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Explore the complex Geologic Time Scale, which spans from the Precambrian to the Cenozoic era, marking significant events in Earth's history, such as extinctions and mountain-building. Learn about the principles of relative and absolute time, including the significance of fossils, radiometric dating, and the structural geology of faults, folds, and deformation mechanisms. This overview covers essential concepts like brittle and ductile behavior, stress types, and geological maps, providing insights into engineering considerations and seismic hazards linked to geological features.
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Geologic Time Scale • Precambrian — Minimal fossil record • Era, Period, Epoch • Based on major changes — extinctions, mountain building events
Relative Time • Principle of Superposition • Fossil Evidence • Cross Cutting Relationships • Unconformities • Alteration • Fracture Termination
Paleozoic (Old Life) — Brachiopods, Trilobites, Fish • Periods based on English Geology • Cambrian for Latin Wales • Ordovician and Silurian for ancient Welsh Tribes • Devonian for Devon • Carboniferous for Coal Measures (also Mississippian and Pennsylvanian in US) • Permian for Perm Basin in Ukraine
Mesozoic (Middle Life) — Ammonites, Dinosaurs • Triassic based on distinctive three-layer stratigraphy in southern Germany • Jurassic based on Jura Mountains in France and Switzerland • Cretaceous (Latin for Chalk) based on chalk unit that forms Dover’s cliffs
Cenozoic (Recent Life) — Mammals, Modern marine fauna (foraminifera) • Periods are Tertiary (before Ice Ages) and Quaternary (ice ages) • Primary and secondary have been long replaces • Rocks of western Washington are Tertiary and Quaternary
Age of the Earth • Kelvin and a basis in heat flow (set at 20 million years) • Problem of fitting all of evolution in this time • Rutherford and the introduction radioactive decay • Added a head source, pushed ages back to 4.5 billion years
Absolute Time • Basis on radiometric dating (see Rahn chapter 1) • Common dating tools • 14C, K-Ar, Rb-Sr,Uranium decay series
CEE 437Structural Geology • World Stress • Brittle and Ductile Deformation • Faults and Joints • Folds
Representing a Plane • Strike and Dip • Quadrant Convention (N 60 E, 45 SE) • 360o Convention (120, 45) • Right hand rule: dip 90o clockwise of strike) • Pole trend and plunge • Dip vector • does not discriminate strike of vertical planes
Brittle Versus Ductile Behavior • Strain Rate Dependence • Non-elastic Deformation Mechanisms • recrystallization • lattice dislocations • pressure solution and redeposition
Brittle Deformation • Extensile or Shear • Continuum of Joints and Faults • Faults as Strain Concentrators • Internal Structure of Faults
In Situ Stress Measurement • Seismic data • First motions • Stress drops • Hydraulic Fracturing • Overcoring • Borehole Breakouts
Fault Types • Normal — Extensile Deformation • Hanging Wall down • Horsts and Grabens • Reverse — Compressive Deformation • Hanging Wall up • Thrust Faults • Strike-slip • Mostly transform faults
Fault Nomenclature • Hanging wall (overhead) • Footwall (underfoot) • Gouge • Damage Zone • Cataclasite • Mylonite
http://www.geo.cornell.edu/geology/classes/RWA/GS_326/photos/tf/DesertPk.jpghttp://www.geo.cornell.edu/geology/classes/RWA/GS_326/photos/tf/DesertPk.jpg
Fault Gouge http://darkwing.uoregon.edu/~millerm/slides.html
Keystone Thrust, Nevada http://darkwing.uoregon.edu/~millerm/slides.html
Strike Slip Faults, Nevada http://darkwing.uoregon.edu/~millerm/slides.html
Engineering Concerns of Faults • Planes of Weakness • Sources of Seismic Hazard if Active • Significant Water Courses • Significant as Groundwater “Dams”
Folds • Anticline • Concave down or oldest beds at core • Syncline • Concave up or youngest beds at core • Overturned and Recumbent Folds • Fold Terms • Hinge, Axis
Identifying Fold Types • Attitude of beds • Pattern of beds on geologic maps • Anticline — oldest at core • Syncline — youngest at core
Engineering Concerns of Folds • Means of Extrapolating Bed Locations • Fracturing related to folding • Favorable or non-favorable orientations of beds to engineered structures or slopes
Recumbent Folds http://darkwing.uoregon.edu/~millerm/slides.html
Fine-Scale Folding http://darkwing.uoregon.edu/~millerm/slides.html