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The reflectance spectra of opal-A (05-22 µm) from the Taupo Volcanic Zone: spectra that may identify hydrothermal systems on planetary systems
Download2004-01-01
Goryniuk, Michelle C., Rivard, Benoit A., Jones, Brian
Opal‐A, the main component of siliceous sinters in many terrestrial hydrothermal systems, is a hydrated silicate that commonly incorporates silicified microorganisms. The detection of opal‐A on the surface of Mars, therefore, may carry important implications in the search for extraterrestrial...
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