Abstract
Megacrysts are common in alkali basalt of Quaternary age in the northeastern Harrat Shamah basalt fields of Jordan. The dominant phases are Al-clinopyroxene, Al-bronzite, pleonaste spinel and kaersutite amphibole. The megacrysts differ in composition from analogous phases in associated lherzolite xenoliths, but are similar to those in associated Al-augite pyroxenite xenoliths. Major and trace element partioning indicates that most of the megacrysts may have been in equilibrium with their host magmas at high pressure.
Original language | English |
---|---|
Pages (from-to) | 349-357 |
Number of pages | 9 |
Journal | Journal of African Earth Sciences |
Volume | 21 |
Issue number | 3 |
DOIs | |
Publication status | Published - Oct 1995 |
Externally published | Yes |
ASJC Scopus subject areas
- Geology
- Earth-Surface Processes