'Seismic profile' presentation slideshows

200 Myr of oceanic crust accumulation

Shear-driven magma segregation. Super-adiabatic boundary layer. REGION B. Hawaii source. Thermal max. 300 km. Tp decreases with depth. Narrow downwellings. Broad passive upwellings. MORB source. TRANSITION ZONE (TZ). 600 km. 600 km. (RIP). 200 Myr of oceanic crust accumulation.

278 views • 17 slides

Searching for blind faults: the Haiti subsurface imaging project

262 views • 15 slides

Tectonics of the Eastern Great Basin

Tectonics of the Eastern Great Basin. Tyler Szwarc and Mark Gorenc. The Great Salt Lake Basin. Bounded by normal faults that reach up down to 5 km into the crust. Cenozoic sediments fill the grabens up to 10,000 feet.

213 views • 5 slides

H Thybo & CA Nielsen Nature 457 , 873-876 (2009) doi:10.1038/nature07688

Model of seismic compressional velocity along the seismic profile across the BRZ. H Thybo & CA Nielsen Nature 457 , 873-876 (2009) doi:10.1038/nature07688.

112 views • 1 slides