| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6442379 | Precambrian Research | 2012 | 22 Pages |
Abstract
⺠The Katherina volcanics is a succession of rhyolitic lavas with minor pyroclastics. ⺠They exhibit a potassic alkaline and peraluminous affinity and A-type character. ⺠Evolution was through fractional crystallization of mantle-derived parental magma. ⺠Had been emplaced within anorogenic period in within-plate volcanic zones setting.
Related Topics
Physical Sciences and Engineering
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Authors
Mohammed Z. El-Bialy, Imbarak S. Hassen,