folds and faults in geology pdf


Folds and Faults - soest.hawaii.edu

Domes and basins result from plate tectonic forces in continental interiors. Page 15. Where's the oldest material? Page 16. Domes and Basins. Page 17. How do

Joints, Folds, and Faults - SOEST Hawaii

Rocks in the Crust Are Bent, Stretched, and Broken … Strain occurs in 3 stages: elastic deformation, ductile deformation, brittle deformation Strain is the change in shape and or volume of a rock caused by Stress. Dip-Slip and Strike-Slip Faults Are the Most Common Types of Faults.

Joints, Folds, and Faults

Rocks in the Crust Are Bent, Stretched, and Broken … Strain occurs in 3 stages: elastic deformation, ductile deformation, brittle deformation Strain is the change in shape and or volume of a rock caused by Stress. Dip-Slip and Strike-Slip Faults Are the Most Common Types of Faults.

Structural Geology

Folds in rocks range from microscopic to hundreds of kilometers across. Faults are fractures along which displacement has occurred. Rocks deform when applied stress exceeds rock strength. Deformation may be ductile flow or brittle fracture.

Geology 3015 Lecture Notes Week 7a.pdf

fracturing, folding, and faulting of rocks. Processes that cause . deformation is a geologic structure, especially fractures, folds, and faults. • Folding occurs in

Faults and Folds Geological Structures - The Geological Society of

Leung Kar Fai. Vale Exploration Geologist. Geological Society of Hong Kong. Faults and Folds. Geological Structures. Geological Structures.

GEOLOGIC STRUCTURES

Patagonian Andes, Argentina. GEOLOGIC STRUCTURES. • Stress and Strain. • Active deformation along faults. • Geologic maps and cross sections. • Folding.

Introduction to Structural Geology - for ES109 Week 3

Reverse and Thrust. Faults. Strike-slip faults. Identifying faults on maps and in the field. Fault Rocks. Folds. Special types. Introduction to Structural Geology - for.

Introduction to Faults

were transferred to geology in its early days, despite the fact that the mining .. che fault surface, the formacion of drag folds is less likely. D. Rollover anticline in

Chapter 10 – Crustal Deformation

AKA – Structural geology. (adapted the surface as folds and faults Folds. • How do rocks fold? • Ductile deformation. • What environments lead to ductile.