COMPOSITE GROWTH
Combination of syntaxial growth of a mineral species found in the host
rock near the margin and of antitaxial growth of other mineral species NOT
found in the host rock near the vein centre gives rise to a composite
vein. Such growth also found in the pressure shadow regions of
porphyroblastic or porphyroclastic mineral such as garnet or quartz. The
photographh is reproduced after Bons.
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