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3-D Structural Geology A Practical Guide to Quantitative Surface and Subsurface Map Interpretation /

Geological structures are three dimensional, yet are typically represented by, and - terpreted from, outcrop maps and structure contour maps, both of which are curved two-dimensional surfaces. Maps plus serial sections, called 2½-D, provide a closer approach to three dimensionality. Computer technol...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Groshong, Richard H. (Autor)
Autor Corporativo: SpringerLink (Online service)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2006.
Edición:2nd ed. 2006.
Temas:
Acceso en línea:Texto Completo

MARC

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100 1 |a Groshong, Richard H.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
245 1 0 |a 3-D Structural Geology  |h [electronic resource] :  |b A Practical Guide to Quantitative Surface and Subsurface Map Interpretation /  |c by Richard H. Groshong. 
250 |a 2nd ed. 2006. 
264 1 |a Berlin, Heidelberg :  |b Springer Berlin Heidelberg :  |b Imprint: Springer,  |c 2006. 
300 |a XVI, 400 p.  |b online resource. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
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347 |a text file  |b PDF  |2 rda 
505 0 |a Elements of Map-Scale Structure -- Location and Attitude -- Structure Contouring -- Thickness Measurements and Thickness Maps -- Fold Geometry -- Cross Sections, Data Projection and Dip-Domain Mapping -- Properties of Faults -- Faulted Surfaces -- Dip-Sequence Analysis -- Quality Control -- Structural Validation, Restoration, and Prediction -- Direction Cosines and Vector Geometry. 
520 |a Geological structures are three dimensional, yet are typically represented by, and - terpreted from, outcrop maps and structure contour maps, both of which are curved two-dimensional surfaces. Maps plus serial sections, called 2½-D, provide a closer approach to three dimensionality. Computer technology now makes it possible for geological interpretations to be developed from the beginning in a fully three dim- sional environment. Fully 3-D geological models allow significantly better interpre- tions and interpretations that are much easier to share with other geologists and with the general public. This book provides an overview of techniques for constructing structural interpretations in 2-D, 2½-D and 3-D environments; for interpolating - tween and extrapolating beyond the control points; and for validating the final int- pretation. The underlying philosophy is that structures are three-dimensional solid bodies and that data from throughout the structure, whether in 2-D or 3-D format, should be integrated into an internally consistent 3-D interpretation. It is assumed that most users of this book will do their work on a computer. C- sequently, the book provides quantitative structural methods and techniques that are designed for use with spreadsheets, mapping software, and three-dimensional c- puter-graphics programs. The book is also intended to provide the background for understanding what interpretive software, for example, a computer contouring p- gram, does automatically. Most techniques are presented in both a traditional format appropriate for paper, pencil, and a pocket calculator, and in quantitative format for use with spreadsheets and computer-graphics or computer-aided-design programs. 
650 0 |a Geology. 
650 0 |a Geotechnical engineering. 
650 1 4 |a Geology. 
650 2 4 |a Geotechnical Engineering and Applied Earth Sciences. 
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776 0 8 |i Printed edition:  |z 9783540819332 
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