The bulk modulus \( K \) is defined by the formula:
\[ K = \frac{\Delta P}{\frac{\Delta V}{V}} \]
Where:
Given:
The change in volume \( \Delta V \) is calculated as:
\[ \Delta V = V' - V = 3.9 \, \text{cm}^3 - 4.0 \, \text{cm}^3 = -0.1 \, \text{cm}^3 \]
The volumetric strain \( \frac{\Delta V}{V} \) is calculated as:
\[ \frac{\Delta V}{V} = \frac{-0.1 \, \text{cm}^3}{4.0 \, \text{cm}^3} = -0.025 \]
Now, we can calculate the bulk modulus \( K \) by substituting the values into the formula:
\[ K = \frac{5 \times 10^4 \, \text{N/m}^2}{-0.025} = 2 \times 10^6 \, \text{N/m}^2 \]
The bulk modulus of the rock is: 2 × 106 N/m2.
In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is _.
The units A to H marked on the figure represent different rock formations. Select the option that describes the chronological sequence from old to young.
Consider two intersecting, north-easterly striking and south-easterly dipping dikes Y1 and Y2, which are exposed on an east-west trending vertical wall of a granite (X) quarry as shown below.
The angle that the dikes make with the horizontal on the quarry wall is