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Journal Article
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2015
Overview
Most of the sills described so far in this chapter [Palisades, Shiant, Dillsburg, Elephant's Head dyke, Black Jack, Tasmanian dolerites, Ferrar dolerites] can be said to exhibit certain features in common. They are sills in which crystal settling has probably taken place, although in most cases this is confined to the earliest stages of crystallization and involves minerals, usually olivine, present in the magma at the time of emplacement.
Publisher
Springer
Subject
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