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  "documentTitle": "Snow Lake Resources | FWP Presentation Deck | 46 slides",
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      "text": "Geological diagram showing pegmatite dykes, faults, and parental granite zonation.",
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      "text": "Lithium pegmatite dykes account for about one-fourth of the world's lithium production and are a distinct class of mineral deposits. Pegmatite dykes are late stage igneous rocks characterized by distinctive textures and massive crystals. Pegmatites tend to be intruded into shallow crustal depths along anisotropies such as faults, fractures, foliation, and bedding.",
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      "text": "Pegmatites do not form in isolation: they typically occur as members of larger populations of cogenetic bodies. At the district scale, pegmatites typically display mineralogical and geochemical zonation. The lithium enriched Thompson Brothers (TB) and Sherritt Gordon (SG) pegmatite dyke clusters occur on either side of the Crowduck Bay Fault.",
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