Chen Ming, Lu Yang, Ning Jiahao, Yang Wenge, Shu Jinfu, Mao Ho-kwang. Discovery of the Baijifeng impact structure in Tonghua, Jilin, China[J]. Matter and Radiation at Extremes, 2023, 8(5): 058403. doi: 10.1063/5.0172186
Citation:
Chen Ming, Lu Yang, Ning Jiahao, Yang Wenge, Shu Jinfu, Mao Ho-kwang. Discovery of the Baijifeng impact structure in Tonghua, Jilin, China[J]. Matter and Radiation at Extremes, 2023, 8(5): 058403. doi: 10.1063/5.0172186
Chen Ming, Lu Yang, Ning Jiahao, Yang Wenge, Shu Jinfu, Mao Ho-kwang. Discovery of the Baijifeng impact structure in Tonghua, Jilin, China[J]. Matter and Radiation at Extremes, 2023, 8(5): 058403. doi: 10.1063/5.0172186
Citation:
Chen Ming, Lu Yang, Ning Jiahao, Yang Wenge, Shu Jinfu, Mao Ho-kwang. Discovery of the Baijifeng impact structure in Tonghua, Jilin, China[J]. Matter and Radiation at Extremes, 2023, 8(5): 058403. doi: 10.1063/5.0172186
An impact structure 1400 m in diameter, formed by a bolide impact, has been discovered on Baijifeng Mountain in Tonghua City in Northeast China’s Jilin province. The impact structure takes the form of a cirque-shaped depression on the top of the mountain and is located in a basement mainly composed of Proterozoic sandstone and Jurassic granite. A large number of rock fragments composed mainly of sandstone, with a small amount of granite, are distributed on the top of Baijifeng Mountain. Planar deformation features (PDFs) have been found in quartz in the rock and mineral clasts collected from the surface inside the depression. The forms of the PDFs indexed in the quartz include among others, {101̄3}, {101̄2}, and {101̄1}. The presence of these PDFs provides diagnostic evidence for shock metamorphism and the impact origin of the structure. The impact event took place after the Jurassic Period and probably much later.
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Figure 1. The Baijifeng impact structure on the top of Baijifeng Mountain. The impact structure is a cirque-shaped depression with a diameter of about 1400 m and a height difference of 418 m. The two peaks surrounding this depression are Front Baijifeng on the left side and Rear Baijifeng on the right side. The panoramic view of the impact structure was taken from the southeast. Image: Google CNES / Airbus Maxar Technologies Landsat / Copernicus Data SIO, NOAA, U.S. Navy, NGA, GEBCO.
Figure 2. Impact-ejected rock fragments and evidence of shock metamorphism. (a) Sandstone fragments with sharp edges and corners on the top of Front Baijifeng. (b) Optical microscope image of a quartz grain with three sets of PDFs (highlighted by three solid white lines) with cross-polarized light illumination. (c) Optical microscope image of a quartz grain with two sets of PDFs indexed as {101̄3} (A) and {101̄1} (B) with cross-polarized light illumination.