西南印度洋脊
西南印度洋脊 (SWIR) 是沿著印度洋西南的海床分割板塊邊界的地质构造，它將南極板塊和非洲板塊以南北向分離。
參考資料
编辑- ^ JOHN G. SCLATER; C. G. A. HARRISON, Elevation of Mid-ocean Ridges and the Evolution of the South-west Indian Ridge, Nature Publishing Group, 1971 [24 February 2015], （原始内容存档于2020-11-26）
- ^ Ansorge, Isabelle Jane; Pakhomov, E. A; Kaehler, S; Lutjeharms, J. R. E; Durgadoo, J. V, Physical and biological coupling in eddies in the lee of the South-West Indian Ridge.(Report), Polar Biology (Springer), 2010-06-01, 33 (6): 747(13), ISSN 0722-4060
- ^ Bruno Hamelin; Claude J. Allègre, Large-scale regional units in the depleted upper mantle revealed by an isotope study of the South-West Indian Ridge, Nature Publishing Group, 1985 [24 February 2015], （原始内容存档于2020-12-02）
- ^ Robinson, Paul T; Von Herzen, Richard P; Adamson, Andrew C; Becker, Keir; Bloomer, Sherman H; Cannat, Mathilde; Dick, Henry J.B; Emmermann, Rolf F.K; Gard, Gunilla; Goldberg, David; Hebert, Rejean; Hertogen, Jan G.H; Hoskins, Hartley; Iturrino, Gerardo; Kassenaar, J. Dirk C; Kempton, Pamela D, Plutonic rocks in fracture zones. (ocean drilling program in the Atlantis II fracture zone on the south-west Indian ridge), Nature (Nature Publishing Group), 1988-05-12, v333 (n6169): p115(2), ISSN 0028-0836
25°30′00″S 70°00′00″E / 25.5000°S 70.0000°E
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