Structural analysis of the Lower Paleozoic rocks of Western Gaspe, Quebec.

Abdul Hakim. Sikander
The Shickshock Group of Cambrian-Ordovician metavolcanic, and metasedimentary rocks outcropsalong mountains of the same name bounded to the south by the Shickshock Fault. Within these rocks a schistosity S1 and layering are parallel, and there is a lineation L1 marked by a mineral elongation and fine striation. These structures suggest the presence of isoclinal, F 1 folds, and the Shickshock rocks are considered to form the core of a major recumbent F1 fold. The absence...
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