Коесит (Ukrainian Wikipedia)

Analysis of information sources in references of the Wikipedia article "Коесит" in Ukrainian language version.

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doi.org

  • Chao, E. C. T.; Shoemaker, E. M.; Madsen, B. M. (1960). First Natural Occurrence of Coesite. Science. 132 (3421): 220—222. Bibcode:1960Sci...132..220C. doi:10.1126/science.132.3421.220. PMID 17748937. Coesite, the high-pressure polymorph of SiO(2), hitherto known only as a synthetic compound, is identified as an abundant mineral in sheared Coconino sandstone at Meteor Crater, Arizona. This natural occurrence has important bearing on the recognition of meteorite impact craters in quartz-bearing geologic formations.(англ.)
  • Chao EC, Fahey JJ, Littler J. (1961 Mar 24). Coesite from Wabar Crater, near Al Hadida, Arabia. Science. 133 (3456): 882—884. doi:10.1126/science.133.3456.882. PMID 17789750. Архів оригіналу за 19 Листопада 2018. Процитовано 19 листопада 2018. The third natural occurrence of coesite, the high pressure polymorph of silica, is found at the Wabar meteorite crater, Arabia. The Wabar crater is about 300 feet in diameter and about 40 feet deep. It is the smallest of three craters where coesite has been found.
  • Bunch TE, Cohen AJ. (1963 Oct 18). Coesite and Shocked Quartz from Holleford Crater, Ontario, Canada. Science. 142 (3590): 379(81). doi:10.1126/science.142.3590.379. PMID 17799478. Архів оригіналу за 19 Листопада 2018. Процитовано 19 листопада 2018. {{cite journal}}: Cite має пусті невідомі параметри: |8= та |10= (довідка)(англ.)

dx.doi.org

handbookofmineralogy.org

harvard.edu

ui.adsabs.harvard.edu

  • Chao, E. C. T.; Shoemaker, E. M.; Madsen, B. M. (1960). First Natural Occurrence of Coesite. Science. 132 (3421): 220—222. Bibcode:1960Sci...132..220C. doi:10.1126/science.132.3421.220. PMID 17748937. Coesite, the high-pressure polymorph of SiO(2), hitherto known only as a synthetic compound, is identified as an abundant mineral in sheared Coconino sandstone at Meteor Crater, Arizona. This natural occurrence has important bearing on the recognition of meteorite impact craters in quartz-bearing geologic formations.(англ.)

main.jp

cnmnc.main.jp

mineralatlas.eu

nih.gov

pubmed.ncbi.nlm.nih.gov

  • Chao, E. C. T.; Shoemaker, E. M.; Madsen, B. M. (1960). First Natural Occurrence of Coesite. Science. 132 (3421): 220—222. Bibcode:1960Sci...132..220C. doi:10.1126/science.132.3421.220. PMID 17748937. Coesite, the high-pressure polymorph of SiO(2), hitherto known only as a synthetic compound, is identified as an abundant mineral in sheared Coconino sandstone at Meteor Crater, Arizona. This natural occurrence has important bearing on the recognition of meteorite impact craters in quartz-bearing geologic formations.(англ.)
  • Chao EC, Fahey JJ, Littler J. (1961 Mar 24). Coesite from Wabar Crater, near Al Hadida, Arabia. Science. 133 (3456): 882—884. doi:10.1126/science.133.3456.882. PMID 17789750. Архів оригіналу за 19 Листопада 2018. Процитовано 19 листопада 2018. The third natural occurrence of coesite, the high pressure polymorph of silica, is found at the Wabar meteorite crater, Arabia. The Wabar crater is about 300 feet in diameter and about 40 feet deep. It is the smallest of three craters where coesite has been found.
  • Bunch TE, Cohen AJ. (1963 Oct 18). Coesite and Shocked Quartz from Holleford Crater, Ontario, Canada. Science. 142 (3590): 379(81). doi:10.1126/science.142.3590.379. PMID 17799478. Архів оригіналу за 19 Листопада 2018. Процитовано 19 листопада 2018. {{cite journal}}: Cite має пусті невідомі параметри: |8= та |10= (довідка)(англ.)

ncbi.nlm.nih.gov

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wikidata.org

wikipedia.org

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