Full Text Available
Note: Clicking the button above will open the full text document at the original institutional repository in a new window.
Basaltic rocks dredged from the Southwest Indian Ridge (SWIR) between 16 and 26°E were investigated by petrographic microscope, electron microprobe and X-ray fluorescence analysis. Basalts are olivine tholeiites with geochemical characteristics similar to normal, depleted mid-ocean ridge basalts (MO...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Thesis |
| Language: | English English |
| Published: |
Department of Geological Sciences
2026
|
| Subjects: | |
| Tags: |
No Tags, Be the first to tag this record!
|
| Summary: | Basaltic rocks dredged from the Southwest Indian Ridge (SWIR) between 16 and 26°E were investigated by petrographic microscope, electron microprobe and X-ray fluorescence analysis. Basalts are olivine tholeiites with geochemical characteristics similar to normal, depleted mid-ocean ridge basalts (MORB) from the SWIR between 0 and 11° East (le Roex et al., 1983). The suite consists predominantly of aphyric or microporphyritic olivine- and olivine-plagioclase basalts. Several porphyritic lavas are also present. |
|---|