn W. VanVeghten University of Missouri-Rolla July 11, 2004

Outline Objective Methodology with example 1-D results TEM Cross-section constrained by sensitivity analysis WinGLink EMMA and results from EMMA Conclusion

Objective Sensitivity analysis –Constrain TEM data at Canyon Site Qualitatively in WinGLink Quantitatively using EMMA

Examples of Raw Data

Sensitivity Test

Sensitivity Test Cont’d

Inverse Models with Error Bars

TEM Cross-Section E W

EMMA Electromagnetic Model Analysis (EMMA) Program Developed by the HydroGeophysics Group, University of Aarhus, Denmark 1-D modeling program for most TEM, FDEM, Resistivity, MT, and borehole methods Includes model sensitivity analysis *From Auken, Nebel, Sorensen, Breiner, Pellerin, and Christensen, June 2002

EMMA Screenshot

Example of EMMA Results Earlier Results for Comparison

TEM Cross-Section after EMMA EW

Conclusion Can’t resolve top and bottom resistive layers Change in character between LB600 and LB650 Possible fault here