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文档格式:PPT 文档大小:5.75MB 文档页数:27
Determination of the relative movement of the two walls from the tension joints
文档格式:PPT 文档大小:3.73MB 文档页数:24
TERMINOLOGY FOR DISPLACEMENT a is the rake angle
文档格式:PPT 文档大小:8.23MB 文档页数:45
Main Bedding Types Bedding Shape level bedding ripple bedding Main Types of plate laminae
文档格式:PPT 文档大小:1.44MB 文档页数:18
Review Show the homework and note book on your desk Practise measurement of attitude of planes and lines in the models
文档格式:PPT 文档大小:11.23MB 文档页数:26
Determination of the top sur faces of the beds from the scour surfaces
文档格式:PPT 文档大小:12.01MB 文档页数:27
Chapter 2 Primary Sedimentary Structures Main types of bedding Determination of younger direction of beds from primary structures Types of stratigraphic break Angular unconformity Soft sedimentary structures
文档格式:PPT 文档大小:0.98MB 文档页数:21
Chapter One Introduction Goals Outline Two supports Types of structures QA uantitative techniques pplication Suggestion
文档格式:PPTX 文档大小:2.27MB 文档页数:70
西安石油大学油气资源学院:《地震勘探原理 Seismic Survey Principle》课程教学资源(PPT课件讲稿)第五章 共反射点叠加法(共反射点时距曲线方程、多次反射波的特点、多次叠加的特性)
文档格式:PPT 文档大小:1.51MB 文档页数:25
Strain Displacement Strain Strain field Strain determination in rocks
文档格式:PPT 文档大小:2.79MB 文档页数:22
Review: 1.What is the orientation relationship between maximum shear stresses and principal stresses? 2. What are trajectories of principal stresses?
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