Mid-plate tectonics in the Indian Ocean
- 10 November 1972
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 77 (32), 6413-6421
- https://doi.org/10.1029/jb077i032p06413
Abstract
Zones of faulted and folded sediments occur at and near the southern margin of the Ganges cone. The cone sediments act as sensitive indicators of crustal distortion, since they consist generally of continuous, flat‐lying sediments that are well stratified. The strike of the faults and folds is approximately 10° south of east, which is about normal to the direction of compression in the Himalayas on the north end of the Indian plate. These faults and folds lie within the NW‐SE trending zone of seismicity in the northeast Indian Ocean which has been speculated to be a nascent arc‐trench, about midway between the spreading midocean ridge on the south and the Himalayan front on the north.Keywords
This publication has 5 references indexed in Scilit:
- The Evolution of the Indian Ocean since the Late CretaceousGeophysical Journal International, 1971
- Growth of the Bengal Deep-Sea Fan and Denudation in the HimalayasGSA Bulletin, 1971
- Wrench Movements in the Baluchistan Arc and Relation to Himalayan-Indian Ocean TectonicsGSA Bulletin, 1971
- Seismicity of the Indian Ocean and a possible nascent island arc between Ceylon and AustraliaJournal of Geophysical Research, 1970
- Sea-floor spreading and continental driftJournal of Geophysical Research, 1968