Origin of the Powai ankaramite, and the composition, P–T conditions of equilibration and evolution of the primary magmas of the Deccan tholeiites
The Powai ankaramite flow from Mumbai, western Deccan Traps, contains abundant crystals of augite (En[subscript 59–47]Fs[subscript 10–14]Wo[subscript 27–42], 22–40 modal %, 3–5 mm) and olivine (Fo[subscript 84–74], 11–16 modal %, 1–2 mm), and minor plagioclase (An[subscript 71], ~0.5 mm) embedded in...
| Main Authors: | , |
|---|---|
| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
Springer Berlin Heidelberg
2017
|
| Online Access: | http://hdl.handle.net/1721.1/107268 |