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The intent of Introduction to Geophysical Fluid Dynamics—Physical and Numerical Aspects is to introduce its readers to the principles governing air and water flows on large terrestrial scales and to the methods by which these flows can be simulated on the computer.
This book discusses how—by analysis of the physical felds and processes within and on the Earth—we learn how old the Earth is, about its internal structure and external form, and about the causes and properties of its magnetic and temperature felds. What will not be discussed are the geophysical survey methods for characterizing the upper crust that are used to explore for mineral ore deposits and hydrocarbon reservoirs; specialized textbooks should be consulted for these.
Most of the natural phenomena we study are variable both in space and time. Considering a topographic surface or a groundwater contamination one can observe high variability within small distances. The variability is a result of natural processes, thus deterministic. As most of these processes are sensitive and the conditions under which the they took place are not fully known, it is not possible to describe them based on physical and chemical laws completely. <...>
This book grew out of class notes for a course that served two purposes: 1. To familiarize graduate students in hydrogeology and environmental engineering with some practical methods for solving interpolation and related estimation problems. The course emphasized geostatistical methods. 2. To illustrate how one may use data to develop empirical models, that is, to provide an introduction to applied statistical modeling.
The process of metamorphism is one of change, and within the mineral assemblage and texture of a metamorphic rock is a memory of that change. The transformations are brought about by geological processes from the global plate tectonic level to the more localised scale. In view of this, recovering the memory of the change locked in metamorphic rocks helps to constrain geological processes well back into the Earth's history.
A large economic mineral deposit, e.g. 200 Mt underlying an area of 2 km2, is minute in comparison with the Earth’s crust and in most countries the easily found deposits cropping out at the surface have nearly all been found. The deposits for which we now search are largely concealed by weathered and leached outcrops, drift, soil, or some other cover, and sophisticated exploration methods are required to find them. The target material is referred to as a mineral deposit, unless we use a more specific term such as coal, gas, oil, or water. Mineral deposits contain mineral resources. What sort of mineral deposit should we seek? To answer this question it is necessary to have some understanding of mineral economics. <...>
This book was written to provide a comprehensive text for teaching mineralogy to undergraduate students in the geosciences. Mineralogy is an essential because all geoscientists continually deal directly or indirectly with minerals in their professional work.
Almost every human endeavor is influenced by minerals. Many natural resources used in the manufacture of goods on which civilization and our lives depend begin as minerals in the ground. The crops that we eat are grown in soil composed of minerals. The safety and stability of structures such as buildings, roads, and bridges depend on the mechanical properties of the minerals that make up the rocks and soil on which they are built. In addition, the chemical composition, structure, and texture of the minerals that compose the rocks beneath our feet provide myriad clues that guide geoscientists as they attempt to decipher the history of the earth.
The crust of the Earth and underlying relatively rigid mantle make up the lithosphere. The crust is composed of a great variety of minerals and rocks. More than 80% of all raw materials that are used in various sectors of economy, society and the environment are of mineral origin, and demand for them is greater every day. In most countries, the values of raw materials used for the metal industry and building materials exceed the value of the funds allocated for oil and gas, although, we hear more about oil and gas <...>