geology, a sill is a tabular plutonthat has intruded between older layers of sedimentary rock, beds of volcanic lavaor tuff, or even along the direction of foliation in metamorphic rock. The term "sill" is synonymous with "concordant intrusive sheet". This means that the sill does not cut across preexisting rocks, in contrast to dikes, which do cut across older rocks.
Sills are always parallel to beds (layers) of the surrounding country rock. Usually they are in a horizontal orientation, although tectonic processes can cause rotation of sills into near vertical orientations. They can be confused with solidified lava flows; however there are several differences between them. Intruded sills will show partial melting and incorporation of the surrounding country rock. On both the "upper" and "lower" contact surfaces of the country rock into which the sill has intruded, evidence of heating will be observed (contact metamorphism). Lava flows will show this evidence only on the lower side of the flow. In addition, lava flows will typically show evidence of vesicles (bubbles) where gases escaped into the
atmosphere. Because sills generally form at depth (up to many kilometers), the pressure of overlying rock prevents this from happening much, if at all. Lava flows will also typically show evidence of weatheringon their upper surface, whereas sills, if still covered by country rock, typically do not.
ultramafic to mafic layered intrusionsare a variety of sill that often contain important oredeposits. Precambrianexamples include the Bushveld, Insizwa, and the Great Dykecomplexes of southern Africa, the Duluth intrusive complex of the Superior District, and the Stillwater igneous complexof the United States. Phanerozoicexamples are usually smaller and include the Rùm peridotitecomplex of Scotlandand the Skaergaard igneous complex of east Greenland. These intrusions often contain concentrations of gold, platinum, chromium, and other rare elements.
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