Titlebook: Geological maps: An Introduction; Alex Maltman Book 1990 Alex Maltman 1990 document.information.remote sensing.time

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Igneous and metamorphic rocks; mineral deposits,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It

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Geological history from maps,geological past. For the outcrop patterns on maps can reveal much of how the rock arrangements evolved through time; they enable interpretations to be made on the geological history of the map area, even the reconstruction of past geological environments. The timings that are derived from maps are u

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Die trigonometrische Parametrisierung,e patterns on the map record the relationships between the rocks, from which the geologist can deduce much about their arrangement underground and about their geological history. This book is aimed at helping you develop these interpretive skills.

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Innenansichten der Gelehrtenrepublik,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It is with these that this chapter is concerned.

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https://doi.org/10.1007/978-3-662-43117-7e of what goes into their production. Many stages are involved, from the detailed field surveying required for large-scale maps, through the preparation of ‘fair copy maps’, and the design and execution of a final printed version. Greenly and Williams (1930, p. 99) list twenty-three steps; this chapter merely outlines what is involved.