Problem 51
Question
Rock faults are ruptures along which opposite faces of rock have slid past each other. In Fig. \(3-35\), points \(A\) and \(B\) coincided before the rock in the foreground slid down to the right. The net displacement \(\overrightarrow{A B}\) is along the plane of the fault. The horizontal component of \(\overrightarrow{A B}\) is the strike-slip \(A C\). The component of \(\overrightarrow{A B}\) that is directed down the plane of the fault is the dip-slip \(A D\). (a) What is the magnitude of the net displacement \(\overrightarrow{A B}\) if the strike-slip is \(22.0 \mathrm{~m}\) and the dip- slip is \(17.0 \mathrm{~m} ?\) (b) If the plane of the fault is inclined at angle \(\phi=52.0^{\circ}\) to the horizontal, what is the vertical component of \(\overrightarrow{A B}\) ?
Step-by-Step Solution
VerifiedKey Concepts
Fault Rupture
These slips can be calculated in various ways, resulting in different types of measurable components like the strike-slip and the dip-slip. The strike-slip refers to horizontal movements, while dip-slip pertains to vertical displacements. Understanding these components is crucial to measure the total displacement accurately.
Net Displacement
It considers both the strike-slip and dip-slip components, which are perpendicular to each other. To find out the net displacement vector, you combine these two components using vector addition.
- Net displacement directly relates to understanding the forces and energy released during an earthquake.
- It gives geologists insights into the dynamics of crustal movements.
Pythagorean Theorem
The theorem states that in a right triangle, the square of the length of the hypotenuse (the side opposite the right angle) is equal to the sum of the squares of the lengths of the other two sides: \[c^2 = a^2 + b^2\]
In the context of this problem, the theorem helps us find the magnitude of the net displacement \(|\overrightarrow{A B}|\) by treating the strike-slip and dip-slip as perpendicular sides of a right triangle.
- It simplifies calculating distances and movements in 2D and 3D spaces.
- Essential for converting component vectors into a single resultant vector.
Vertical Component
In this exercise, the vertical component is calculated using the dip-slip and the sine of the inclination angle. This calculation gives insight into how much of the slip is vertical as opposed to horizontal.
- Vertical component = Dip-slip \(\times \sin(\phi)\).
- Important for assessing the lifting or sinking of earth materials during faulting.