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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 <...>
Since time immemorial the minerals, rocks and soil had been the major attraction for the growth, development, and survival of every living entity including human, animals, birds, plants, and trees. That indeed forced us to know more about the minerals (mineralogy) and the rocks and soils (petrology).
We are all familiar with the subdivision of the natural world into the plant, animal, and mineral kingdoms. Of these the realm of minerals is the study and research area of mineralogy. A mineralogist uses the word mineral, however, in a much more restricted sense than prevails with common usage. If we examine a rock rather closely, we notice, for example, that a sandstone is composed of individual quartz grains.
This book is a practical, hands-on introduction to numerical geodynamic modelling for inexperienced people, i.e. for young students and newcomers from other fields. It does not require much background in mathematics or physics and is therefore written with a maximum amount of simple technical details. If you are inexperienced – this book is yours! <...>
This book is a practical, hands-on introduction to numerical geodynamic modelling for inexperienced people, i.e. for young students and newcomers from other fields. It does not require much background in mathematics or physics and is therefore written with a maximum amount of simple technical details. If you are inexperienced – this book is for you! <...>
This book is intended for use in an introductory optical mineralogy course. The objective in preparing the book was to present in a single volume of reasonable size both a thorough treatment of optical theory as it pertains to mineral identification with the petrographic microscope, and detailed mineral descriptions of the common rock-forming minerais. The first seven chapters <leal with optical theory and provide an introduction to the properties oflight, a description of the petrographic microscope, and a discussion of the optical properties of isotropic and anisotropic materiais. Detailed step-by-step procedures have been included to guide students through the measurement of optical properties in both thin section and grain mount. Selected spindle stage techniques also are included. <...>
In some ways light is an enigma. We know that it is a form of energy that is transmitted from one place to another at finite velocity and that it can be detected with the eye. In many ways it behaves as though it were composed of numerous tiny particles that travel bullet-like from one point to another. But it also behaves as though it were a wave phenomena in which the energy moves somewhat like the waves started by dropping a pebble in a pond. Because light behaves in these two seemingly contradictory ways, two different theories, the particle theory and the wave theory, have been developed to explain it. <...>