Unit 4 GPS infinitesimal strain analysis presentation

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Using Velocities from a Triangle of GPS Sites to Investigate Crustal Strain UNAVCO GPS Crustal Strain Curriculum Team September 9, 2012

Transcript of Unit 4 GPS infinitesimal strain analysis presentation

Page 1: Unit 4 GPS infinitesimal strain analysis presentation

Using Velocities from a Triangle of GPS Sites to

Investigate Crustal Strain

UNAVCO GPS Crustal Strain Curriculum Team

September 9, 2012

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September 9, 2012

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September 9, 2012 Locate three non-colinear GPS sites

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September 9, 2012 E-W and N-S components of sites’ velocities

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September 9, 2012 E-W + N-S components = total site velocity

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September 9, 2012 Total site velocities

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September 9, 2012 Define the triangle between the GPS sites

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September 9, 2012 Define the centroid of the triangle

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Transform coordinate system to a new origin at the centroid of the triangle

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Inscribe a circle in the center of the undeformed triangle

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The average of the three total site velocities is the translation vector

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The triangle deforms as it moves. The vector from the centroid of the undeformed triangle to the centroid of the deformed triangle is

the same as the translation vector.

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Subtracting the translation vector from the site velocities brings the two triangle centroids together.

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Subtracting the translation vector from the site velocities brings the two triangle centroids together.

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The total site velocities minus the translation vector yields the site vectors associated with the change in shape of the triangle.

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The red line is the major axis of the strain ellipse, and the blue line is the minor axis

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The ellipse axes remain perpendicular to each other when the strain is reversed.

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The rotational component of strain is indicated by the angular change in the orientation of the red lines.

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September 9, 2012