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Lamprophyre

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lamprophyre [′lam·prə‚fī·ər]
(petrology)
Any of a group of igneous rocks characterized by a porphyritic texture in which abundant, large crystals of dark-colored minerals appear set in a not visibly crystalline matrix.

Lamprophyre 

melanocratic igneous dike rock that differs from the corresponding igneous rocks to which it is genetically related by its sharply increased content of dark minerals (usually at least 30 percent of the rock). The color of lamprophyre varies from dark gray to black. Its constituents include feldspar (sometimes feldspathoid) and dark minerals (biotite, amphibole, pyroxene, and sometimes olivine). In the porphyritic varieties of lamprophyre the phenocrysts are usually represented by dark minerals—this is called lamprophyric texture. There are calcalkalic lamprophyres (spessartite, kersantite) and alkalic lamprophyres (camptonite, alnöite). Lamprophyres sometimes grade into porphyrites.



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There are a series lamprophyre dykes on ground acquired five years ago by a series of companies but data hasn't been submitted, "so we don't know what was found," says Pace.
Farther north, a swarm of carbonatite and lamprophyre dykes was outlined in the course of mapping the Aigneau Lake area (Fig.
Gold mineralization is hosted in silty carbonate rocks of the Denay Formation associated with altered lamprophyre dikes; and high levels of arsenic, antimony, mercury and thallium.
 
 
 
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