Reference Type | - plain text - |
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Original Entry | Large Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu. |
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Mindat Ref. ID | 15941518 | Long-form Identifier | mindat:1:5:15941518:6 |
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GUID | 01cf101b-2464-4597-8aa6-20f49d843c12 |
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Full Reference | Large Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu. |
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Plain Text | Large Tolbachik Fissure Eruption, S.A. Fedotov, Moscow 1984 p340, states that Cristobalite does not occur as independent mineral, but as inclusions in high temp sublimates. After dissolving the sublimates, Cristobalite was found in the residu. |
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