Cronostratigrafie
Cronostratigrafie, also known as chronostratigraphy, is the branch of geology that focuses on the temporal ordering of rock layers (strata). It enables geologists to identify and correlate layers across vast geographic distances by assigning them to time intervals based on shared characteristics. The discipline integrates absolute dating techniques such as radiometric dating with relative stratigraphic markers like index fossils, mineral assemblages, and magnetic polarity reversals.
The central unit of chronostratigrafie is the chronostratigraphic unit, which can range from large eons to
To delineate chronostratigraphic boundaries, scientists use a variety of tools. Radiometric dating provides absolute ages by
Accurate chronostratigrafie is crucial for reconstructing Earth’s history, understanding the timing of tectonic events, climate change,