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From your statement it sounds like you are referring to an igneous dyke rather than a sill, however see the following:

A sill is a sheet of intruded magma that forms between to layers of older "country" rock. This is technically described as a "concordant sheet intrusion". If it is later over turned due to tectonic folding it may be vertical but as it was originally emplaced between and parallel to pre-existing rock layers, it is still an igneous sill! However if the intrusion cross cuts the bedding planes of the country rock - known as a discordant intrusion (and was originally (sub)vertical at the time of emplacement) it is known as a dyke.

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