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The Undyulyung Meteorite

机译:Undyulyung陨石

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A meteorite fall was observed by a helicopter crew in flight on September 11, 1986. The meteorite fell to the point bar at the mouth of the Byukkyakh River, the right tributary of the Undyulyung River influent on the right into the Lena River, 80 km upstream the Zhigansk Settlement (Fig. 1). After landing, the pilots immediately found two stones that were still warm, which were distinguished by their black color against the background of the light dolomite pebbles of the point bar. The meteorite had broken into three fragments, two of which were found by the crew. Due to time constraints, the third small fragment was not detected. In 1989, V.V. Korotkov, a member of the helicopter crew, delivered the meteorite samples to the IGABM museum. At present, this meteorite may be studied by permission of the museum staff. The meteorite was called Undyulyung after its locality (φ = 66°8′ N and λ = 124°46′ E). The fall area is located in the Zhigansk administrative district of Yakutia. The total weight of two meteorite samples is 113.4 g. A flattened sample, 65 x 38 x 31 mm in size and 97.7 g in weight, was taken for the investigation (Fig. 2). The second fragment was sent as a sample to the Committee for Meteorites of the Russian Academy of Sciences. The meteorite is enveloped in a black crust of melting. The light gray material of the meteorite is solid and devoid of fractures. The chondritic structure is distinctly observed on polished surfaces and shear planes. Chondrules are 0.3-2.0 mm in size. The uniform impregnation of small metallic particles is seen on the surface of a fresh chip.
机译:1986年9月11日,在飞行中的直升机机组人员观察到陨石坠落。陨石坠落在Byukkyakh河口处的点形柱上,Byukkyakh河是Undyulyung河的右支流,向右流入Lena河,距离80 km Zhigansk居民区上游(图1)。降落后,飞行员立即发现了两块仍很温暖的石头,它们以点状酒吧的浅白云石小石块为背景的黑色来区分。陨石分成三个碎片,机组人员发现了两个。由于时间限制,未检测到第三个小片段。 1989年直升机机组人员科罗特科夫将陨石样品运送到IGABM博物馆。目前,可以在博物馆工作人员的允许下研究这种陨石。陨石因其位置(φ= 66°8'N和λ= 124°46'E)而被称为Undyulyung。下降区位于雅库特的日甘斯克行政区。两个陨石样品的总重量为113.4 g。取一个扁平样品,尺寸为65 x 38 x 31 mm,重量为97.7 g,进行研究(图2)。第二个片段作为样本发送给俄罗斯科学院陨石委员会。陨石被包裹在黑色熔化的外壳中。陨石的浅灰色物质是固体,没有破裂。在抛光的表面和剪切面上清楚地观察到软骨组织。软骨大小为0.3-2.0毫米。在新碎屑的表面上可以看到小金属颗粒的均匀浸渍。

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