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ppt geostruk dari kelas geologi dasar untuk teknik geologi, teknik perminyakan, teknik pertambangan
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Program Studi Teknik Geologi Fakultas Teknologi Kebumian dan Energi Universitas Trisakti 2011
Structural Geology study of the “architecture of the crust” ….by examination of deformed rocks DEFORMATION: changes in location, orientation, shape, volume …results from stresses that exceed rock strength… same material (fence) deforms in different ways ductile (bends) brittle (breaks) from: Davis and Reynolds, 1996
rocks, like the fence, will deform in different ways, depending upon the properties of the rock and the nature of the applied stress folds faults
Earth’s Plates
Offset Ditch, Hollist er, CA
Offset Ditch, Hollist er, CA
translation (rigid body) rotation (rigid body) distortion; strain (shape changes) time 1 time 2 kinematic analysis: 4 possible types of movements volume change (dilation, contraction)
from: Davis and Reynolds, 1996 looking at it another way: dilation translation rotation distortion (strain)
Stress-Strain
Shear stress and strain
Structures as a Record of the Geologic Past
Strike and Dip Measuring Folds Other Strain Markers
Steepl y Dippin g Beds, Pt. Arena, Ca