For example, with [[Uranium-lead dating]] with the crystallization of magma, this remains a closed system until the uranium decays. As it decays, it disrupts the crystal and allows the lead atom to move. Likewise, heating the rock such as [[granite]] forms [[gneiss]] or [[basalt]] forms [[schist]]. This can also disrupt the ratios of lead and uranium in the sample. | For example, with [[Uranium-lead dating]] with the crystallization of magma, this remains a closed system until the uranium decays. As it decays, it disrupts the crystal and allows the lead atom to move. Likewise, heating the rock such as [[granite]] forms [[gneiss]] or [[basalt]] forms [[schist]]. This can also disrupt the ratios of lead and uranium in the sample. |