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Difference between revisions of "Igneous intrusive layer"

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[[ru:Igneous intrusive layer]]

Revision as of 19:00, 23 October 2018

This article is about the current version of DF.
Note that some content may still need to be updated.

Igneous intrusive stone layers can consist of granite, diorite, or gabbro, all of which typically contain gold and tetrahedrite.

Gabbro can also contain garnierite (the ore of nickel), kimberlite (which may contain diamonds), and olivine (which may contain native platinum). Granite can contain cassiterite (the ore of tin), bismuthinite (the ore of bismuth), and galena (the ore of lead, plus a 50% chance of silver).

Igneous intrusive layers

Stone found in igneous intrusive layers

Stone appearing in both igneous intrusive and igneous extrusive layers

Gems found in igneous intrusive layers

Gems appearing in both igneous intrusive and igneous extrusive layers

* See also: stone found everywhere

In the real world

Igneous intrusive stone is formed by magma solidification occurring below the surface, as opposed to igneous extrusive stone which forms above the surface of the earth.

Sedimentary
Igneous
Intrusive
Extrusive
Metamorphic
Ore
Economic
Other