craton मीनिंग इन हिंदी

अधिक: आगे

The Indian Craton was once part of the supercontinent of Pangaea.
The history of the Archaean cratons is extremely complex and protracted.
To the east are the rocks of the Archean Rae Craton.
The North Atlantic Craton fragmented 2450 to 2000 million years ago.
During the Neoproterozoic, South China Craton was intruded by magma.
The Canadian Shield is the largest exposure of this craton.
At that depth, craton roots extend into the asthenosphere.
A parageosyncline is an epeirogenic geosynclinal basin located within a craton area.
Most rocks in Africa facing the SWIR are Archean cratons.
On a side note about continental crust Craton might be of interest.

संज्ञा.

the part of a continent that is stable and forms the central mass of the continent; typically Precambrian