編號 99681295

已出售
沒有保留價 綠色, 黃色 黝簾石  - 4.56 ct - 國際寶石學院(International Gemological Institute (IGI)) - Epidote 稀有宝石
最終出價
€ 25
5 小時前

沒有保留價 綠色, 黃色 黝簾石 - 4.56 ct - 國際寶石學院(International Gemological Institute (IGI)) - Epidote 稀有宝石

"IGI Certified Natural Rare Epidote Certificate Number :700597249 Weight -4.56 Carat Color - Yellowish-Green Shape -Oval Cut - Brilliant/Step Dimensions - 13.07 x 11.42 x 4.48mm Transparency - Transparent Treatment -No Indications of heating " The Epidote group includes minerals like Epidote, Clinozoisite, Zoisite, and Piemontite, characterized by their complex silicate structure with calcium, aluminum, and other trivalent metals (Fe, Mn, V). Key members also feature rare-earth elements (Allanite) or substitutions like strontium and lead, forming solid-solution series (e.g., Epidote-(Sr), Hancockite, Mukhinite, Niigataite, Tweddillite) with specific chemical variations, all sharing similar crystal frameworks but differing in cation content, leading to distinct mineral names. Major Members Epidote: The namesake, rich in iron (Fe³⁺), giving it distinct green colors. Clinozoisite: The iron-free, aluminum-rich end-member, chemically similar to epidote but monoclinic. Zoisite: An orthorhombic dimorph of clinozoisite, forming a separate subgroup (e.g., Tanzanite, Thulite). Piemontite: Contains manganese (Mn³⁺), creating vibrant red to violet hues. Allanite: A complex member incorporating rare-earth elements (REEs) like Cerium (Ce). Other Notable Members & Substitutions Hancockite: A lead (Pb) bearing epidote. Mukhinite: Vanadium (V³⁺) rich. Niigataite: Strontium (Sr) rich. Epidote-(Sr): Contains strontium. Piemontite-(Pb/Sr): Lead or Strontium substitutions in piemontite. Key Characteristics Structure: Contain isolated [SiO₄] tetrahedra and [Si₂O₇] double tetrahedra with octahedral chains. Occurrence: Common in metamorphic rocks (low-grade metamorphism) and altered igneous rocks. Color: Varies from green (Epidote) to reddish (Piemontite) to colorless (Clinozoisite). Shipping 1-3 working days by FedEx

編號 99681295

已出售
沒有保留價 綠色, 黃色 黝簾石  - 4.56 ct - 國際寶石學院(International Gemological Institute (IGI)) - Epidote 稀有宝石

沒有保留價 綠色, 黃色 黝簾石 - 4.56 ct - 國際寶石學院(International Gemological Institute (IGI)) - Epidote 稀有宝石

"IGI Certified Natural Rare Epidote
Certificate Number :700597249
Weight -4.56 Carat
Color - Yellowish-Green
Shape -Oval
Cut - Brilliant/Step
Dimensions - 13.07 x 11.42 x 4.48mm
Transparency - Transparent
Treatment -No Indications of heating "

The Epidote group includes minerals like Epidote, Clinozoisite, Zoisite, and Piemontite, characterized by their complex silicate structure with calcium, aluminum, and other trivalent metals (Fe, Mn, V). Key members also feature rare-earth elements (Allanite) or substitutions like strontium and lead, forming solid-solution series (e.g., Epidote-(Sr), Hancockite, Mukhinite, Niigataite, Tweddillite) with specific chemical variations, all sharing similar crystal frameworks but differing in cation content, leading to distinct mineral names.
Major Members
Epidote: The namesake, rich in iron (Fe³⁺), giving it distinct green colors.
Clinozoisite: The iron-free, aluminum-rich end-member, chemically similar to epidote but monoclinic.
Zoisite: An orthorhombic dimorph of clinozoisite, forming a separate subgroup (e.g., Tanzanite, Thulite).
Piemontite: Contains manganese (Mn³⁺), creating vibrant red to violet hues.
Allanite: A complex member incorporating rare-earth elements (REEs) like Cerium (Ce).
Other Notable Members & Substitutions
Hancockite: A lead (Pb) bearing epidote.
Mukhinite: Vanadium (V³⁺) rich.
Niigataite: Strontium (Sr) rich.
Epidote-(Sr): Contains strontium.
Piemontite-(Pb/Sr): Lead or Strontium substitutions in piemontite.
Key Characteristics
Structure: Contain isolated [SiO₄] tetrahedra and [Si₂O₇] double tetrahedra with octahedral chains.
Occurrence: Common in metamorphic rocks (low-grade metamorphism) and altered igneous rocks.
Color: Varies from green (Epidote) to reddish (Piemontite) to colorless (Clinozoisite).


Shipping 1-3 working days by FedEx

最終出價
€ 25
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