Titlebook: 3-D Structural Geology; A Practical Guide to Richard H. Groshong Textbook 19991st edition Springer-Verlag Berlin Heidelberg 1999 fault.faul

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Acute Exacerbation of Chronic Hepatitis Be that agrees with all the data. This can be difficult or ambiguous because the complete structure is usually undersampled. Thus an interpretation of the complete geometry will probably require a significant number of inferences, as, for example, in the interpolation of a folded surface between the

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Christian Stevoff MD,Ikuo Hirano MDlt maps with horizon maps, mapping the displacement transfer zones between faults, mapping cross-cutting faults, and interpreting faults from isopach maps. The topics are covered in the sequence normally followed in order to define, map, and validate the interpretations of faults and faulted horizon

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Gregory M. Bolduc MD,David A. Peura MDnterprétation. This makes a cross section a powerful tool for checking and improving the structural interprétation presented on a map. Poorly controlled map horizons may be improved with information from other horizons. Errors in mapping on one horizon can be recognized as incompatibilities with the

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Textbook 19991st editionare based on geo- logical maps. Because a map-scale structure is never completely sampled in three dimensions, geological maps and the cross sections derived from maps are always interpretations. The interpretation may be complicated by direct structural observati- ons,likebedding attitudes,that are

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