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...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριος συγγραφέας: Groshong, Richard H. (Συγγραφέας)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2006.
Έκδοση:Second Edition.
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
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100 1 |a Groshong, Richard H.  |e author. 
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 Second Edition. 
264 1 |a Berlin, Heidelberg :  |b Springer Berlin Heidelberg :  |b Imprint: Springer,  |c 2006. 
300 |a XVI, 400 p.  |b online resource. 
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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 Earth sciences. 
650 0 |a Geology. 
650 0 |a Structural geology. 
650 0 |a Geotechnical engineering. 
650 1 4 |a Earth Sciences. 
650 2 4 |a Geology. 
650 2 4 |a Structural Geology. 
650 2 4 |a Geotechnical Engineering & Applied Earth Sciences. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer eBooks 
776 0 8 |i Printed edition:  |z 9783540310549 
856 4 0 |u http://dx.doi.org/10.1007/978-3-540-31055-6  |z Full Text via HEAL-Link 
912 |a ZDB-2-EES 
950 |a Earth and Environmental Science (Springer-11646)