GEOPHYSICS (GEOL 4433)

EXAM 1- FALL 1998

YOUR BIG SEISMIC REFRACTION ADVENTURE

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It is the year 2025 and you have finally completed your Master’s Degree in Geology (we knew you could do it! Congratulations!). President Chelsea Clinton has declared that it's about time we explore the crustal structure of the ocean basins. You receive a phone call from the President informing you that she wants you to be the Chief Scientist on a cruise to the middle of the Pacific Ocean to discover the nature of Earth's internal layers there.

Initially, you panic because you know nothing about the Pacific Ocean, except that there is a lot of water there. However, you quickly come to your senses and recognize what a unique opportunity is being offered to you. Furthermore, you have taken GEOL 4433 four times and feel that you are sufficiently well-versed in the Principles of Geophysics to do a good job, so you accept your President’s offer.

Your first task is to familiarize yourself with the Pacific Basin and review what is presently known regarding its geologic history. To do this, you visit a number of World-Wide Web locations containing information on the Oceans. Among the more useful sites, you find:

http://www.ngdc.noaa.gov/mgg/global/seltopo.html

http://www.soest.hawaii.edu/

http://www2.ocean.washington.edu/

After several years of training and a 1-month journey to the center of the Pacific Basin, you are finally on station and ready to begin your study. The first order of business is to design and execute a seismic refraction survey along a 100 km track in order to gain some knowledge of the seafloor and its layered structure. To do this, you place a receiver array aboard one of the ships in your expedition. This vessel remains on station at your starting point throughout the survey. The boat you are on will serve as the source for seismic impulses, and is ordered to steam due west from the starting point for 100 km. Every kilometer along this track, an explosive charge is detonated and the resulting p-waves recorded by the receiver ship. The table at the bottom of the page represents the results of your survey listing offset distance (in meters) and time of first-arriving p-waves (in seconds) for each offset position.

As a result of this survey, you should:

1) Provide a plot of arrival times vs. distance (source-receiver offset).

2) Determine the number of layers in the Pacific Basin subsurface.

3) Determine the velocity of p-waves traveling through the Pacific Basin subsurface layers.

4) Determine the thickness of the Pacific Basin subsurface layers.

5) Determine the critical angles of refraction for each refractor.

6) Provide a summary SCALE diagram of the Pacific Basin crustal structure indicating the number of layers revealed by the refraction survey, the thickness of each layer, the p-wave velocity for each layer, the critical angle of incidence for each refractor, and for deeper refractors, the angles of incidence and refraction in overlying layers which yield critical refraction on the deeper interface.

7) Finally, speculate on the nature and composition of the Pacific Ocean layers (i.e. what specific type of geologic material is it?). I suspect you will need to visit our library for some insight on this.

OFFSET TIME
0 0.000
1000 0.357
2000 0.714
3000 1.071
4000 1.384
5000 1.593
6000 1.801
7000 1.971
8000 2.116
9000 2.261
10000 2.406
11000 2.551
12000 2.696
13000 2.841
14000 2.986
15000 3.131
16000 3.276
17000 3.421
18000 3.566
19000 3.711
20000 3.855
21000 4.000
22000 4.145
23000 4.290
24000 4.435
25000 4.580
26000 4.725
27000 4.870
28000 5.015
29000 5.160
30000 5.305
31000 5.450
32000 5.595
33000 5.740
34000 5.884
35000 6.029
36000 6.174
37000 6.319
38000 6.464
39000 6.609
40000 6.754
41000 6.899
42000 7.044
43000 7.189
44000 7.334
45000 7.479
46000 7.624
47000 7.769
48000 7.913
49000 8.058
50000 8.203
51000 8.335
52000 8.468
53000 8.600
54000 8.733
55000 8.865
56000 8.998
57000 9.130
58000 9.262
59000 9.395
60000 9.527
61000 9.660
62000 9.792
63000 9.925
64000 10.057
65000 10.190
66000 10.322
67000 10.454
68000 10.587
69000 10.719
70000 10.852
71000 10.984
72000 11.117
73000 11.249
74000 11.382
75000 11.514
76000 11.647
77000 11.779
78000 11.911
79000 12.044
80000 12.176
81000 12.309
82000 12.441
83000 12.574
84000 12.706
85000 12.839
86000 12.971
87000 13.103
88000 13.236
89000 13.368
90000 13.501
91000 13.633
92000 13.766
93000 13.898
94000 14.031
95000 14.163
96000 14.296
97000 14.428
98000 14.560
99000 14.693
100000 14.825

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