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Material Type: Assignment; Professor: Kattenhorn; Class: Earthquakes and Seismic Hazards; Subject: Geology; University: University of Idaho; Term: Spring 2008;
Typology: Assignments
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Homework Set 4: Focal Mechanism Solutions: Answers
c) Use a table to document the following information for EACH of the six faults. Be sure to use the right- hand rule when determining the fault strike. (24) I. fault strike (in degrees) II. fault dip (in degrees) III. dip direction (compass direction) IV. fault type (if a strike-slip component exists, mention whether left-lateral or right-lateral) Solution A: FAULT: 1 2 Strike 064º 154 / 334º Dip 90º 90º Dip direction NA NA Fault type Strike-slip (left-lateral) Strike-slip (right-lateral) (8) Solution B: FAULT: 1 2 Strike 038º 218º Dip 84º 6º Dip direction SE NW Fault type reverse reverse (8) Solution C: FAULT: 1 2 Strike 110º 320º Dip 42º 40º Dip direction SSW NE Fault type Normal oblique (right-lateral) Normal oblique (left-lateral) (8) d) One of the focal mechanism solutions above represents a major earthquake that happened along the San Andreas fault in California. Determine which of the solutions (A, B, or C) is most likely to represent the California earthquake. EXPLAIN YOUR REASONING!! Then, decide which of the two faults in the solution you selected is the most likely fault that actually produced the earthquake. Again, EXPLAIN YOUR REASONING! (6) Solution A most likely represents the San Andreas fault as this solution shows an earthquake caused by a strike-slip fault and the San Andreas fault is a strike-slip fault. Of the two fault plane solutions in A, the most likely fault that caused the earthquake is fault 2 (strike/dip of 154º/90º) because it is oriented NW/SE and is a right-lateral fault, both of which agree with the characteristics of the San Andreas fault. (6)
(a) Use this information to construct a focal mechanism solution using the double-couple assumption. Shade in the compressional areas. Remember, the two fault planes must divide up the compressional first-arrival quadrants from the dilatational first-arrival quadrants. The easiest way to do this is to figure out where the two lines should intersect the outside of the circle in order to separate the shaded squares from the open circles. Then determine how curved each line needs to be. Remember, any fault plane always intersects the edges of the circle at two points spaced 180º apart. Also, the two fault planes must be mutually perpendicular in 3-D space (try to picture it in your head to see if the two planes your drew obey this requirement). (8) (8) (b) What are the strike, dip, dip direction, and slip sense of each fault that was potentially responsible for this earthquake? (8) FAULT: 1 2 Strike 345º 245º Dip 75º 70º Dip direction ENE NNW Fault type normal oblique (right-lateral) normal oblique (left-lateral) (8) [76]