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Using Data from the Trans-California Seismic Refraction Profile to Illustrate the Utility of Travel-Time Diagrams
Magali BillenU. C. Davis, Dept. of
GeologyCourse: Exploration
Geophysics
http://www.dkimages.com
Exploration Geophysics
• Upper division (juniors/seniors)• Elective course
– No pre-requisites beyond basic math/physics required for geology majors (eeck!!)
• Also serves as elective for engineering students
• Class size varies from 10 - 20 students.
Course Goals• Master basic analysis of several geophysical field methods– Seismic reflection/refraction– Gravity surveying– Resistivity– Electrical methods
• Develop understanding of basic crustal structure & geophysical anomalies– Geometry: size, thickness, depth, shape, magnitude
– Physical origin: density, composition, water
Challenges• Topic is outside my area of research.– Access to interesting/useful data is limited.
• Analysis is formulaic & students get bored or overwhelmed by the multiple steps required.
• Students have highly variable math skills & physics background.
Possible Solution?• Redesign course to focus on a region.
• New, additional goal is to learn something about regional geology & tectonics.– Example: Northern California, from the coast to the Sierras.
• Each technique is taught in the context of learning about some aspect of the subsurface structure for this region.– Example: use seismic refraction data to determine crustal thickness of the Great Valley.
Baby-Steps in Course Re-Design• Step 1: find
appropriate data sets– Search web (seismic data, gravity profiles)
– Search journal articles• Initial analysis were often simple & straightforward
• Step 2: integrate data sets into lectures– Can start by using data as examples.
• Step 3: rewrite homework assignments– apply analysis to regional data sets.
Cost vs. Rewards• Costs: time, lots of time!!• Rewards:
– More interesting for ME!!– More interesting for the students.– More effective at instilling long-term knowledge of when/where methods are useful.
– More effective at developing a deeper knowledge & appreciation of methods & Earth’s structure.
– More exposure to real geologic/tectonic data.
Refraction Seismology Homework
• Data from published paper:– Trans-California Seismic Profile - Pahute Mesa to San Francisco Bay, D. S. Cardier, Anthony Qamar, T. V. Mc Evilly, BSSA, v. 60, p 1829-1846, 1970.
• First homework on refraction seismology.
• Lecture introduced:– Survey geometry.– Seismic wave paths in the sub-surface.
– Travel-time relationship.– Relationships between travel time curve & subsurface structure.
Refraction Seismology Concepts
• Basic data is a travel-time curve (linear).
• Offset vs. arrival time
• Slope is related to layer velocity.– v2 = 1/m2
• Intercept is related to layer thickness.– z = tiv1v2/2(v2
2-v12)1/2
– v1 from slope of direct arrival.
Homework Exercise• Data
– Background explanation about Nevada Test Site as a seismic source.
– Introduction from paper.– Map of stations & source,– Table of station distances & arrival times.
Homework Exercise• Plot Data– Three sets of arrivals: Pn, Pg, P2
– Note haven’t told students what these mean.
• Identify linear arrivals• Determine slopes of
lines and intercepts• Calculate layer velocity
and thickness• Use previous knowledge,
geology books, google to determine what crustal layers these might be.
Results/Student Feed-Back• Positive feedback to having geologic goal.
• Liked learning about NTS seismic sources.• Straight-forward to plot data & get results.
• Some confusion about interpreting data in terms of crustal structure.
• Would like to use this data set again in another assignment... – look at travel-time residuals to get basic info. on non-planar structure.