Gupeiite Body in the Siberian Taiga (the Zone of Passage of the Tunguska Meteorite and the Vitim Bollid)

N. Savva, P. Minyuk, T. V. Subbotnikova
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引用次数: 1

Abstract

Many years have passed since the two cosmic bodies of the Tunguska meteorite and the Vitim bollid fell to Earth, but so far the substance of these bodies has not been found on Earth. Therefore, each metal body found on the territory of their passage is of particular interest. The body of iron silicide weighing 12 kg was studied, which was accidentally discovered by a hunter of the village of Kyker in the Siberian taiga on the right bank of the Nercha River, Tungokochensky district, Trans-Baikal Territory. Coordinates of the place of discovery are: 53˚19'N lat, 116˚19'E long. The territory is located in the zone of the passage of the Tunguska meteorite and the Vitim bollid, 25 km from the hunting village of Green Lake. The body is named “Ilekta” after the nearest stream flowing into the Nercha River. The composition and magnetic properties of the exotic find have been determined. It is established that its main mass is composed of iron silicide, gupesiite Fe3Si (zussite?) and contains inclusions of needle-like rhabdite. On the surface, the body is covered with a melting crust, with signs of boiling, a bubbly structure and a film of clay minerals of terrestrial origin. In the molten porous crust, eutec-tic-schreibersite-gupeiite is observed, and rare titanium carbide crystals are also noted. The magnetic susceptibility of the samples is not uniform (286.6 -461.8 10-6E-06 m 3 /kg). It is assumed that a drop of melt separated from the flying space body, and experienced overheating and boiling of the surface layer in the dense layers of the atmosphere.
西伯利亚针叶林中的古佩岩体(通古斯陨石与受害者波利德的穿越带)
通古斯陨石和“受害者”陨石这两个宇宙天体落到地球上已经很多年了,但到目前为止,还没有在地球上发现它们的物质。因此,在它们经过的地方发现的每一个金属体都是特别有趣的。研究人员研究了重达12公斤的硅化铁,它是由一名猎人偶然发现的,该猎人位于外贝加尔湖地区通古科钦斯基地区涅尔恰河右岸西伯利亚针叶林中的Kyker村。发现地点坐标为:北纬53˚19,东经116˚19。该领土位于通古斯陨石和受害者波利德通道的区域,距离格林湖狩猎村25公里。这具尸体被命名为“Ilekta”,以最近的一条流入尼尔恰河的小溪命名。这一奇异发现的成分和磁性能已被测定。确定了其主要质量为硅化铁、铁长石Fe3Si (zussite?),内含针状横纹石。从表面上看,它的身体被一层融化的地壳所覆盖,有沸腾的迹象,有气泡结构,还有一层来自陆地的粘土矿物。在熔融多孔壳中,观察到共晶晶-晶氏体-古贝岩,并观察到罕见的碳化钛晶体。样品的磁化率不均匀(286.6 -461.8 10-6E-06 m 3 /kg)。假设有一滴熔体从飞行的空间体中分离出来,在大气层的稠密层中经历了表层的过热和沸腾。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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