我国3种绿色图章石中白云母的矿物学特征

陈涛; 韩文; 李甜; 皱倩

doi:10.3799/dqkx.2012.106

Volume 37 Issue 5

Sep. 2012

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Article Navigation > Earth Science > 2012 > 37(5): 981-988

CHEN Tao, HAN Wen, LI Tian, Zhou Qian, 2012. Mineralogy Characterization of Muscovite in Three Kinds of Green Sealed Stones from China. Earth Science, 37(5): 981-988. doi: 10.3799/dqkx.2012.106

Citation:

CHEN Tao, HAN Wen, LI Tian, Zhou Qian, 2012. Mineralogy Characterization of Muscovite in Three Kinds of Green Sealed Stones from China. Earth Science, 37(5): 981-988. doi: 10.3799/dqkx.2012.106

CHEN Tao, HAN Wen, LI Tian, Zhou Qian, 2012. Mineralogy Characterization of Muscovite in Three Kinds of Green Sealed Stones from China. Earth Science, 37(5): 981-988. doi: 10.3799/dqkx.2012.106

Citation:

CHEN Tao, HAN Wen, LI Tian, Zhou Qian, 2012. Mineralogy Characterization of Muscovite in Three Kinds of Green Sealed Stones from China. Earth Science, 37(5): 981-988. doi: 10.3799/dqkx.2012.106

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Mineralogy Characterization of Muscovite in Three Kinds of Green Sealed Stones from China

doi: 10.3799/dqkx.2012.106

CHEN Tao^{1, 2
,},
HAN Wen¹,
LI Tian¹,
Zhou Qian¹

1.
Gemology Institute, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-01-16
Available Online: 2021-11-10
Publish Date: 2012-09-15

Abstract

Abstract

Three kinds of seal stones from China, namely, Shan PaoLv (SPL) seal stone in Qingtian, Yue WeiLv (YWL) seal stone in Shoushan and newly found Xi AnLv (XAL) seal stone have been studied by X-ray diffractometer, electronic microprobe analyses, environmental scanning electron microscope, and energy dispersive spectroscopy to obtain their mineral composition, chemical composition, micro-morphology characterization, and cause of color formation. It has been found that the green parts in these three seal stones are dio-octahedral 2M₁ muscovites and they belong to mica-seal stone. As to minor mineral compositions, they are dolomite, pyrite and apatite in SPL; it is kaolinite in YWL, and it is dolomite in XAL, which can provide some information for their respective places of origin. Micro-morphology characterization of the three kinds of muscovites indicate crystallization of muscovite in XAL is better than that in YWL, and the crystal shape of muscovite in SPL is not good because it has undergone hydrothermal alteration. On the other hand, chemical analyses of impurity ions in octahedral sheet have been studied in order to discuss color causing factors of green muscovite which suggests that green color in YWL and XAL are caused by Fe³⁺ and Ti⁴⁺ while green color in SPL is caused by Cr³⁺ in company with Fe³⁺ and Ti⁴⁺.
- muscovite,
- crystal structure,
- color causing,
- seal stone,
- mineralogy

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Mineralogy Characterization of Muscovite in Three Kinds of Green Sealed Stones from China

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