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pyroxene |
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pyroxene (pī`rŏksēn), name given to members of a group of widely distributed rock minerals called metasilicates in which magnesium, iron, and calcium, often with aluminum, sodium, lithium, manganese, or zinc occur as X in the chemical formula XSiO3. The pyroxene minerals crystallize in three different systems—orthorhombic, monoclinic, and triclinic—but all have a fundamental prism with angles of 87° to 93° and cleavages parallel to the prism angles. They are commonly white, grayish white, greenish white, greenish black, black, or brown, but other varieties occur. Pyroxene minerals are found chiefly in igneous and metamorphic rocks and in lunar rocks. Varieties include enstatite, bronzite, hypersthene, diopside, wollastonite, augite, pectolite, spodumene, and rhodonite. pyroxeneA group of important rock-forming silicate minerals of variable composition, among which calcium-, magnesium-, and iron-rich varieties predominate. Common pyroxenes belong to either the low-calcium enstatite-(ortho)ferrosilite series, (Mg,Fe)SiO3, or the high-calcium diopside-hedenbergite series, Ca(Mg,Fe)Si2O6. Rare pyroxenes include jadeite, aegirine, and johannsenite. See also enstatite. |
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? Mentioned in | ? References in periodicals archive | ||
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| Even such a minuscule amount could have important effects because pyroxenes make up between 30 and 40 percent of the mantle, says Bell. Results to date indicate that there are indicator minerals (G9 and G10 garnets, ilmenites, pyroxenes and chromites) with chemistry consistent with derivation from the diamond stability field and magnetic anomalies consistent with intrusions of the size and magnetic susceptibilities ranges of kimberlites. Tests carried out for diamond indicator minerals revealed a suite of eclogitic garnets, chrome diopsides, diamond stability field chromites as well as olivine and pyroxenes. |
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