玻璃陨石为半透明的玻璃质体,有微弱磁性,颜色为墨绿色、绿色,淡绿色,棕色,褐色,深褐色,还有少见的朱砂色。玻璃陨石是在高空、高温、高压和高速下形成的,通体布满致密的小气泡,外部有融壳,融壳上有流纹,外部和融壳下有时会产生大的气印。玻璃陨石是一种天然玻璃物质。由于外观似黑曜岩,故又称似黑曜岩。
玻陨石,全称玻璃陨石,其是某种石陨石降落过程中融化的液质冷却后的产物。它是一种天然玻璃物质。由于外观似黑曜岩,故又称似黑曜岩。但两者的成分、结构都不同。大多数玻璃陨石的形状与熔融溅射物的形状相似,有球状、细长状、哑铃状、 滴状、钮扣状和不规则的块状等。
玻璃陨石的母石为淡绿色和黑色两种,因此,玻璃陨石的降落都是与母石共同进行的。英国生物学家达尔文1844在澳大利亚获得一块钮扣状玻璃质石块,以后在世界范围内这种类似玻璃质石块通称为“玻璃陨石”。它是一种天
然玻璃物质。由于外观似黑曜岩,故又称似黑曜岩。但两者的成分,结构都不同。大多数玻璃陨石的形
状与熔融溅射物的形状相似,有球状、细长状、哑铃状、液滴状、钮扣状和不规则的块状等。它成群地撒落在上或海底沉积物中。玻璃陨石的颜色有黑、墨绿、棕褐,表层具拉长状气泡及大小不等的气
泡,有的似如日球表面的环形,状冬案,密度约为2.38.3.0。
关于玻璃陨石的成因现已探明,科学家研究表明它是某种石陨石高速陨落时融化后的产物。但对于其形成过程,却还是未知,虽然如今大多数科学家认为是巨大的陨石或彗星(核)撞击地球,使地球表面物质熔融,溅射到空中,急速冷却而成。促使其玻璃陨石研究价值收藏价值极高。
Meteorites are translucent glassy bodies with weak magnetism. Their colors are dark green, green, light green, brown, brown, dark brown, and a rare cinnabar color. Glass meteorites are formed at high altitude, high temperature, high pressure and high speed. The whole body is covered with dense small bubbles, and there are molten shells on the outside. There are flow lines on the molten shells, and sometimes large gas marks are produced on the outside and under the molten shells. Glass meteorite is a kind of natural glass material. Because it looks like obsidian, it is also called obsidian.
Glass meteorite, the full name of glass meteorite, is the product of cooling the melted liquid during the fall of some stone meteorite. It is a natural glass substance. Because it looks like obsidian, it is also called obsidian. But the composition and structure of both are different. The shape of most glass meteorites is similar to that of molten sputtering, such as spherical, slender, dumbbell, drop, button and irregular block.
The parent stones of glass meteorites are light green and black. Therefore, the landing of glass meteorites is carried out together with the parent stones. Darwin, a British biologist, got a button-shaped glass stone in Australia in 1844. Later, this kind of glass-like stone was called "glass meteorite" all over the world. It's a kind of sky.
However, glass material. Because it looks like obsidian, it is also called obsidian. But the composition and structure of both are different. The shape of most glass meteorites
Similar to the shape of molten sputtering, it has spherical shape, slender shape, dumbbell shape, droplet shape, button shape and irregular block shape, etc. It is scattered in groups on the mainland or in seabed sediments. The color of the meteorite is black, dark green and brown, and the surface layer has elongated bubbles and gases of different sizes.
Bubbles, some of which are ring-shaped and winter-shaped like the surface of the heliosphere, have a density of about 2.38.3.0.
The cause of the glass meteorite has been proved, and scientists' research shows that it is the product of melting when some kind of stone meteorite falls at a high speed. However, its formation process is still unknown, although most scientists now believe that it was a huge meteorite or comet (nucleus) that hit the earth, melted the earth's surface material, sputtered it into the air, and cooled it rapidly. It makes the research value of glass meteorites extremely high.
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