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Geology 5640/6640 Introduction to Seismology 09 Jan 2015 © A.R. Lowry 2015 Read for Mon 12 Jan: S&W 1-28 Last time: Course overview Discussed: syllabus,

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Presentation on theme: "Geology 5640/6640 Introduction to Seismology 09 Jan 2015 © A.R. Lowry 2015 Read for Mon 12 Jan: S&W 1-28 Last time: Course overview Discussed: syllabus,"— Presentation transcript:

1 Geology 5640/6640 Introduction to Seismology 09 Jan 2015 © A.R. Lowry 2015 Read for Mon 12 Jan: S&W 1-28 Last time: Course overview Discussed: syllabus, resources, course objectives The observation: A seismogram is a record of ground motion (specifically, ground acceleration!) as a function of time Animations of vertical movement in EarthScope’s Transportable Array seismic network (for the Feb 2008 Wells, NV and several Gulf of California earthquakes)

2 Trabant et al. (2012) Seismol. Res. Lett. Various Gulf of California earthquakes, 2007-2013

3 What’s the point of showing this? Seismology provides crucial information about the nature of high energy seismic sources like earthquakes!

4 Finite fault model (http://www.geerassociation.org/ GEER_Post%20EQ%20Reports/ Baja%20California_2010/ Baja10_Ch02.html) M7.2 El Mayor- Cucapah Event (2010)…

5 Note however that earthquakes aren’t the only significant seismic energy source on the block!

6 A more familiar application of seismology, for most of you… Would be the application to imaging of the Earth’s subsurface

7 For example, seismic reflection* imaging as it is employed in exploration for petroleum and natural gas…

8 Seismic Reflections * *Sound waves reflect off of points in the subsurface where rock elastic properties change (  change in rock type, porosity, fluid, etc.). Energy returns are “migrated” to the approximate spatial location of the reflection source to form an image of the subsurface.

9 Example of subsurface imaging: thickness of the crust & seismic velocity ratio using P-to-S converted waves from distant earthquakes

10 Example of subsurface imaging: Upper mantle V P, V S and V P /V S ratios from waves from distant earthquakes (Schmandt & Humphreys, EPSL, 2010)


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