isotopic geological age

基本解釋

Isotopic age has become an important means solving geological problems.
巖石同位素年齡已成為解決地質(zhì)問(wèn)題的一個(gè)重要手段。
Obviously, it is very difficult to determine the initial age of subduction by using the isotopic age of only one geological event.
顯然，如果只想使用任何一種地質(zhì)事件的年齡來(lái)確定碰撞作用的初始作用時(shí)間都是很困難的。
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An approach has been made to the ore genesis from the ore composition, the typical mineral assemblage, the mineral geological thermometer, the K-Ar isotopic age, the sulfur iso- top…
并從礦石物質(zhì)成分、典型礦物組合、同位素組成、稀土元素豐度型式，以及礦化分布和相關(guān)分析等方面、探討了成巖成礦的物質(zhì)來(lái)源及成因問(wèn)題。