Add to ORKGThesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1991.Includes bibliographical references (p. 208-224).by Anne Frances Sheehan.Ph.D
Large-scale topography may be due to several causes, including (1) variations in crustal thickness a...
The nature of subsidence near the ridge crest of the intermediate and fast spreading mid-ocean ridge...
Oceanic residual depth varies on urn:x-wiley:jgrb:media:jgrb54314:jgrb54314-math-0001 5,000 km wavel...
Resolution of both the extent and mechanism of lateral heterogeneity in the upper mantle constraints...
Long-wavelength variations in geoid height, bathymetry, and SS-S travel times are all relatable to l...
A 20-Myr record of creation of oceanic lithosphere at a segment of the central Mid-Atlantic-Ridge is...
Using seismic body and surface waves, the velocity structure of the Earth's mantle is determined wit...
A 20-Myr record of creation of oceanic lithosphere at a segment of the central Mid-Atlantic-Ridge is...
Using seismic body and surface waves, the velocity structure of the Earth's mantle is determined wit...
An analysis of records of multiply reflected ScS phases from ten deep‐focus earthquakes yields near‐...
Temperature, velocity, and viscosity profiles for coupled thermal and mechanical models of the upper...
An analysis of records of multiply reflected ScS phases from ten deep‐focus earthquakes yields near‐...
Oceanic lithosphere constitutes the upper boundary layer of the Earth’s convecting mantle. Its struc...
.We investigate seismic layering i.e., discontinuities, regions of anomalous velocity gradients, and...
A 20-Myr record of creation of oceanic lithosphere is exposed along a segment of the central Mid-Atl...
Large-scale topography may be due to several causes, including (1) variations in crustal thickness a...
The nature of subsidence near the ridge crest of the intermediate and fast spreading mid-ocean ridge...
Oceanic residual depth varies on urn:x-wiley:jgrb:media:jgrb54314:jgrb54314-math-0001 5,000 km wavel...
Resolution of both the extent and mechanism of lateral heterogeneity in the upper mantle constraints...
Long-wavelength variations in geoid height, bathymetry, and SS-S travel times are all relatable to l...
A 20-Myr record of creation of oceanic lithosphere at a segment of the central Mid-Atlantic-Ridge is...
Using seismic body and surface waves, the velocity structure of the Earth's mantle is determined wit...
A 20-Myr record of creation of oceanic lithosphere at a segment of the central Mid-Atlantic-Ridge is...
Using seismic body and surface waves, the velocity structure of the Earth's mantle is determined wit...
An analysis of records of multiply reflected ScS phases from ten deep‐focus earthquakes yields near‐...
Temperature, velocity, and viscosity profiles for coupled thermal and mechanical models of the upper...
An analysis of records of multiply reflected ScS phases from ten deep‐focus earthquakes yields near‐...
Oceanic lithosphere constitutes the upper boundary layer of the Earth’s convecting mantle. Its struc...
.We investigate seismic layering i.e., discontinuities, regions of anomalous velocity gradients, and...
A 20-Myr record of creation of oceanic lithosphere is exposed along a segment of the central Mid-Atl...
Large-scale topography may be due to several causes, including (1) variations in crustal thickness a...
The nature of subsidence near the ridge crest of the intermediate and fast spreading mid-ocean ridge...
Oceanic residual depth varies on urn:x-wiley:jgrb:media:jgrb54314:jgrb54314-math-0001 5,000 km wavel...