Geology Reference
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(a)
(b)
Figure 10.7 (a) Mode 1 (tensile) primary cooling joints in grey diorite marked
out by pink granophyre intruded while both magmas were rheologically in a
fluid-like state (note cuspate contact). (b) Type II shear joint comprising quartz-
pegmatite displacing an earlier sheared quartz vein in deformed granite, Peru.
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