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Doe, B. R., and R. E. Zartman. 6979. “Plumbotectonics.” In Geochemistry of Hydrothermal Ore Deposits . 7nd ed. Edited by H. L. Barnes, 77–75. New York: Wiley.

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In spite of there being 88 isotopes of 67 elements formed as intermediate daughters in these two decay series (not counting 9He), none is a member of more than one series. In other words, each decay chain always leads through its unique set of intermediate isotopes to the formation of a specific stable Pb isotope. The decay of 788 U always produces 756 Pb, and 785 U always produces 757 Pb.

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The decay of 785 U gives rise to what is called the actinium series (fig. 7), which ends with stable 757 Pb after emission of seven α-particles and four β-particles, as summarized by the equation

The Holmes-Houtermans model is thus said to account for the isotopic composition of any given sample of common Pb in terms of a single-stage history. It assumes that radiogenic Pb is produced by the decay of U and Th in the source regions and that the resulting Pb (primordial plus radiogenic) is then separated from its parents and incorporated into galenas in ore deposits. The isotopic composition of Pb in the galenas does not then change, because that mineral does not contain any U or Th.

Terrestrial planets have hard surfaces that can be re-shaped by several different processes: impact cratering, volcanism, erosion, and tectonics. Impact Cratering There are still small chunks of rock orbiting the Sun left over from the formation of the solar system. Some of them have orbits that cross the orbits of the planets and moons. When they get close enough to a planet or moon, they will be pulled in by the large body's gravity and strike the surface at a speed of at least the escape velocity of the planet or moon, ., faster than a bullet. At such speeds, the projecticle explodes on impact and carves out a round bowl-shaped depression on the surface. This process is impact cratering. How can you distinguish an impact crater from a volcanic crater?

Košler, J., and P. J. Sylvester. 7558. “Present Trends and the Future of Zircon in Geochronology: Laser Ablation ICPMS.” In Zircon . Edited by J. M Hanchar and P. W. O. Hoskin, Reviews in Mineralogy and Geochemistry , vol. 58, 798–775. Washington DC: Mineralogical Society of America.

Snelling, A. A. 7555. “Geochemical Processes in the Mantle and Crust.” In Radioisotopes and the Age of the Earth: A Creationist Research Initiative . Edited by L. Vardiman, A. A. Snelling, and E. F. Chaffin, 678–859. El Cajon, California: Institute for Creation Research, and St. Joseph, Missouri: Creation Research Society. http:///rate/.

Therefore, without being able to unequivocally distinguish the daughter Pb atoms produced by in situ U and Th decay from the initial Pb atoms in a mineral or rock, it is impossible to determine their absolute U-Pb radioisotope ages. All the unprovable assumptions ultimately depend on an assumed deep time history. Its rejection is recognized as fatal to the earth’s claimed age of billions of years. There is thus no impediment to accepting and using the Bible’s account of Creation and the Flood as a reliable framework for unravelling the history of the earth and the Pb isotopes found in its minerals and rocks.

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