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The lithosphere-asthenosphere boundary
Seismological models of upper-mantle structure are providing new constraints on the
physical and chemical properties that differentiate the lithosphere from the asthenosphere. A …
physical and chemical properties that differentiate the lithosphere from the asthenosphere. A …
Towards a better understanding of African topography: a review of passive-source seismic studies of the African crust and upper mantle
S Fishwick, ID Bastow - 2011 - pubs.geoscienceworld.org
Explaining the cause and support of Africa's varied topography remains a fundamental
question for our understanding of the long-term evolution of the continent. As geodynamical …
question for our understanding of the long-term evolution of the continent. As geodynamical …
The seismic mid-lithosphere discontinuity
Seismic S-wave receiver functions (SRF) are a uniquely powerful tool for imaging velocity
discontinuities within the upper mantle. SRF data frequently contain negative phases at …
discontinuities within the upper mantle. SRF data frequently contain negative phases at …
North American lithospheric discontinuity structure imaged by Ps and Sp receiver functions
Sp and Ps converted seismic waves at 93 permanent seismic stations are used to image
upper mantle velocity discontinuities across the contiguous United States and portions of …
upper mantle velocity discontinuities across the contiguous United States and portions of …
Surface wave tomography: imaging of the lithosphere–asthenosphere boundary beneath central and southern Africa?
The lithosphere–asthenosphere boundary (LAB) remains a controversial subject in Earth
sciences, and beneath cratonic regions appears to be a particularly difficult boundary to …
sciences, and beneath cratonic regions appears to be a particularly difficult boundary to …
The lithosphere–asthenosphere boundary and cratonic lithospheric layering beneath Australia from Sp wave imaging
Sp and Ps scattered wave receiver functions were calculated for nineteen stations across
Australia and the island of Tasmania in order to image the lithosphere–asthenosphere …
Australia and the island of Tasmania in order to image the lithosphere–asthenosphere …
Constraints on the depth and thermal history of cratonic lithosphere from peridotite xenoliths, xenocrysts and seismology
Despite the relatively long-standing availability of numerical approaches for estimating
palaeogeotherms using peridotite xenolith Pressure–Temperature (P–T) data, the practise of …
palaeogeotherms using peridotite xenolith Pressure–Temperature (P–T) data, the practise of …
Characterization and petrological constraints of the midlithospheric discontinuity
Within continental lithosphere, widespread seismic evidence suggests a sharp
discontinuous downward decrease in seismic velocity at 60–160 km depth. This …
discontinuous downward decrease in seismic velocity at 60–160 km depth. This …
On the feasibility and use of teleseismic P wave coda autocorrelation for map** shallow seismic discontinuities
Seismic body waves from distant earthquakes, which propagate near vertically beneath
recording stations, provide tools for imaging shallow Earth structures with high vertical …
recording stations, provide tools for imaging shallow Earth structures with high vertical …
New insights into the crust and lithospheric mantle structure of Africa from elevation, geoid, and thermal analysis
We present new crust and lithosphere thickness maps of the African mainland based on
integrated modeling of elevation and geoid data and thermal analysis. The approach …
integrated modeling of elevation and geoid data and thermal analysis. The approach …