Results 281 to 290 of about 36,759 (336)
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Spatial analysis of lineaments
Computers & Geosciences, 1994Abstract This paper describes a program that will perform some simple spatial analysis of lineaments, and which is useful particularly for lineaments that are arranged as parallel sets. The lineaments may be geological faults, drumlins, linear sand dunes, or any other phenomena that can be mapped as single line-elements.
Chris D. Clark, Colin Wilson
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2003
If we hope to identify the perpetrator of the Piltdown fraud, or to get near doing so, we may begin with some quite obvious questions. This may help us to sketch out what manner of man we are dealing with and perhaps give us a few clues. How could the faked jaw have been obtained? We can at once dispose of the notion that any difficulty would have been
J. S. Weiner, Chris Stringer
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If we hope to identify the perpetrator of the Piltdown fraud, or to get near doing so, we may begin with some quite obvious questions. This may help us to sketch out what manner of man we are dealing with and perhaps give us a few clues. How could the faked jaw have been obtained? We can at once dispose of the notion that any difficulty would have been
J. S. Weiner, Chris Stringer
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Hybrid extraction of tectonic lineaments from digital elevation model
Applied Geomatics, 2022Andongma W. Tende +4 more
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Mapping and validating lineaments
The Leading Edge, 2015Data enhancement can help to emphasize edges that correspond to contrasts in acoustic impedance, magnetic susceptibility, or bulk density. Such contrasts often indicate the presence of important geologic boundaries. Emphasizing the edges can help with mapping and interpretation of those boundaries.
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Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1986
Fluid infiltration into fault zones and their deeper level counterparts, brittle-ductile shear zones, is examined in five different tectonic environments. In the 2.7 Ga Abitibi Greenstone Belt major tectonic discontinuities have lateral extents of hundreds of kilometres.
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Fluid infiltration into fault zones and their deeper level counterparts, brittle-ductile shear zones, is examined in five different tectonic environments. In the 2.7 Ga Abitibi Greenstone Belt major tectonic discontinuities have lateral extents of hundreds of kilometres.
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Journal of the Indian Society of Remote Sensing, 2020
Kamini Singh, A. Arya, K. K. Agarwal
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Kamini Singh, A. Arya, K. K. Agarwal
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