Status Report

NASA Mars Odysey THEMIS Image: Relative Dating Via Fractures

By SpaceRef Editor
April 1, 2005
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Medium image for 20050401a

Image Context:

Context image for 20050401a
Context image credit: NASA/Mars Orbiter Laser Altimeter (MOLA) Team
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ParameterValue ParameterValue
Latitude12.4 &nbsp InstrumentVIS
Longitude284.9E (75.1W) &nbsp Resolution (m)36
Image Size (pixels)6588×1338 &nbsp Image Size (km)237.2×48.2



This VIS image of the eastern part of the Tharsis region

illustrates how fractures can be used in relative dating

of a surface. The fractured materials on the right side

of the image are embayed by younger volcanic flows originating

to the west of the image. Note how the younger flows

cover the ends of the fractures, and are not at all fractured

themselves.


[Source: ASU THEMIS Science Team]


Note: this THEMIS visual image has not been radiometrically nor geometrically calibrated for this preliminary release. An empirical correction has been performed to remove instrumental effects. A linear shift has been applied in the cross-track and down-track direction to approximate spacecraft and planetary motion. Fully calibrated and geometrically projected images will be released through the Planetary Data System in accordance with Project policies at a later time.


NASA’s Jet Propulsion Laboratory manages the 2001 Mars Odyssey mission for NASA’s Office of Space Science, Washington, D.C. The Thermal Emission Imaging System (THEMIS) was developed by Arizona State University, Tempe, in collaboration with Raytheon Santa Barbara Remote Sensing. The THEMIS investigation is led by Dr. Philip Christensen at Arizona State University. Lockheed Martin Astronautics, Denver, is the prime contractor for the Odyssey project, and developed and built the orbiter. Mission operations are conducted jointly from Lockheed Martin and from JPL, a division of the California Institute of Technology in Pasadena.

Image Credit: NASA/JPL/Arizona State University


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