1969
DOI: 10.1080/00206816909475124
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Chlorine in the formation of Ampalyk magnetite deposit

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“…CHLORINE-BEARING potassium amphiboles are typical of metasomatites from ore deposits, particularly iron-ores, but sometimes occur in granites, potassic syenites, and gneisses (Krutov, 1936;Hallimond, 1947;Ontoev, 1958: Geijer, 1960Serdyuchenko, 1960;Kalinin, 1983;Lobanova, 1963;Pavlov, 1964;Deer et al, 1965;Vakhrushev, 1965;Knyazev, 1966;Kostyuk, 1970;Leake, 1978;Dick and Robinson, 1979;Minerals, 1981;Sharma, 1981;Kamineri and Bonardi, 1982). A high chlorine content is the most typical feature of amphiboles from metasomatites of iron-ore deposits (Minerals, 1981).…”
Section: High Potassium-chlorine-bearing Hastingsites In Skarns From mentioning
confidence: 99%
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“…CHLORINE-BEARING potassium amphiboles are typical of metasomatites from ore deposits, particularly iron-ores, but sometimes occur in granites, potassic syenites, and gneisses (Krutov, 1936;Hallimond, 1947;Ontoev, 1958: Geijer, 1960Serdyuchenko, 1960;Kalinin, 1983;Lobanova, 1963;Pavlov, 1964;Deer et al, 1965;Vakhrushev, 1965;Knyazev, 1966;Kostyuk, 1970;Leake, 1978;Dick and Robinson, 1979;Minerals, 1981;Sharma, 1981;Kamineri and Bonardi, 1982). A high chlorine content is the most typical feature of amphiboles from metasomatites of iron-ore deposits (Minerals, 1981).…”
Section: High Potassium-chlorine-bearing Hastingsites In Skarns From mentioning
confidence: 99%
“…3). This may be due to the fact that potassic granosyenites occur as a rule in all deposits containing potassic amphiboles (Pavlov, 1964;Vakhrushev, 1965;Minerals, 1981;and others). The chlorine content in CI-K amphiboles does not correlate with potassium content.…”
Section: Chemical Composition and Features Of Amphibolesmentioning
confidence: 99%