Olivine and Cr-spinel as indicators of the petrogenesis and partial melting conditions of the high-MgO ultramafic volcanic rocks from NW Ad Dhala Province—Yemen
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
https://link.springer.com/content/pdf/10.1007/s11631-021-00454-6.pdf
Reference106 articles.
1. Albaréde F (1992) How deep do common basaltic magmas form and differentiate? J Geophys Res 97:10997–11009
2. Al-kadasi, M.A (1994) Temporal and spatial evolution of the basal flow of the Yemen volcanic group. University of London. 284.
3. Almond DC (1986) Geological evolution of the Afro-Arabian Dome. Tectonophysics 131:301–332
4. Arai S (1992) Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry. Mineral Mag 56:173–218
5. Arai S (1994) Compositional variation of olivine-chromian spinel in Mg-rich magmas as a guide to their residual spinel peridotites. J Volcanol Geoth Res 59:279–293
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