Neolith

NaFe3+[Si2O6]

[Chemical composition] Usually NaFe3+Ca(Mg, Fe2+) is substituted to form neonite, which can be regarded as an intermediate product between neon and ordinary pyroxene.

[crystal structure] monoclinic system,
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Pure neon a0=0.966 nm, b0=0.8780 nm, c0=0.529 nm; β=107°42′; Z=4.

[Form] Crystals are often needle-like, columnar, and more monomorphic (see Figures G-30, G-31).

Picture 26

Figure G-30 neolithic crystal

((a) quoted from Pan Zhaoyu et al., 1993, (b), (c) according to Zhao Shanrong, Wang Wenkui, produced in the Kuiqi rock mass cave in Fujian, 1990) Oblique column: {110}, {111}, { 461},{

Figure G-31 The neon crystal is columnar, column mask vertical

[Physical properties] Dark green; streaks are colorless; glass luster. The cleavage {110} is complete with an angle of 87°. The hardness is 6, and the relative density is 3.55 to 3.60.

[genesis and occurrence] is the main rock-forming mineral of alkaline magmatic rock.

[identification characteristics] are characterized by green, long columnar crystal form, cleavage and alkaline rock occurrence.

[Main use] Only mineralogical and petrological.

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