Chalcedony: Béda antara owahan

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Kaca anyar: {{Infobox mineral | name = Chalcedony | category = Mineral oksida | image = Chalcedony geode.JPG | imagesize = 250 | caption = Batu chalcedony | formul...
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Révisi kala 20 Fèbruari 2018 02.42

Chalcedony /kælˈsɛdəni/ inggih menika satunggaling wujud ingkang sami tumpuk-

Chalcedony
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Batu chalcedony
Umum
KategoriMineral oksida
Rumus kimiaSilika (silikon dioksida, SiO2)
Identifikasi
Massa molekul60 g / mol
Warnamaneka werna
Skala kekerasan Mohs6 - 7
Berat jenis2.59 - 2.61
Referensi[1]

tumpukan.[2] Kuarsa lan moganit

menika kalebet mineral silika, ananging kuarsa menika kagungan perangan trigonal wondene ingkang

moganit menika gadhah sifat ingkang monoklinik. Struktur kimia saking chalcedony inggih menika

SiO2.

Nama chalcedony menika asalipun saking basa Latin chalcedonius (utawi calchedonius).

Istilah menika ingkang kaping sepisan wonten ing satunggaling karyanipun Pliny the Elder,

Naturalis Historia ingkang dipunginakaken kangge nyebat batuan Jaspis ingkang asifat

transparan.Masalah sitiran: </ref> panutup ora ana tumrap tenger <ref> Ananging

istilah khalkedon (χαλκηδών) menika ugi medal wonten ing Book of Revelation.[3]

Geokimia

Struktur

Chalcedony menika nate dipunwastani minangka kriptokristalin kuarsa ingkang gadhah kandhutan

serat[4] ananging

samenika dipunmangertosi bilih chalcedony menika ugi gadhah sifat ingkang polimorf amargi wonten

moganit wonten ing salebeting chalsedony kasebat.[2][5][6] Kadar moganit ing satunggal sampel chalcedony maneka werna, Padatanipun

ing antawisipun 5 dumugi 20 persen.[7]

Kelarutan

Sinaosa gadhah senyawa kimia ingkang memper kaliyan kuarsa, ananging chalcedony menika gadhah sifat

langkung larut tinimbang kaliyan kuarsa wonten ing temperatur ingkang andhap. Bab menika saged amargi

kristal chalcedony menika langkung alus satemah gadhah rasio wiyaring permukaan lan volume ingkang

langkung inggil ingkang dipunprakirakaken amargi wontenipun moganit.[7]

Referensi

  1. Rudolf Duda and Lubos Rejl: Minerals of the World (Arch Cape Press, 1990)
  2. a b Heaney, Peter J., 1994. Structure and Chemistry of the low-pressure silica polymorphs. In: Reviews in Mineralogy v. 29; Silica: Physical Behavior, geochemistry and materials applications. Ed. Heaney, P.J., Prewitt, C.T., Gibbs, G.V., 1-40
  3. James Orr, èd. (1915). "Chalkēdōn". [http://books.google.com/? id=CqPNAAAAMAAJ&pg=PA2859&dq=chalcedony+Chalkedon#v=onepage&q=chalcedony%20Chalkedon&f=false The International Standard Bible Encyclopaedia]. The Howard-Severance company. kc. 2859. {{cite book}}: Check |url= value (pitulung); Missing pipe in: |url= (pitulung); line feed character in |publisher= at position 22 (pitulung); line feed character in |url= at position 26 (pitulung)
  4. Chalcedony mineral information and data. http://www.mindat.org/min-960.html
  5. Origlieri, Marcus. "Moganite: a New Mineral -- Not!" Lithosphere (1994). Aug. 2007 <http://fgms.home.att.net/moganite.htm>.
  6. Nickel, Ernest H., and Monte C. Nichols. "IMA/CNMNC List of Mineral Names." Materials Data. June 2007. Aug. 2007 <http://www.geo.vu.nl/users/ima- cnmmn/MINERALlist.pdf>
  7. a b Heaney, Peter J., and Jeffrey E. Post. "The Widespread Distribution of a Novel Silica Polymorph in Microcrystalline Quartz Varieties." Science ns 255 (1992): 441-443. JSTOR. Aug. 2007. Keyword: moganite

Pranala njawi

Chalcedony locations]