Presentation is loading. Please wait.

Presentation is loading. Please wait.

Fig. 5 Final velocity model showing map view of the MHT and a cross section passing through the Gorkha mainshock hypocenter. Final velocity model showing.

Published byよしじろう ひでやま Modified over 5 years ago

Similar presentations

Presentation on theme: "Fig. 5 Final velocity model showing map view of the MHT and a cross section passing through the Gorkha mainshock hypocenter. Final velocity model showing."— Presentation transcript:

1 Fig. 5 Final velocity model showing map view of the MHT and a cross section passing through the Gorkha mainshock hypocenter. Final velocity model showing map view of the MHT and a cross section passing through the Gorkha mainshock hypocenter. Front face to the east and rear face to the west of the cube are Vp wave speeds below and above the MHT surface along the line of profile through the Gorkha mainshock at 84.8°E. Colored subhorizontal plane is the wave speed as measured along our interpreted MHT, showing clear along-strike variability. The wide gray line is gravity lineament (30). Dashed line is a 4000-m elevation contour that trends SE cross-cutting the ESE orogenic strike (elevations increase eastward). Image is true scale (depth scaled 1:1 with latitude and longitude). Ling Bai et al. Sci Adv 2019;5:eaav0723 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

Download ppt "Fig. 5 Final velocity model showing map view of the MHT and a cross section passing through the Gorkha mainshock hypocenter. Final velocity model showing."

Similar presentations

Fig. 2 Nonlinearities in a cavity-embedded perovskite single crystal.

Fig. 2 Nonlinearities in a cavity-embedded perovskite single crystal.
Fig. 4 Altitudinal distributions of ice thickness change (m year−1) for the 650 glaciers. Altitudinal distributions of ice thickness change (m year−1)

Fig. 4 Altitudinal distributions of ice thickness change (m year−1) for the 650 glaciers. Altitudinal distributions of ice thickness change (m year−1)
Fig. 3 FM MnBi2Te4 bulk. FM MnBi2Te4 bulk. Crystal structure (A) and band structure (B) of the FM bulk. (C) Zoom-in band structures along the out-of-plane.

Fig. 3 FM MnBi2Te4 bulk. FM MnBi2Te4 bulk. Crystal structure (A) and band structure (B) of the FM bulk. (C) Zoom-in band structures along the out-of-plane.
Fig. 4 Cross sections across-strike and along-strike of the collision zone (for profile locations see Fig. 3). Cross sections across-strike and along-strike.

Fig. 4 Cross sections across-strike and along-strike of the collision zone (for profile locations see Fig. 3). Cross sections across-strike and along-strike.
Fig. 2 Global production, use, and fate of polymer resins, synthetic fibers, and additives (1950 to 2015; in million metric tons). Global production, use,

Fig. 2 Global production, use, and fate of polymer resins, synthetic fibers, and additives (1950 to 2015; in million metric tons). Global production, use,
Fig. 2 CFD results. CFD results. Results of CFD simulations in horizontal (left column) and vertical (right column) cross-sections. All models oriented.

Fig. 2 CFD results. CFD results. Results of CFD simulations in horizontal (left column) and vertical (right column) cross-sections. All models oriented.
Fig. 2 Data for an example earthquake on 23 August 2015.

Fig. 2 Data for an example earthquake on 23 August 2015.
Fig. 5 Thermal conductivity of n-type ZrCoBi-based half-Heuslers.

Fig. 5 Thermal conductivity of n-type ZrCoBi-based half-Heuslers.
Fig. 1 Map of water stress and shale plays.

Fig. 1 Map of water stress and shale plays.
Fig. 3 Tracing Poynting flux along Polar’s orbit during a period of 28 days, which includes a moderate storm and a major storm. Tracing Poynting flux along.

Fig. 3 Tracing Poynting flux along Polar’s orbit during a period of 28 days, which includes a moderate storm and a major storm. Tracing Poynting flux along.
Fig. 1 NP-free Ch-CNC droplets.

Fig. 1 NP-free Ch-CNC droplets.
Fig. 3 Electron PSD in various regions.

Fig. 3 Electron PSD in various regions.
Fig. 4 Morphogenesis in the Ch-CNC host droplets and NP assemblies.

Fig. 4 Morphogenesis in the Ch-CNC host droplets and NP assemblies.
Fig. 4 Resynthesized complex boronic acid derivatives based on different scaffolds on a millimole scale and corresponding yields. Resynthesized complex.

Fig. 4 Resynthesized complex boronic acid derivatives based on different scaffolds on a millimole scale and corresponding yields. Resynthesized complex.
Fig. 6 Comparison of properties of water models.

Fig. 6 Comparison of properties of water models.
Fig. 2 Reference-fixing experiment, results.

Fig. 2 Reference-fixing experiment, results.
Fig. 2 Ferroelectric domains resolved in WTe2 single crystals.

Fig. 2 Ferroelectric domains resolved in WTe2 single crystals.
Fig. 3 Scan rate effects on the layer edge current.

Fig. 3 Scan rate effects on the layer edge current.
Fig. 2 Stratigraphic profile of the Area 15 excavation block showing the diagnostic cultural materials and components alongside the stratigraphic sequence.

Fig. 2 Stratigraphic profile of the Area 15 excavation block showing the diagnostic cultural materials and components alongside the stratigraphic sequence.
Fig. 3 Rotation experiment, setup.

Fig. 3 Rotation experiment, setup.

Similar presentations

Ads by Google