HELP
|
This article needs your attention, for these possible reasons:
- Lacking references
- Too many "red links"
- Cluttery, too scientific, or unable to understand.
Please help us bring this article up standard. Thanks!. The reason given is: No references
|
Macrocrystalline rocks are rocks that have crystals large enough to be seen with the unaided eye.
In igneous rocks[]
Macrocrystalline (or phaneritic) texture is common in intrusive igneous rocks which cooled slowly enough to allow crystal growth.
In sedimentary rocks[]
Expand.
See also[]