GLG310 Structural Geology Force, Stress, and Strength [start reading Chapter 3] • • • • • • • Introduction Dynamic analysis Force Tractions Stress Relationships between stress and strain Deformation experiments 11 March 2016 GLG310 Structural Geology Structural Geology • Introduces the physical side of Geological Sciences and emphasizes – Geometry (shape, orientation, position, size, etc.) – Motion (beginning and ending positions and paths of particles and bodies—deformation or change in geometry) – Mechanics (explanations of why the geometry and motion are how they are) 3/11/2016 GLG310 Structural Geology http://gdavis.web.arizona.edu/node/105 Geometric and kinematic description Structural Analysis • Descriptive Analysis – Recognize and describe structures and measure their locations, geometries and orientations • Scale, Structural Elements • Kinematic Analysis – Focus on motion of materials • Dynamic Analysis – Interpret motions in terms of applied forces 4 September 2012 GLG310 Structural Geology Physical Models Simulate earth processes in a controlled experiment Build intuition versus actual prediction Identify controlling processes or conditions http://www.youtube.com/watch?v=A5hC47RGq0Y 11 March 2016 GLG310 Structural Geology http://www.youtube.com/watch?v=xDQRfNEBR2w 11 March 2016 GLG310 Structural Geology Mechanics • Develop simple rules to explain behavior • Can be stated in symbolic or mathematical terms 11 March 2016 GLG310 Structural Geology Isaac Newton Sir Isaac Newton was an English physicist, mathematician, astronomer, natural philosopher, alchemist and theologian, who has been "considered by many to be the greatest and most influential scientist who ever lived.” F=mA 11 March 2016 Philosophiæ Naturalis Principia Mathematica, often referred to as simply the Principia, is a work in three books by Sir Isaac Newton, first published 5 July 1687 GLG310 Structural Geology Force: Newton’s Laws of Motion • Law I: Every body continues in its state of rest, or in uniform motion in a straight line, unless it is compelled to change its state by forces impressed upon it. 11 March 2016 GLG310 Structural Geology http://www.poolplayers.com/instruction/terry-bell/2011/04/billiardsmaster-class-9-approach-and-procedure/ 1:25 cue ball to pool ball force transfer Force: Newton’s Laws of Motion • Law II: The rate of change of momentum is proportional to the impressed force and is made in the direction in which the force is impressed. 11 March 2016 GLG310 Structural Geology 11 March 2016 GLG310 Structural Geology Force: Newton’s Laws of Motion Dimensional analysis: fundamental units Mass = amount of material in a body Weight = Force due to gravity action on a body 1 liter of water has a mass of on earth it weighs on the moon it weighs 11 March 2016 GLG310 Structural Geology 11 March 2016 GLG310 Structural Geology What does a Newton feel like? http://www.youtube.com/watch?v=LOINRpWGrlw What does a Newton feel like? -Davis and Reynolds (vo. 2), p. 101 11 March 2016 GLG310 Structural Geology Force: Forces as vectors use the tip-to-tail method to find the resultant force http://www.hk-phy.org/contextual/ http://www.hk-phy.org/contextual/mechanics/for/add_force/resultant_force_e.html Block mass is 10000 kg What is normal and shear force along base? Dip is 10 degrees. 11 March 2016 GLG310 Structural Geology Force: Newton’s Laws of Motion • Law III: To every action there is always opposed an equal reaction, or the mutual actions of two bodies on each other are always equal in magnitude and opposite in direction http://www.hk-phy.org/contextual/ Force: Newton’s Laws of Motion • Law III: To every action there is always opposed an equal reaction, or the mutual actions of two bodies on each other are always equal in magnitude and opposite in direction Equilibrium 11 March 2016 GLG310 Structural Geology Driving and resisting forces of plate tectonics