方铁矿

Also known as wuestite

thumb|Crystal structure of Wüstite

In the Vinony graph

Within Vinony's link graph, 方铁矿 is referenced by 40 other articles, and connects out to Mohs scale of mineral hardness, relative density and iron.

It sits within the topics Cubic minerals, Iron(II) minerals and Minerals described in 1927.

Its subject is documented across 19 Wikipedia language editions.

Key facts

Mineral.name: Wüstite
Mineral.category: Oxide mineral
Mineral.image: Wüstite-110970.jpg
Mineral.imagesize: 260
Mineral.formula: FeO
Mineral.IMAsymbol: Wüs
Mineral.strunz: 4.AB.25
Mineral.color: Greyish white to yellow or brown; colorless in thin section
Mineral.habit: Pyramidic, prismatic
Mineral.system: Cubic
Mineral.class: Hexoctahedral (mm) H–M symbol: (4/m 2/m)
Mineral.symmetry: Fm3m (no. 225)
Mineral.cleavage: {001} perfect
Mineral.fracture: Subconchoidal to rough
Mineral.mohs: 5–5.5
Mineral.refractive: 1.735–2.32 in synthetic crystals
Mineral.pleochroism: None
Mineral.gravity: 5.88

via Wikipedia infobox

Wikidata facts

Has part: iron(II) oxide
Image: Wüstite-110970.jpg

Show 7 more facts

IMA Mineral Symbol: Wüs
crystal system: cubic crystal system
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update): 4.AB.25
Commons category: Wüstite
chemical formula: FeO
Nickel-Strunz 9th edition (updated 2009): 4.AB.25
Strunz 8th edition (series ID, updated): IV/A.04

Sources (2)

via Wikidata · CC0

Article · 中文

方铁矿（Fe1-xO）是一种以氧化亚铁为主的矿物，常见于陨石和天然铁矿中。其色泽灰暗，不透明，常带绿色金属光泽。方铁矿为立方晶体，莫氏硬度为5-5.5，比重大约为5.7到6.0左右。方铁矿是一种常见的非整比化合物，其化学式中x的范围在0.04-0.12之间。方铁矿的英文名称（wüstite）是为了纪念德国金属学家，矿物學家，基尔大学教授，马克斯·普朗克铁研究所公司首任所长，因其首次合成该矿物。方铁矿的特征产地位于德国巴登-符腾堡州斯图加特附近。除此之外，在格陵兰的迪斯科岛和印度的贾里亚也有发现。在一些金伯利岩管的钻石包体以及深海锰结核中也可找到方铁矿。方铁矿的通常出现于强还原性的环境中。

Abstract from DBpedia / Wikipedia · CC BY-SA