GEOL4714 Final Exam Fall 2005, C. H. Jones instructor

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GEOL4714 Final Exam Fall 2005 p. 1 GEOL4714 Final Exam Fall 2005, C. H. Jones instructor Name: Student ID #: Feel free to use the back of the sheets for answers needing more space. (1) (10 pts) For each of the possible targets below, list one of the best techniques and one of the worst of those that we used in class: Target Best technique Worst technique Salt water under freshwater Denver Basin thickness Buried pueblo ruin Metal utility pipe Depth to the water table (2) (10 pts) Identify 4 deficiencies (omissions or improper usages) in the fieldbook entry below: October 19 Gravity survey, Boulder County, Colorado Real-time differential kinematic GPS system from UNAVCO used Scribe: Marty Malaprop Reader: Sue Shakey. Reading Latitude Longitude Elevation (m) Base Measurement 4011.122 40.00122 105.4302 2011.1 4011.143 4011.121 4011.163 4011.170 05-011-01 4015.221 40.00223 105.4558 2002.1 4015.200 4015.238 05-011-02 4005.988 40.00388 105.4678 2112.7 4006.198 4006.001

GEOL4714 Final Exam Fall 2005 p. 2 (3) (a; 5 points) Suppose you made a gravity measurement at a spot near some hills, and a developer came and bladed the entire area down to the same elevation as your gravity spot. If you now remeasured gravity at that spot, would it be different? If so, what correction from the first measurement (if any) would the difference be the same as? (b; 5 points) Now suppose you took a measurement in a fire tower and one at the base of the fire tower. The difference between the two measurements would be equivalent to what standard gravity correction (if the second measurement was your local base station)?

GEOL4714 Final Exam Fall 2005 p. 3 (4) (10 pts) Consider the fit to Wenner-array resistivity data shown below. The fit shown is from this model: Layer Thickness (m) Resistivity (ohm-m) 1 2.752692 512 2 9.330057 75 3 infinite 1007 A) Are there alternative models as likely or more likely? If so, how would you find them (what layers would you adjust, and in what manner)? If not, explain why not. B) A refraction profile in the same area places bedrock at a depth of 5 m. Could there be an interface in the resistivity structure consistent with this depth? If so, what resistivity structure would you expect?

GEOL4714 Final Exam Fall 2005 p. 4 (5) (15 pts) Consider the shot gather shown below for a shot 10m from the first geophone. Distances from the shot are listed on the right. A) (5 points) Identify the reflected arrival (mark it clearly) B) (5 points) If you were to conduct a fixed-offset reflection profile seeking to image variations in the depth of the reflector, what offset would you choose and why?

GEOL4714 Final Exam Fall 2005 p. 5 C) (5 points) Estimate the depth of the reflector under the shot. (Hint: there are two pieces of information you need to do this). Show intermediate results clearly.

GEOL4714 Final Exam Fall 2005 p. 6 (6) (15 pts) A GPR profile is acquired in an area with glacial till overlying lake beds. The till contains boulders comparable to and larger than the wavelength of the GPR unit used. A colleague has interpreted these results to indicate that the till extends to a depth of at least 8.5 meters. Do you agree with this interpretation or not? If not, how would you modify the interpretation? Justify your answer.

GEOL4714 Final Exam Fall 2005 p. 7

GEOL4714 Final Exam Fall 2005 p. 8 (7) (10 pts) Below is a plot of arrival times picked for a reversed refraction profile (left is west). What are the apparent velocities of the refracted arrival (second layer) in the forward (west to east) direction reversed direction Which direction (if any) does the base of the top layer dip? Describe a simple geologic scenario that might be consistent with these observations, indicating the basis for this interpretation.

GEOL4714 Final Exam Fall 2005 p. 9 (8) (5 pts) Consider the gravity profile below that was acquired over a sedimentary basin. One possible fit is to use an anomaly 0.2 g/cc less dense than the basement rock 300m thick with vertical walls on the basin margins at 1 and 2.5 km along the profile. Seismic refraction suggests a basin bottom at 100 m depth. Can this be reconciled with the gravity, and if so, how? How would you have to change the gravity model?

GEOL4714 Final Exam Fall 2005 p. 10 (9) (15 pts) New natural gas wells are to be drilled in eastern Boulder County near Louisville. The Louisville area was the site of extensive underground coal mining about 100 years ago to depths of several hundred meters. Records of the old mine workings have been lost or are incomplete. The drilling company wants very much to avoid drilling through any mine workings because hitting a void causes the drilling muds to drain and expensive measures must be undertaken to complete the hole (or it must be abandoned). If the company is hoping to drill holes roughly at the corners of a squares 2 miles on a side, what sort of geophysical survey would you suggest? Keep in mind that reflection surveys are most expensive to conduct, followed by refraction, resistivity sounding, GPR, gravity, and magnetic surveys, which are the cheapest to acquire. Sketch the location(s) of any geophysical surveys on the sketch map.