I think with some paper discuss about thin sections are an essential tool for studying mineral recrystallization caused by earthquakes. They provide detailed insights into the microstructural and mineralogical changes that occur due to heat and pressure, helping scientists understand the dynamics of fault zones and earthquake processes.
The classical universal rotary table (after Sander) can determine the microdynamics as to its 3D direction and size and enable us to correlate it with field-based 3-D macrostructural measure up to the satelite image. From satellite to ground truthing under the polarizing/petrographic microscope.
Not a very easy task indeed but can be very successfully applied ny petrographers, structural geologists, mineralogists. Can also be used as pre-stage to tomography
HGD
There is information on the issue you are investigating on my page.
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