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。
SWIR延展在西南印度洋的羅德里格斯三相點和南大西洋的布維三聯接合點之間。[1][2][3][4]
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
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坐标：25°30′00″S 70°00′00″E / 25.5000°S 70.0000°E
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