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A xenolith (Ancient Greek: "foreign rock") is a rock fragment which becomes enveloped in Xenoliths may be engulfed along the margins of a magma chamber, torn loose from the walls. — “Xenolith - Wikipedia, the free encyclopedia”, en.wikipedia.org
The mineral assemblage is greater than 90% olivine, with minor amounts of other minerals found in the lowermost parts of ophiolites, alpine peridotite massifs, and xenoliths. — “Dunite - Wikipedia, the free encyclopedia”, en.wikipedia.org
Among the xenoliths there are igneous inclusions genetically related to basalts. Several other igneous xenoliths are also related to the upper mantle. — “Szentbékkálla - Wikipedia, the free encyclopedia”, en.wikipedia.org