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Lehmann discontinuity

Chapter 3. the Crust and Upper Mantle
The Deep Structure of Continents
Upper-Mantle Low-Velocity Zone Structure Beneath the Kaapvaal Craton from S-Wave Receiver Functions
MAPS CCP STACKS of P- & S-Wave RECEIVER
Inge Lehmann: Discoverer of the Earth's Inner Core 2/4/17, 524 PM
Anisotropic Shear-Wave Velocity Structure of the Earth's Mantle
Seismic and Electrical Signatures of the Lithosphere–Asthenosphere System of the Normal Oceanic Mantle
Earth's Internal Structure: a Seismologist's View
Mantle Flow and Melting Beneath Young Oceanic Lithosphere: Seismic
Kshamayaa Dharithri 1 (Oh Tolerant Mother Earth! Forgive Me)
Interior Parts of the Earth in Reference to Seismology
Oceanic Mantle Dynamics Implementation Plan: Report of a Community Workshop
The Lehmann Discontinuity Due to Dehydration of Subducted Sediment Shigeaki Ono*,1,2
Not My Fault: Celebrating Inge Seismic Waves Suddenly Vanished
The Shear-Wave Velocity Structure in the Upper Mantle Beneath Eurasia
3 Seismic Structure of the Lithosphere
Structure of the Oceanic Lithosphere and Upper Mantle North of the Gloria Fault in the Eastern Mid-Atlantic by Receiver Function Analysis
Inge Lehmann's Work Materials and Seismological Epistolary Archive

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Detection of a New Sub-Lithospheric Discontinuity in Central Europe with S-Receiver Functions
[Comment on Seismology in the Days of Old by Inge Lehmann] The
The Crust and Upper Mantle
The Solid Earth: an Introduction to Global Geophysics, Second Edition C
Paper Were Calculated Using the LQT Coordinate System, for Simplicity We
Inge Lehmann's Paper: “ P'” (1936)
Dynamic Planet Answer Key Science Olympiad North Regional Tournament at the University of Florida

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