I am presently working on the evolution of a part of the basement complex rocks in Nigeria. The area is marked by shear zones. My field visits have shown that the shear zones cut across granitic gneisses, pegmatite (extensive and comprises mainly feldspar) and some mica schist. A part of my objectives is to determine the strain (quantitatively) by way of field and laboratory analysis. I need guide and may be peer-reviewed papers that have addressed such case(s). Thank you.

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