| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4731697 | Journal of Asian Earth Sciences | 2011 | 17 Pages |
Abstract
⺠The Hadb adh Dayheen ring complex (HDRC), comprises alkaline to peralkaline granites. ⺠Field and textural observations indicate that HDRC formed at different stages. ⺠Textural and chemical characteristics show primary and secondary metasomatic effects. ⺠Geochemical characteristics indicate that the HDRC granite has a post-orogenic A-type affinity. ⺠Magma that formed the HDRC may have originated by partial melting of underplated juvenile lower crust.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
A.M. Moghazi, H.M. Harbi, K.A. Ali,