Crustal Structure of the Northeast Indian Ocean.
NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
Pagination or Media Count:
Seismic reflection and refraction measurements indicate that four separate velocity layers exist above the mantle in this area. Their combined thickness ranges from 4 to 8 km. The Mohorovicic Discontinuity occurs at a depth of 9.3 km. above sea level in several of the seismic sections shown. Author
- Physical and Dynamic Oceanography
- Geology, Geochemistry and Mineralogy