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Discover (Random Books)

First Break

First Break

A.J. Guus Berkhout

Общая геофизика (1)

Making Treaties Work: Human Rights, Environment and Arms Control

Making Treaties Work: Human Rights, Environment and Arms Control

Geir Ulfstein & Thilo Maaruhn & Andreas Zimmermann (...)

Medical Geography (1)

Совесть академии: к 100-летию со дня рождения М.А. Леонтовича

Совесть академии: к 100-летию со дня рождения М.А. Леонтовича

Leontovich M.A. & Shafranov V.D.

Медицинская география (1)

The role of dilation and cementation in the formation of cataclasite in low temperature deformation of well cemented quartz-rich rocks

The role of dilation and cementation in the formation of cataclasite ...

Charles M. Onasch & John R. Farver & William M. Dunne (...)

Lithology (1)

Category: phase

Fault rocks from the SAFOD core samples: Implications for weakening at shallow depths along the San Andreas Fault, California

Fault rocks from the SAFOD core samples: Implications for weakening ...

R.E. Holdsworth & E.W.E. van Diggelen & C.J. Spiers & J.H.P. de Bresser (...)

Lithology (1)

Key-ring structure gradients and sheath folds in the Goantagab Domain of NW Namibia

Key-ring structure gradients and sheath folds in the Goantagab ...

Cees Passchier & Rudolph Trouw & Sara Coelho & Eric de Kemp (...)

Normal-fault development during two phases of non-coaxial extension: An experimental study

Normal-fault development during two phases of non-coaxial extension: ...

Alissa A. Henza & Martha O. Withjack & Roy W. Schlische (...)

Geological and geophysical studies of the deep structure of the Earth (1)

Overview - Mineral Physics: Past, Present, and Future

Overview - Mineral Physics: Past, Present, and Future

G. D. Price

Overview – Mineral Physics: Past, Present, and Future

Overview – Mineral Physics: Past, Present, and Future

Density of the Earth & by Williamson & Adams (1923). Here, elastic constants of various rock types ... & gravitational data. Their work was marked by taking into account ... & the longitudinal & shear seismic wave velocities Vp & Vs) & mineral properties (Ks, the adiabatic bulk modulus & density, x1a), via d x1aðr Þ = – gðr Þdr _jðr Þ, ½1Š ... & is given by j(r) = V2 p (r)–4_3V2 s (r) = Ks (r) x1a (r) ½2Š. ... (...)

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