Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2557-2020
https://doi.org/10.5194/se-11-2557-2020
Research article
 | 
23 Dec 2020
Research article |  | 23 Dec 2020

Seismic gaps and intraplate seismicity around Rodrigues Ridge (Indian Ocean) from time domain array analysis

Manvendra Singh and Georg Rümpker

Viewed

Total article views: 1,868 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,241 552 75 1,868 219 63 72
  • HTML: 1,241
  • PDF: 552
  • XML: 75
  • Total: 1,868
  • Supplement: 219
  • BibTeX: 63
  • EndNote: 72
Views and downloads (calculated since 27 Apr 2020)
Cumulative views and downloads (calculated since 27 Apr 2020)

Viewed (geographical distribution)

Total article views: 1,868 (including HTML, PDF, and XML) Thereof 1,672 with geography defined and 196 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 28 Mar 2024
Download
Short summary
Using seismic array methods, 63 events were located in the Rodrigues–CIR region, not reported by any global network, most of them being off the ridge axis. The lack of seismicity along this section of the CIR, as observed from global data and this study, can possibly be attributed to the presence of partially molten mantle beneath Rodrigues Ridge. The results will be of interest for a broad range of geoscientists interested in the tectonic evolution of Indian Ocean and plume–crust interaction.