In some cases, they spread between the layers of near-horizontal sedimentary or volcanic units to form bodies called sills. In this situation, fragments of the host rock must be found within the intrusive body to establish its relatively younger age. Once most or all of the relative ages of various strata have been determined in a region, it may be possible to deduce that certain units geelong singles dating been offset by movement along fractures or faults while others have not.
Dikes that cross fault boundaries may even be found. Application of the simple principle of crosscutting relationships can allow the relative ages of all units to be deduced. The principles for relative age dating described above require no special equipment and can be applied by anyone on a local or regional scale.
They are based on visual observations and simple logical deductions and rely on a correlation and integration of data that occurs in fragmentary form at many outcrop locations. We welcome suggested improvements to any of our articles.
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