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  2. Crystal twinning - Wikipedia

    en.wikipedia.org/wiki/Crystal_twinning

    Twinning, a version of macle, is a form of symmetrical intergrowth between two or more adjacent crystals of the same mineral. It differs from the ordinary random intergrowth of mineral grains in a mineral deposit, because the relative orientations of the two crystal segments show a fixed relationship that is characteristic of the mineral structure.

  3. Microcline - Wikipedia

    en.wikipedia.org/wiki/Microcline

    This combination leads to a grid pattern, hence microcline displays gridiron twinning. Can also display carlsbad twinning, simple twins, or lack twinning altogether. Lamellae in microcline are discontinuous and "pinch and swell". Photomicrograph of thin section of microcline showing crosshatched crystal twinning (in cross polarized light) Cleavage

  4. Plagioclase - Wikipedia

    en.wikipedia.org/wiki/Plagioclase

    Plagioclase displaying cleavage. (unknown scale) In volcanic rocks, fine-grained plagioclase can display a "microlitic" texture of many small crystals. Plagioclase (/ ˈ p l æ dʒ (i) ə ˌ k l eɪ s, ˈ p l eɪ dʒ-,-ˌ k l eɪ z / PLAJ-(ee)-ə-klayss, PLAYJ-, -⁠klayz) [4] is a series of tectosilicate (framework silicate) minerals within the feldspar group.

  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. Thin section - Wikipedia

    en.wikipedia.org/wiki/Thin_section

    An ordinary 30 μm thin section is prepared as described above but the slice of rock is attached to the glass slide using a soluble cement such as Canada balsam (soluble in ethanol) to allow both sides to be worked on. The section is then polished on both sides using a fine diamond paste until it has a thickness in the range of 2–12 μm.

  7. Orthoclase - Wikipedia

    en.wikipedia.org/wiki/Orthoclase

    Orthoclase crystal twinning from the Organ Mountains in New Mexico. Orthoclase is a common constituent of most granites and other felsic igneous rocks and often forms huge crystals and masses in pegmatite. Typically, the pure potassium endmember of orthoclase forms a solid solution with albite, the sodium endmember (NaAlSi 3 O 8), of plagioclase.

  8. Ultramicrotomy - Wikipedia

    en.wikipedia.org/wiki/Ultramicrotomy

    Ultramicrotomy is a method for cutting specimens into extremely thin slices, called ultra-thin sections, that can be studied and documented at different magnifications in a transmission electron microscope (TEM). It is used mostly for biological specimens, but sections of plastics and soft metals can also be prepared.

  9. Talk:Thin section - Wikipedia

    en.wikipedia.org/wiki/Talk:Thin_section

    For the medical use of thin sections, see histology, which includes a detailed description of the preparation of tissue thin sections using a microtome. How widespread is the use of the actual words "thin section" in medicine? It is the commonly used term in mineralogy. Are there any doctors in the house? Jon 12:25, 12 March 2006 (UTC)