Subophitic dolerite
A rock subtype
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Subophitic dolerite describes a texture in the igneous rock dolerite where larger plagioclase crystals (laths) are partially enclosed by smaller crystals of clinopyroxene (like augite), but the pyroxene isn't fully surrounding them like in true ophitic texture; it's an intermediate stage showing how magma cooled, often found in the middle of thick intrusions like dykes, indicating slower cooling than fine-grained margins but faster than coarse-grained cores, featuring common minerals like plagioclase, augite, hornblende, and sometimes olivine.
Unique Identifiers
Mindat ID:
498932
Long-form identifier:
mindat:1:1:498932:1
Classification of Subophitic dolerite
Mineralogy of Subophitic dolerite
Essential minerals - these are minerals that are required within the classification of this rock:
| Feldspar > Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Pyroxene | ADSi2O6 |
Internet Links for Subophitic dolerite
mindat.org URL:
https://www.mindat.org/min-498932.html
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References for Subophitic dolerite
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