The geothermal temperature can be calculated using the formula:
\[ T = T_{\text{surface}} + (\text{gradient} \times \text{depth}) \]
Where:
Substitute the given values into the formula:
\[ T = 25^\circ \text{C} + (0.02^\circ \text{C/m} \times 18000 \, \text{m}) \]
Now, calculate the geothermal temperature:
\[ T = 25^\circ \text{C} + 360^\circ \text{C} = 385^\circ \text{C} \]
The temperature at a depth of 18 km is: 385°C (rounded to the nearest integer).
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