<sod>Within the metamorphic belts, pegmatite tends to concentrate around granitic bodies within zones of low mean strain and within zones of extension, for example within the strain shadow of a large rigid granite body. Similarly, pegmatite is often found within the contact zone of granite, transitional with some [[greisen]]s, as a late-stage magmatic-hydrothermal effect of syn-metamorphic granitic magmatism. Some [[skarn]]s associated with granites also tend to host pegmatites.<eod>
<sod>e is often found within the contact zone of granite, transitional with some [[greisen]]s, as a late-stage magmatic-hydrothermal effect of syn-metamorphic granitic magmatism. Some [[skarn]]s associated with granites also tend to host pegmatites.<eod>