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Sulphide infilled vesicles form numerous zones of disseminated magmatic sulphides within B-zones of thick komatiite lavas.
In some cases the secondary pore space created by feldspar dissolution may be infilled by clay reaction products, or the secondary pore space may be a net contribution to total rock porosity.
Only in places close to outer wall do some small interseptal spaces remain free, not infilled by dilation.
This indurated metamorphic rock and its tectonic fabrics are cut across by several centimetre-scale cracks infilled by undeformed quartzitic matrix.
Still others impose moratoriums on any new development until all established areas are infilled .
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