Skip to content
معدن قاتم
EntityQ764372· pop 30· linked from 813 articles

معدن قاتم

Sign in to save

Also known as mafic

thumbnail|Basalt Mafic is a term used in geology to describe silicate minerals, magmas, and igneous rocks that are rich in magnesium and iron, while being relatively low in silica content. Most mafic minerals are dark in color, and common rock-forming mafic minerals include olivine, pyroxene, amphibole, and biotite. Common mafic rocks include basalt, diabase and gabbro. Mafic rocks often also contain calcium-rich varieties of plagioclase feldspar. Mafic materials can also be described as ferromagnesian.

Wikidata facts

Named after
iron
Image
Anthophyllite Suède Fond.jpg
Show 3 more facts
Commons category
Mafic
characteristic of
mafic mineral
opposite of
felsicity
Sources (2)

via Wikidata · CC0

Article · العربية

الصخر المافي أو المعدن القاتم هو صخر ناري كثيف داكن اللون، يحتوي أساسيا على المغنسيوم والحديد وفقير نسبياً في السيليكون تتراوح نسبة السيليكا SiO2 بين 45% و 25%.والاسم مافي هو اختصار لكلمتي مغنسيوم (بالإنجليزية: Magnesium)‏ وحديد (بالإنجليزية: Ferrum)‏.

Abstract from DBpedia / Wikipedia · CC BY-SA

Gallery (8)