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Titlebook: 3-D Structural Geology; A Practical Guide to Richard H. Groshong Textbook 2006Latest edition Springer-Verlag Berlin Heidelberg 2006 Fundame

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期刊全稱3-D Structural Geology
期刊簡(jiǎn)稱A Practical Guide to
影響因子2023Richard H. Groshong
視頻videohttp://file.papertrans.cn/101/100636/100636.mp4
發(fā)行地址Enables readers/users to produce better geological maps and cross sections, judge the quality of existing maps, and locate and fix mapping errors..Focus on applied topics.Logical order of text followi
圖書封面Titlebook: 3-D Structural Geology; A Practical Guide to Richard H. Groshong Textbook 2006Latest edition Springer-Verlag Berlin Heidelberg 2006 Fundame
影響因子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 2?-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, 2?-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 struct
Pindex Textbook 2006Latest edition
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Textbook 2006Latest editionwhich are curved two-dimensional surfaces. Maps plus serial sections, called 2?-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 geolog
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Epistemic Entrenchment and Its RelativesThis chapter focuses on the recognition of faults, their geometrical properties, displacement distributions, and the correlation of multiple fault cuts into continuous fault surfaces. Unconformities are treated here because, by truncating units at the map scale, they share characteristics with faults and need to be distinguished from faults.
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Credulous Nonmonotonic InferenceThis chapter covers how to construct maps containing faults, the integration of fault maps with horizon maps, interpreting faults from isopach maps, mapping overlapping and intersecting faults, and mapping cross-cutting faults.
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