A Contribution to the Genesis of Analcite after Leucite in Potassic Volcanic Rocks of the Nadik Area, Kerman, Iran
The origin of analcite-bearing lavas and potassic volcanic rocks is controversial in the geological record. Two main hypotheses are either primary analcite or replacement pseudomorphous of leucite. Spectacular large (5 cm) euhedral trapezohedra occur as single crystals of analcite in tephriphonolite...
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| Format: | Article |
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| Language: | English |
| Published: |
University of Tehran
2008-04-01
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| Series: | Journal of Sciences, Islamic Republic of Iran |
| Online Access: | https://jsciences.ut.ac.ir/article_31090_035ea5fdca39233db5a464e1d4771001.pdf |
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