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  1. Martian meteorite NWA 7034, nicknamed "Black Beauty," weighs approximately 320 g (11 oz). [2] A Martian meteorite is a rock that formed on Mars, was ejected from the planet by an impact event, and traversed interplanetary space before landing on Earth as a meteorite. As of September 2020, 277 meteorites had been classified as Martian, less than ...

    • 277 as of 15 September 2020[update]
    • Achondrite
  2. Allan Hills 84001. /  76.92028°S 156.77361°E  / -76.92028; 156.77361. Allan Hills 84001 ( ALH84001 [1]) is a fragment of a Martian meteorite that was found in the Allan Hills in Antarctica on December 27, 1984, by a team of American meteorite hunters from the ANSMET project. Like other members of the shergottite – nakhlite ...

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  4. Found date. 2011. TKW. 320 grams (11 oz) [1] Northwest Africa 7034 is a Martian meteorite believed to be the second oldest yet discovered. [4] It is estimated to be two billion years old and contains the most water of any Martian meteorite found on Earth. [5] Although it is from Mars it does not fit into any of the three SNC meteorite ...

    • Martian (basaltic breccia)
    • Achondrite
  5. Aug 20, 2014 · Tissint fragment. (Image credit: Heritage Auctions) This fragment of the Tissint meteorite, which fell in Morocco in 2011, was auctioned off for $43,750. The 1.6-ounce (46-gram) rock, like others ...

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  6. Jul 12, 2022 · The Mars Meteorite Compendium (MMC) is an attempt to introduce these rocks to new investigators and give. Figure 1. Log-log comparison of Vikingmeasured Mars atmosphere to trapped gases in EETA79001 glass. Figure from Pepin (1985), Nature 317, 473. specialists a view of what is being learned by their colleagues in different fields.

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  7. Jul 12, 2022 · An image of the Martian meteorite nicknamed "Black Beauty." (Image credit: NASA) The scientists identified 19 craters as the most likely points of origin for the Martian meteorites on Earth. When ...

  8. Feb 1, 2022 · The Allan Hills 84001 (ALH 84001) martian meteorite is an approximately four billion-year-old igneous rock composed primarily of the mineral orthopyroxene. It was discovered in Antarctica in 1984 and subsequently studied for its record of the early geological history of Mars.

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