yes, that is not a bad thing to do. But how do u understand the discontinuities from the map itself, just by looking at the dip directions and relative dip amounts ?
Can you tell me the steps to interpret a map? i can more or less understand the topography, then identify the litho units. The main problem i have is with the discontinuity surfaces. Even if i am able to identify them, i cannot get the details of the surfaces.
I wanted to know a bit more... actually i read about a cycle somewhere which goes like this... high temperature > low viscosity > faster convection > higher heat flow > low temperature > high viscosity > slower convection > slower heat flow > high temperature. How could this be related to the...