Deformation of the Makran accretionary sediment prism in the Gulf of Oman (north-west Indian Ocean)

@article{White1982DeformationOT,
  title={Deformation of the Makran accretionary sediment prism in the Gulf of Oman (north-west Indian Ocean)},
  author={Robert S. White},
  journal={Geological Society, London, Special Publications},
  year={1982},
  volume={10},
  pages={357 - 372}
}
  • R. White
  • Published 1982
  • Geology
  • Geological Society, London, Special Publications
Summary The offshore Makran of Pakistan and Iran in the Gulf of Oman forms the seaward margin of a folded and faulted accretionary sediment wedge which extends several hundred kilometres inland across the onshore Makran. Sediment is being scraped off the oceanic Arabian plate as it subducts shallowly northward beneath the Eurasian plate. The submerged front of the accretionary prism has been traced along the entire width of the Makran continental margin, from the Strait of Hormuz in the west to… 

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References

SHOWING 1-10 OF 46 REFERENCES
Tectonics of the western Gulf of Oman
The Oman line, running northward from the Strait of Hormuz separates a continent-continent plate boundary to the northwest (Persian Gulf region) from an ocean-continent plate boundary to the
Makran of Iran and Pakistan as an active arc system
The character of convergence along the Arabian-Iranian plate boundary changes radically eastward from the Zagros ranges to the Makran region. This appears to be due to collision of continental crust
Tertiary Geology of Part of South Makran, Baluchistan, West Pakistan
The South Makran basin in the southern part of the Baluchistan basin was the site of considerable clastic sedimentation from the Oligocene onward. The sediments formed a wedge thickening seaward from
The Structure of the Crust and Upper Mantle in the Region of Barbados and the Lesser Antilles
Summary The results of marine geophysical surveys across the Lesser Antilles in 1971 and 1972 by Durham University and the Royal Navy as part of the CICAR Project have revealed that the arc front
Anatomy of the Mexican Ridges, Southwestern Gulf of Mexico: Small Basin Margins
Six subparallel multichannel seismic lines across the Mexican Ridges foldbelt in the southwestern Gulf of Mexico between 21°N and 22°N latitude show details of the folds and provide new insight into
Wrench Movements in the Baluchistan Arc and Relation to Himalayan-Indian Ocean Tectonics
Satellite photographs provide evidence that the structural discontinuity between the east-west-trending Makran Ranges and the north-south-trending Kirthar and Sulaiman Ranges of the Baluchistan Arc
Seismotectonic provinces of Iran
  • Ali A. Nowroozi
  • Geology
  • 1976
abstract Over 600 earthquakes that occurred in Iran between 1920 and 1972 have been relocated. The new epicentral positions delineate many active faults and seismically active tectonic zones in Iran.
...
1
2
3
4
5
...