The phrase "age of formation" is correct and usable in written English.
It can be used in contexts discussing the period during which something was created or established, often in relation to geological or historical events.
Example: "The age of formation of the mountain range dates back millions of years, providing insight into the Earth's geological history."
Alternatives: "period of formation" or "time of creation".
They were dated by different dating methods (K/Ar and U/Pb) and yielded the same age of formation.
The SHRIMP (Sensitive High Resolution Ion Microprobe) enables the accurate determination of the uranium-lead age of the mineral zircon, and this has revolutionized the understanding of the isotopic age of formation of zircon-bearing igneous granitic rocks.
The SHRIMP (Sensitive High Mass Resolution Ion Microprobe) enables the accurate determination of the uranium-lead age of the mineral zircon, and this has revolutionized the understanding of the isotopic age of formation of zircon-bearing igneous granitic rocks.
To understand this little-known period, the following factors have to be considered: the age of formation at 4.6 billion years ago, the processes in operation until 4.3 billion years ago, the bombardment of Earth by meteorites, and the earliest zircon crystals.
The ages of rift structures' activation can be assessed by determining the age of formation of the metallic mineral deposits they host, especially large and super-large deposits.
As the age of formation of the sediment-deformation structures is similar to that of the deposition of sand bed T1, it is likely that they were caused by the same earthquake.
Over the years, scientists have taken a variety of approaches to determine the canyon's age, such as estimating how quickly sediment traveled from one end of the canyon to the other and studying the age of formations within the canyon.
Terman, A. The effect of age on formation an elimination of autophagic vacuoles in mouse hepatocyte.
Ages of formation, enlargement rates, water and lake-bottom temperatures, the configuration of permafrost, and active-layer thickness were measured at a typical thermokarst lake in the Beiluhe basin between 2007 and 2009.
Rocks reveal their ages of formation in several ways and provide Earth scientists with their most reliable clocks.
U Pb ages of detrital zircons from the same units identify the age of melt formation in the source rocks, while Lu Hf isotope data from zircons resolve discrete crust formation ages in the multiple eroding terrains.
