) is an earth science concerned with the solid Earth, the rocks of which it is composed, and the processes by which they change over time.Geology can also refer generally to the study of the solid features of any terrestrial planet (such as the geology of the Moon or Mars).THE DINARIDES The Dalmatian-Herzegovinian Zone (formerly inadequately designated as the High Karst Nappe) has been thurst over the Budva Zone.The direction and distance of movement of this zone is still a matter of speculation.Geology also plays a role in geotechnical engineering and is a major academic discipline.The majority of research in geology is associated with the study of rock, as rock provides the primary record of the majority of the geologic history of the Earth.PERIADRIATIC MARGIN The South Adriatic-Ionian Zone is built up of Cretaceous shallow marine limestones and anhydrites, also accompanied by dolomites in the upper parts; next, of transgressive Middle Eocene limestone and Eocene-Oligocene flysch.
By comparing fossils of different primate species, scientists can examine how features changed and how primates evolved through time.
Geochronology is the science of determining the age of rocks, fossils, and sediments using signatures inherent in the rocks themselves.
Absolute geochronology can be accomplished through radioactive isotopes, whereas relative geochronology is provided by tools such as palaeomagnetism and stable isotope ratios.
The science of geochronology is the prime tool used in the discipline of chronostratigraphy, which attempts to derive absolute age dates for all fossil assemblages and determine the geologic history of the Earth and extraterrestrial bodies.
By measuring the amount of radioactive decay of a radioactive isotope with a known half-life, geologists can establish the absolute age of the parent material.