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  2. Kerogen - Wikipedia

    en.wikipedia.org/wiki/Kerogen

    In these formations, oil and gas are produced directly from the kerogen-rich source rock (i.e. the source rock is also the reservoir rock). Much of the porosity in these shales is found to be hosted within the kerogen, rather than between mineral grains as occurs in conventional reservoir rocks.

  3. Ringwoodite - Wikipedia

    en.wikipedia.org/wiki/Ringwoodite

    Ringwoodite is polymorphous with forsterite, Mg 2 SiO 4, and has a spinel structure.Spinel group minerals crystallize in the isometric system with an octahedral habit. Olivine is most abundant in the upper mantle, above about 410 km (250 mi); the olivine polymorphs wadsleyite and ringwoodite are thought to dominate the transition zone of the mantle, a zone present from about 410 to 660 km

  4. Phosphogypsum - Wikipedia

    en.wikipedia.org/wiki/Phosphogypsum

    Although Chinese phosphogypsum generally contain less toxic heavy metals and radioactive elements [why?] [citation needed], some nevertheless exceed acceptable radioactivity limits for building material, or produce crops with unacceptable amounts of arsenic (As), lead (Pb), cadmium (Cd), or mercury (Hg). Barriers to further use include cost of ...

  5. Kyanite - Wikipedia

    en.wikipedia.org/wiki/Kyanite

    Kyanite's elongated, columnar crystals are usually a good first indication of the mineral, as well as its color (when the specimen is blue). Associated minerals are useful as well, especially the presence of the polymorphs of staurolite, which occurs frequently with kyanite. However, the most useful characteristic in identifying kyanite is its ...

  6. Anorthosite - Wikipedia

    en.wikipedia.org/wiki/Anorthosite

    The mafic mineral in Proterozoic anorthosite may be clinopyroxene, orthopyroxene, olivine, or, more rarely, amphibole. Oxides, such as magnetite or ilmenite, are also common. Most anorthosite plutons are very coarse grained; that is, the individual plagioclase crystals and the accompanying mafic mineral are more than a few centimetres long ...

  7. Provenance (geology) - Wikipedia

    en.wikipedia.org/wiki/Provenance_(geology)

    The transportation process breaks rocks into smaller particles by physical abrasion, from big boulder size into sand or even clay size. At the same time minerals within the sediment can also be changed chemically. Only minerals that are more resistant to chemical weathering can survive (e.g. ultrastable minerals zircon, tourmaline and rutile ...

  8. Mining industry of China - Wikipedia

    en.wikipedia.org/wiki/Mining_industry_of_China

    Taken as a whole, China's economy and exports do not rely on the mining industry, but the industry is critical to various subnational Chinese governments. Mining is extensively regulated in China and involves numerous regulatory bodies. The Chinese state owns all mineral rights, regardless of the ownership of the land on which the minerals are ...

  9. Apatite - Wikipedia

    en.wikipedia.org/wiki/Apatite

    Apatite is the defining mineral for 5 on the Mohs scale. [11] It can be distinguished in the field from beryl and tourmaline by its relative softness. It is often fluorescent under ultraviolet light. [12] Apatite is one of a few minerals produced and used by biological micro-environmental systems. [7]