2017년 1월 25일 수요일

コマチアイト

コマチアイト

コマチアイト
Volcanic rock
KomatiiteCanada 682By512.jpg
コマチアイト of the Canadian shield, size 9cm
A project: Earth science /Portal: Earth science

A kind of the volcanic rock where it is thought that コマチアイト (British: komatiite[1]) comes from a quality of super pain iron mantle.

The name comes from the South African Komachi River.

Table of contents

Property, the that it features it

Magnesium is high more than 18% and is different from the kimberlite which is rich in potassium others because the ingredient of silica and others has few characteristics. Rocks of the Archeozoic era are often found and receive metamorphism. It is 1,600 degrees Celsius, and the melting point of this magma is higher than basalt, and it is estimated that the earth at the time was a high temperature more.

I am distributed between two kinds in having aluminum or not. This depends on partial molten degree in the mantle inside.

Chemical composition
Ingredient コマチアイト [2]
SiO2 45.8
TiO2 0.30
Al2O3 7.30
Cr2O3 0.20
Fe2O3
FeO 11.2
MnO
MgO 26.1
CaO 7.60
Na2O 0.70
K2O 0.10
P2O5
The total 99.3

Fluidity got into the crack remarkably, and the コマチアイト lava did not create the warm sedimentation layer. But deposit value is high in Australia, Canada, South Africa, a Guyanese shield to have possibilities to have thickness of 500m into a sill form, and to be full of nickel, cobalt, money.

Footnote

[Help]
  1. For ^ Geological Society of Japan "geology vocabulary - Japanese and English, English and Japanese" Kyoritsu publication, 2,004 years, it is page 328. ISBN 4-320-04643-9
  2. It is page 631 for Maruzen, 2,007 years in ^ National Astronomical Observatory "chemical composition "science chronological table 2008" of the main igneous rock". ISBN 978-4-621-07902-7

References

Allied item

Outside link

This article is taken from the Japanese Wikipedia コマチアイト

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