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  2. Crystal twinning - Wikipedia

    en.wikipedia.org/wiki/Crystal_twinning

    Closely spaced polysynthetic twinning is often observed as striations or fine parallel lines on the crystal face. Cyclic twins are caused by repeated twinning around a rotation axis. This type of twinning occurs around three, four, five, six, or eight-fold axes, the corresponding patterns are called threelings, fourlings, fivelings, sixlings ...

  3. Plagioclase - Wikipedia

    en.wikipedia.org/wiki/Plagioclase

    Plagioclase in hand samples is often identified by its polysynthetic crystal twinning or "record-groove" effect. Plagioclase is a major constituent mineral in Earth's crust and is consequently an important diagnostic tool in petrology for identifying the composition, origin and evolution of igneous rocks.

  4. Ulexite - Wikipedia

    en.wikipedia.org/wiki/Ulexite

    Ulexite displays polysynthetic twinning parallel to the elongation, along {010} and {100} (Murdoch, 1940). [11] In thin sections cut parallel to the fibers, ulexite grains display both length-fast and length-slow orientations in equal quantities because the intermediate axis (y) of the indicatrix is roughly parallel to the elongation of the ...

  5. Albite - Wikipedia

    en.wikipedia.org/wiki/Albite

    Albite is a plagioclase feldspar mineral.It is the sodium endmember of the plagioclase solid solution series. It represents a plagioclase with less than 10% anorthite content. . The pure albite endmember has the formula Na

  6. Spurrite - Wikipedia

    en.wikipedia.org/wiki/Spurrite

    Spurrite is a white, yellow or light blue mineral with monoclinic crystals. Its chemical formula is Ca 5 (Si O 4) 2 CO 3. [5]Spurrite is generally formed in contact metamorphism zones as mafic magmas are intruded into carbonate rocks. [6]

  7. Pressure-temperature-time path - Wikipedia

    en.wikipedia.org/wiki/Pressure-temperature-time_path

    Microcline (cross-hatched twinning) included in magnetite (black, opaque) in plagioclase (polysynthetic twinning). Therefore, the sequence of formation is: microcline → magnetite → plagioclase. Peak porphyroblasts: A garnet-mica schist with porphyroblastic garnet (black) in fine-grained mica matrix: Retrograde (Post-peak) reaction rims

  8. Simmonsite - Wikipedia

    en.wikipedia.org/wiki/Simmonsite

    Simmonsite contains no observable euhedral crystals but it does have complex polysynthetic twinning. Its color is pale buff to cream in the hadn specimens accompanied by a white streak and has a greasy appearance. It exhibits a hardness of 2.5-3 on the Mohs hardness scale. There is no apparent cleavage, a subconchoidal fracture, no parting, and ...

  9. Canasite - Wikipedia

    en.wikipedia.org/wiki/Canasite

    Twinning is usual, and can occur as polysynthetic, which is when multiple twins align in a parallel. [4] It has a barely detectable 1.12% potassium radioactivity based on the GRapi unit (Gamma Ray American Petroleum Institute Units). [5]