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Changesite—(Y), with the chemical formula (Ca8Y)□Fe2+(PO4)7, is a mineral found forming colorless transparent columnar crystals in basalt particles on the Moon. Changesite—(Y) is a member of the merrillite group of phosphate minerals.

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  • Changesita–(Y)
  • Changesite–(Y)
  • Changesite–(Y)
  • Changesite–(Y)
  • Чан'езит-(Y)
  • 嫦娥石
  • 嫦娥石
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  • Changesite—(Y), with the chemical formula (Ca8Y)□Fe2+(PO4)7, is a mineral found forming colorless transparent columnar crystals in basalt particles on the Moon. Changesite—(Y) is a member of the merrillite group of phosphate minerals.
  • 嫦娥石(英語:Changesite-(Y))是一種磷酸鹽礦物,呈柱狀晶體,存在於月球玄武岩顆粒中,是人類在月球上發現的第六種新礦物(前五種包括鎂鐵鈦礦、、、和自然鈰單質),也讓中國成為繼美蘇後第三個在月球發現並命名新物質的國家。 嫦娥石的英文名稱由change(嫦娥的汉语拼音)+s+ite(英文后缀,表示矿物)+ Y(稀土礦物後綴,表示其中富含稀土元素釔)组成,經國際礦物學協會(IMA)新礦物和礦物命名委員會(CNMNC)投票通過,批准号为IMA2022-023a,確認為新礦物。 嫦娥石的理想化学式为(Ca8Y)□Fe2+(PO4)7,晶体结构属三方晶系,空间群R3c。颗粒约2~30微米,呈微小柱状,伴生矿物有、单斜辉石、钛铁矿、长石、、、陨硫铁和玻璃等。
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  • Changesite—(Y), with the chemical formula (Ca8Y)□Fe2+(PO4)7, is a mineral found forming colorless transparent columnar crystals in basalt particles on the Moon. Changesite—(Y) is a member of the merrillite group of phosphate minerals.
  • 嫦娥石(英語:Changesite-(Y))是一種磷酸鹽礦物,呈柱狀晶體,存在於月球玄武岩顆粒中,是人類在月球上發現的第六種新礦物(前五種包括鎂鐵鈦礦、、、和自然鈰單質),也讓中國成為繼美蘇後第三個在月球發現並命名新物質的國家。 嫦娥石的英文名稱由change(嫦娥的汉语拼音)+s+ite(英文后缀,表示矿物)+ Y(稀土礦物後綴,表示其中富含稀土元素釔)组成,經國際礦物學協會(IMA)新礦物和礦物命名委員會(CNMNC)投票通過,批准号为IMA2022-023a,確認為新礦物。 嫦娥石的理想化学式为(Ca8Y)□Fe2+(PO4)7,晶体结构属三方晶系,空间群R3c。颗粒约2~30微米,呈微小柱状,伴生矿物有、单斜辉石、钛铁矿、长石、、、陨硫铁和玻璃等。
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