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I was married to the same woman for over 35 years up un. I have been through thick and thin in life, which has made me more conf. By dating meteorites Patterson was directly dating the age of various planetesimals.
As planetesimals collided, various fragments were scattered and produced meteorites. Iron meteorites were identified as pieces of the core, while stony meteorites were segments of the mantle and crustal units of these various planetesimals. Samples of iron meteorite from Canyon Diablo Meteor Crater Arizona were found to have the least radiogenic composition of any material in the solar system.
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Therefore, troilite found in Canyon Diablo represents the primeval lead isotope composition of the solar system, dating back to 4.
Together, these samples define an isochron, whose slope gives the age of meteorites as 4.
Patterson also analyzed terrestrial sediment collected from the ocean floor, which was believed to be representative of the Bulk Earth composition. Because the isotope composition of this sample plotted on the meteorite isochron, it suggested that earth had the same age and origin as meteorites, therefore solving the age of the Earth and giving rise to the name 'geochron'.
Lead isotope isochron diagram used by C. Patterson to determine the age of the Earth in Animation shows progressive growth over million years Myr of the lead isotope ratios for two stony meteorites Nuevo Laredo and Forest City from initial lead isotope ratios matching those of the Canyon Diablo iron meteorite.
Chondrules and calcium-aluminium-rich inclusions CAIs are spherical particles that make up chondritic meteorites and are believed to be the oldest objects in the solar system.
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Hence precise dating of these objects is important to constrain the early evolution of the solar system and the age of the earth. The U-Pb dating method can yield the most precise ages for early solar-system objects due to the optimal half-life of U. However, the absence of zircon or other uranium-rich minerals in chondrites, and the presence of initial non-radiogenic Pb common Pbrules out direct use of the U-Pb concordia method.
Therefore, the most precise dating method for these meteorites is the Pb-Pb method, which allows a correction for common Pb. When the abundance of Pb is relatively low, this isotope has larger measurement errors than the other Pb isotopes, leading to very strong correlation of errors between the measured ratios.
This makes it difficult to determine the analytical uncertainty on the age. To avoid this problem, researrs  developed an 'alternative Pb-Pb isochron diagram' see figure with reduced error correlation between the measured ratios.
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The most accurate ages are produced by samples near the y-axis, which was achieved by step-wise leaching and analysis of the samples. The result of U-corrected Pb-Pb dating has produced ages of This supports the idea that CAIs crystallization and chondrule formation occurred around the same time during the formation of the solar system.
However, chondrules continued to form for approximately 3 My after CAIs.
Hence the best age for the original formation of the solar system is This date also represents the time of initiation of planetary accretion. Successive collisions between accreted bodies led to the formation of larger and larger planetesimals, finally forming the Earth-Moon system in a giant impact event.
The age difference between CAIs and chondrules measured in these studies verifies the chronology of the early solar system derived from extinct short-lived nuclide methods such as 26 Al- 26 Mg, thus improving our understanding of the development of the solar system and the formation of the earth.
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