Evolution of the Southwest Indian Ridge from 55°45′E to 62°E : changes in plate-boundary geometry since 26 Ma
Baines, A. Graham
Cheadle, Michael J.
Dick, Henry J. B.
Scheirer, Allegra Hosford
John, Barbara E.
Kusznir, Nick J.
MetadataShow full item record
From 55°45′E to 58°45′E and from 60°30′E to 62°00′E, the ultraslow-spreading Southwest Indian Ridge (SWIR) consists of magmatic spreading segments separated by oblique amagmatic spreading segments, transform faults, and nontransform discontinuities. Off-axis magnetic and multibeam bathymetric data permit investigation of the evolution of this part of the SWIR. Individual magmatic segments show varying magnitudes and directions of asymmetric spreading, which requires that the shape of the plate boundary has changed significantly over time. In particular, since 26 Ma the Atlantis II transform fault grew by 90 km to reach 199 km, while a 45-km-long transform fault at 56°30′E shrank to become an 11 km offset nontransform discontinuity. Conversely, an oblique amagmatic segment at the center of a first-order spreading segment shows little change in orientation with time. These changes are consistent with the clockwise rotation of two ~450-km-wide first-order spreading segments between the Gallieni and Melville transform faults (52–60°E) to become more orthogonal to spreading. We suggest that suborthogonal first-order spreading segments reflect a stable configuration for mid-ocean ridges that maximizes upwelling rates in the asthenospheric mantle and results in a hotter and weaker ridge-axis that can more easily accommodate seafloor spreading.
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry Geophysics Geosystems 8 (2007): Q06022, doi:10.1029/2006GC001559.
Suggested CitationArticle: Baines, A. Graham, Cheadle, Michael J., Dick, Henry J. B., Scheirer, Allegra Hosford, John, Barbara E., Kusznir, Nick J., Matsumoto, Takeshi, "Evolution of the Southwest Indian Ridge from 55°45′E to 62°E : changes in plate-boundary geometry since 26 Ma", Geochemistry Geophysics Geosystems 8 (2007): Q06022, DOI:10.1029/2006GC001559, https://hdl.handle.net/1912/1790
Showing items related by title, author, creator and subject.
Montesi, Laurent G. J.; Behn, Mark D.; Hebert, Laura B.; Lin, Jian; Barry, Jennifer L. (American Geophysical Union, 2011-10-04)Crustal thickness variations at the ultraslow spreading 10–16°E region of the Southwest Indian Ridge are used to constrain melt migration processes. In the study area, ridge morphology correlates with the obliquity of the ...
Tucholke, Brian E.; Houtz, Robert E.; Barrett, Douglas M. (American Geophysical Union, 1981-05-10)The Agulhas Plateau lies 500 km off the Cape of Good Hope in the southwestern Indian Ocean. Acoustic basement beneath the northern one third of this large, aseismic structural high has rugged morphology, but basement in ...
Mineralogical and geochemical features of sulfide chimneys from the 49°39′E hydrothermal field on the Southwest Indian Ridge and their geological inferences Tao, Chunhui; Li, Huaiming; Huang, Wei; Han, XiQiu; Wu, GuangHai; Su, Xin; Zhou, Ning; Lin, Jian; He, YongHua; Zhou, JianPing (Springer, 2011-08-24)During January–May in 2007, the Chinese research cruise DY115-19 discovered an active hydrothermal field at 49°39′E/37°47′S on the ultraslow spreading Southwest Indian Ridge (SWIR). This was also the first active hydrothermal ...