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Sediments and Sedimentary Rocks
2018We are on more familiar ground in this chapter, looking at processes and materials found in the world all around us. Even the names of sedimentary rocks are well known—sandstone, shale, limestone, and so on. Clearly, these materials are highly relevant to vineyard geology because more than three-quarters of the land surface is sedimentary in origin ...
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Diffusivity in sedimentary rocks
Magnetic Resonance Imaging, 2007U. Mayer +3 more
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Nature, 1961
Microscopic Sedimentary Petrography By Prof. Albert V. Carozzi Pp. viii + 485. (New York: John Wiley and Sons, Inc.; London: Chapman and Hall, Ltd., 1960.) 92s. net.
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Microscopic Sedimentary Petrography By Prof. Albert V. Carozzi Pp. viii + 485. (New York: John Wiley and Sons, Inc.; London: Chapman and Hall, Ltd., 1960.) 92s. net.
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The Morphology of Sedimentary Rocks
1987The formation of sedimentary rocks in sedimentary basins can be described as follows. Rock grains - formed by erosion, sand, dust, or skeletons of marine animals - fall to the bottom of a body of water overlying the sedimentary basin. This process of sedimentation buries earlier sediments which descend downward into the earth as the process continues ...
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1993
Abstract Over vast areas of the undeformed platform of southwestern Canada, the sedimentary cover of the ancient North American Craton is entirely of Phanerozoic age. In northwestern Canada, on the other hand, thick Proterozoic strata intervene between Phanerozoic deposits and crystalline basement (Fig. 4A.1).
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Abstract Over vast areas of the undeformed platform of southwestern Canada, the sedimentary cover of the ancient North American Craton is entirely of Phanerozoic age. In northwestern Canada, on the other hand, thick Proterozoic strata intervene between Phanerozoic deposits and crystalline basement (Fig. 4A.1).
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Microstructures of sedimentary rocks
2004Introduction Although this book is mainly concerned with igneous, metamorphic and deformation processes, in this chapter I briefly review the main sedimentary microstructures, partly because they need to be understood in order to interpret residual sedimentary microstructures in some metamorphic rocks.
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