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  2. K–Ar dating - Wikipedia

    en.wikipedia.org/wiki/K–Ar_dating

    Clay minerals are less than 2 μm thick and cannot easily be irradiated for Ar–Ar analysis because Ar recoils from the crystal lattice. In 2013, the K–Ar method was used by the Mars Curiosity rover to date a rock on the Martian surface, the first time a rock has been dated from its mineral ingredients while situated on another planet. [11] [12]

  3. Radiometric dating - Wikipedia

    en.wikipedia.org/wiki/Radiometric_dating

    [2] [3] Radiometric dating is now the principal source of information about the absolute age of rocks and other geological features, including the age of fossilized life forms or the age of Earth itself, and can also be used to date a wide range of natural and man-made materials.

  4. K–Ca dating - Wikipedia

    en.wikipedia.org/wiki/K–Ca_dating

    Potassium–calcium dating, abbreviated K–Ca dating, is a radiometric dating method used in geochronology. It is based upon measuring the ratio of a parent isotope of potassium (40 K) to a daughter isotope of calcium (40 Ca). [1] This form of radioactive decay is accomplished through beta decay. Calcium is common in many minerals, with 40

  5. Potassium-40 - Wikipedia

    en.wikipedia.org/wiki/Potassium-40

    Potassium-40 is especially important in potassium–argon (K–Ar) dating. Argon is a gas that does not ordinarily combine with other elements. So, when a mineral forms – whether from molten rock , or from substances dissolved in water – it will be initially argon-free, even if there is some argon in the liquid.

  6. Isotopes of potassium - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_potassium

    Ar is used in potassium-argon dating of rocks. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic 40 Ar that has accumulated. Typically, the method assumes that the rocks contained no argon at the time of formation and all subsequent radiogenic argon (i.e., 40 Ar) was retained. [citation needed] 40

  7. Sanidine - Wikipedia

    en.wikipedia.org/wiki/Sanidine

    Sanidine is found most typically in felsic volcanic rocks such as obsidian, rhyolite and trachyte. Sanidine crystallizes in the monoclinic crystal system. Orthoclase is a monoclinic polymorph stable at lower temperatures. At yet lower temperatures, microcline, a triclinic polymorph of potassium feldspar, is stable.

  8. 30 Intriguing Posts From This Page Dedicated To Ancient History

    www.aol.com/mysteries-marvels-past-70-posts...

    Picture this: a tomb hiding a jaw-dropping 5,000-year-old dagger made from rock crystal, stretching about 8.7 inches of pure craftsmanship, complete with an opulent ivory hilt and sheath.

  9. Absolute dating - Wikipedia

    en.wikipedia.org/wiki/Absolute_dating

    One of the most widely used is potassium–argon dating (K–Ar dating). Potassium-40 is a radioactive isotope of potassium that decays into argon-40. The half-life of potassium-40 is 1.3 billion years, far longer than that of carbon-14, allowing much older samples to be dated. Potassium is common in rocks and minerals, allowing many samples of ...