MicroRaman spectroscopy of anomalous planar microstructures in quartz from Mt. Oikeyama: Discovery of a probable impact crater in Japan |
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| Authors: | Masao SAKAMOTO Arnold GUCSIK Hirotsugu NISHIDO Kiyotaka NINAGAWA Tasuku OKUMURA Shin TOYODA |
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| Institution: | 1. Iida City Museum, 2‐655 Ohtemach, Iida, Nagano 395‐0034, Japan;2. Department of Geochemistry, Max Planck Institute for Chemistry, Joh.‐J.‐Becherweg 27, D‐55128 Mainz, Germany;3. Okayama University of Science, Research Institute of Natural Sciences, 1‐1 Ridai‐cho, Kita‐ku, Okayama 700‐0005, Japan;4. Department of Applied Physics, Okayama University of Science, 1‐1 Ridai‐cho, Kita‐ku, Okayama 700‐0005, Japan |
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| Abstract: | Abstract– Planar deformation features (PDFs) and planar fractures (PFs) have been found and confirmed by optical microscope observations and microRaman spectroscopy in quartz grains from Mt. Oikeyama (Akaishi Mountains, Central Japan), for which the semicircular topographic feature of the ridge suggests a crater formed by an impact event. According to the optical microscope observations, a low shock pressure (8–10 GPa) is estimated by the occurrence of basal or ω PDFs leading to lack of multiple sets of PDFs. In addition, a new type of planar microstructure was found in several quartz grains. The microRaman characteristics of PDFs in quartz from Mt. Oikeyama show the amorphous state indicating the presence of weak broad bands at 400 and 800 cm?1 peak positions. These characteristics are indicative of PDFs that are limited to shocked quartz. This indicates an impact origin for distinct planar microstructures in quartz from Mt. Oikeyama. |
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