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11.11.2015

Upgrade Helps NASA Study Mineral Veins on Mars

Diverse composition of mineral veins at the "Garden City" site investigated by NASA's Curiosity Mars rover suggests multiple episodes of groundwater activity.

Veiny 'Garden City' Site and Surroundings on Mount Sharp, Mars
Veiny 'Garden City' Site and Surroundings on Mount Sharp, Mars
This view from the Mast Camera (Mastcam) on NASA's Curiosity Mars rover shows a site with a network of prominent mineral veins below a cap rock ridge on lower Mount Sharp. Credit:NASA/JPL-Caltech/MSSS

Scientists now have a better understanding about a site with the most chemically diverse mineral veins NASA's Curiosity rover has examined on Mars, thanks in part to a valuable new resource scientists used in analyzing data from the rover.

Curiosity examined bright and dark mineral veins in March 2015 at a site called "Garden City," where some veins protrude as high as two finger widths above the eroding bedrock in which they formed.

The diverse composition of the crisscrossing veins points to multiple episodes of water moving through fractures in the bedrock when it was buried. During some wet periods, water carried different dissolved substances than during other wet periods. When conditions dried, fluids left clues behind that scientists are now analyzing for insights into how ancient environmental conditions changed over time.

'Garden City' Vein Complex on Lower Mount Sharp, Mars
'Garden City' Vein Complex on Lower Mount Sharp, Mars
Credit:NASA/JPL-Caltech/MSSS

"These fluids could be from different sources at different times," said Diana Blaney, a Curiosity science team member at NASA's Jet Propulsion Laboratory, Pasadena, California. "We see crosscutting veins with such diverse chemistry at this localized site. This could be the result of distinct fluids migrating through from a distance, carrying chemical signatures from where they'd been."

Researchers used Curiosity's laser-firing Chemistry and Camera (ChemCam) instrument to record the spectra of sparks generated by zapping 17 Garden City targets with the laser. The unusually diverse chemistry detected at Garden City includes calcium sulfate in some veins and magnesium sulfate in others. Additional veins were found to be rich in fluorine or varying levels of iron.

As researchers analyzed Curiosity's observations of the veins, the ChemCam team was completing the most extensive upgrade to its data-analysis toolkit since Curiosity reached Mars in August 2012. They more than tripled -- to about 350 -- the number of Earth-rock geochemical samples examined with a test version of ChemCam. This enabled an improvement in their data interpretation, making it more sensitive to a wider range of possible composition of Martian rocks.

Blaney said, "The chemistry at Garden City would have been very enigmatic if we didn't have this recalibration."

Thick, Dark Veins at 'Garden City,' Mars
Thick, Dark Veins at 'Garden City,' Mars
Credit: NASA/JPL-Caltech/LANL/CNES/IRAP/LPGNantes/CNRS/IAS

The Garden City site is just uphill from a mudstone outcrop called "Pahrump Hills," which Curiosity investigated for about six months after reaching the base of multi-layered Mount Sharp in September 2014. The mission is examining ancient environments that offered favorable conditions for microbial life, if Mars has ever hosted any, and the changes from those environments to drier conditions that have prevailed on Mars for more than 3 billion years. Curiosity has found evidence that base layers of Mount Sharp were deposited in lakes and rivers. The wet conditions recorded by the Garden City veins existed in later eras, after the mud deposited in lakes had hardened into rock and cracked.

Eye-catching geometry revealed in images of the veins offers additional clues. Younger veins continue uninterrupted across intersections with veins that formed earlier, indicating relative ages.

ChemCam provides the capability of making distinct composition readings of multiple laser targets close together on different veins, rather than lumping the information together. The chemistry of these veins is also related to mineral alteration observed at other places on and near Mount Sharp. What researchers learned here can be used to help understand a very complex fluid chemical history in the region. Since leaving Garden City, Curiosity has climbed to higher, younger layers of Mount Sharp.

Dark, Thin Fracture-Filling Material
Dark, Thin Fracture-Filling Material
Credit: NASA/JPL-Caltech/LANL/CNES/IRAP/LPGNantes/CNRS/IAS

Today, Blaney presented findings from ChemCam's Garden City investigations at the annual meeting of the American Astronomical Society's Division for Planetary Science, in National Harbor, Maryland.

The U.S. Department of Energy's Los Alamos National Laboratory in Los Alamos, New Mexico, developed ChemCam in partnership with scientists and engineers funded by the French national space agency. More information is available at:

http://www.msl-chemcam.com

NASA's Jet Propulsion Laboratory built Curiosity and manages the project for NASA's Science Mission Directorate in Washington. For more the mission, visit:

http://www.nasa.gov/msl
http://mars.nasa.gov/msl

You can follow the mission on Facebook and Twitter at:

http://www.facebook.com/marscuriosity
http://www.twitter.com/marscuriosity

2015-345

Guy Webster
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-6278
guy.webster@jpl.nasa.gov

Dwayne Brown / Laurie Cantillo
Headquarters, Washington
202-358-1726 / 202-358-1077
dwayne.c.brown@nasa.gov/ laura.l.cantillo@nasa.gov


All Related Images
  • This March 27, 2015, view from the Mast Camera (Mastcam) on NASA's Curiosity Mars rover shows a site with a network of prominent mineral veins below a cap rock ridge on lower Mount Sharp. At this "Garden City" site, the veins have been more resistant to erosion than the surrounding host rock.
    Veiny 'Garden City' Site and Surroundings on Mars
  • This March 27, 2015, view from the Mast Camera (Mastcam) on NASA's Curiosity Mars rover shows a site with a network of prominent mineral veins below a cap rock ridge on lower Mount Sharp. At this "Garden City" site, the veins have been more resistant to erosion than the surrounding host rock.
    Veiny 'Garden City' Site and Surroundings on Mars
  • Prominent mineral veins at the "Garden City" site examined by NASA's Curiosity Mars rover vary in thickness and brightness, as seen in this image from Curiosity's Mast Camera (Mastcam). The image covers and area roughly 2 feet across.
    'Garden City' Vein Complex on Lower Mount Sharp, Mars
  • These images and overlay bar charts from the Chemistry and Camera (ChemCam) instrument on NASA's Curiosity Mars rover indicate where some high-potassium material is localized within mineral veins at "Garden City."
    Dark, Thin Fracture-Filling Material
  • These images from the Chemistry and Camera (ChemCam) instrument on NASA's Curiosity Mars rover indicate similarly dark material, but with very different chemistries, in mineral veins at "Garden City."
    Thick, Dark Veins at 'Garden City,' Mars
  • This view from the Mars Hand Lens Imager (MAHLI) on the arm of NASA's Curiosity Mars rover shows texture within a light-toned vein at a site called "Garden City" on lower Mount Sharp.
    Crystal Growth Texture in Light Vein at 'Garden City'
  • Light material emplaced within darker vein material is seen in this view of a mineral vein at the "Garden City" site on lower Mount Sharp, Mars. The Mars Hand Lens Imager (MAHLI) on the arm of NASA's Curiosity Mars Rover took the image on April 4, 2015. The area shown is roughly 0.4 inch wide.
    Injection of Light Material into an Older Dark Vein
  • This view from the Mars Hand Lens Imager (MAHLI) on the arm of NASA's Curiosity Mars rover shows a combination of dark and light material within a mineral vein at a site called "Garden City" on lower Mount Sharp. The image was taken on April 4, 2015, and covers an area roughly 1 inch wide.
    Light Material Ripped Up Older Dark Vein Material
Credit: NASA/JPL-Caltech

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