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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Rahul kumar
GPTS, or Geomagnetic Polarity Time Scale has been derived from an analysis of magnetic anomalies measured over the ocean floors and combining these anomalies to known and dated magnetic polarity reversals found on land. By convention, positive anomalies represent periods when Earth's magnetic field was pointing north (same as today) as it is today, while negative anomalies represent periods in Earth's history when Earth's magnetic field pointed to the south pole. Chron is the geochronological unit indicates a time Interval whereas chronozone is a chronostratigraphic unit (a rock sequence deposited during a chron).