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А. Е. Саргсян & А. Т. Демченко & Н. В. Дворянчиков & Г. А. Джинчвелашвили (...)
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Why joints are more abundant than faults. A conceptual model ...
Riccardo Caputo
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Waves in the Ocean and Atmosphere: Introduction to Wave Dynamics
Dr. Joseph Pedlosky
Hydrogeology (1)
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Brian B. Looney & Ronald W. Falta
Vadose zone science and technology solutions
Ronald W. Falta, Ph.D. & Brian B. Looney, Ph.D.
Unlocking the effects of friction on fault damage zones
Heather M. Savage & Michele L. Cooke
Geological and geophysical studies of the deep structure of the Earth (1)
U-X-L encyclopedia of science
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Methods of laboratory mineralogical-petrographic and geochemical research (1)
THE FLOW OF HOMOGENEOUS FLUIDS THROUGH POROUS MEDIA
M. Muskat & R. D. Wyckoff
The effect of the intermediate principal stress on fault formation ...
Bezalel Haimson & John W. Rudnicki
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Strain pattern within and around denser blocks sinking within ...
Stef? Burchardt & Hemin Koyi & Harro Schmeling (...)
Stochastic modeling for the stress inversion of vein orientations: ...
Atsushi Yamaji & Katsushi Sato & Satoshi Tonai (...)
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Statistical Analysis in Climate Research
Hans von Storch & Francis W. Zwiers
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Spatial Data Modelling for 3D GIS
Alias Abdul-Rahman & Morakot Pilouk
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Arnold Verruijt
Shear band formation and strain localization on a regional scale: ...
P. Moni?d & P. Agard & R. Augier (...)
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Gerard C. Herman^ & A. P. E. ten Kroode** & Jose M. Carcione* (...)
Richardson's Dream: The Emergence of Scientific Weather Forecasting
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Remote Sensing Digital Image Analysis An Introduction
John A. Richards & Xiuping Jia
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Quantitative Modeling of Earth Surface Processes
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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. ... & minerals as a function of pressure & temperature. Notably, this work was pioneered over several decades ... & experimental studies, however, a greater understanding of the ... & Birch (1938). These insights into the equations of state of ... & author & Elasticity & the Constitution of the Earth's Interior, (...)