Examples of porphyritic

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It should be noted that some 'porphyritic' gabbros evidently formed by disintegration from enclaves of leucogabbro.
The porphyritic granophyre consists of 35-45 % phenocrysts contained within a fine-grained grey-pink matrix.
In porphyritic varieties, this mineral occurs as crystals several centimetres in size in addition to matrix plagioclase.
Andesites are commonly porphyritic and consist of plagioclase, hornblende, and subordinate amounts of clinopyroxene, quartz and biotite phenocrysts.
Both are massive and porphyritic, with euhedral phenocrysts (up to 0.12 cm) of zoned olivine (about 20 %), leucite (about 5 %), and phlogopite (about 2-5 %).
The basalts are generally porphyritic, and phenocryst assemblages show a gradual change from olivine to olivine-clinopyroxene-oxides and olivine-clinopyroxene-plagioclase.
It is a very distinctive hypidiomorphic, coarse-grained porphyritic granite.

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