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The Panthalassa superocean 250 million years ago
The Panthalassa superocean 250 million years ago
The supercontinent Pangaea in the early Mesozoic (at 200 Ma) surrounded by Panthalassa.
The supercontinent Pangaea in the early Mesozoic (at 200 Ma) surrounded by Panthalassa.
The Pacific Plate began forming when the triple junction at the center of Panthalassa destabilized about 190 million years ago.
The Pacific Plate began forming when the triple junction at the center of Panthalassa destabilized about 190 million years ago.
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As the slab is subducted into the mantle, the more dense material will break off and sink to the lower mantle creating a discontinuity elsewhere known
As the slab is subducted into the mantle, the more dense material will break off and sink to the lower mantle creating a discontinuity elsewhere known as a slab avalanche
The effects of mantle plumes possibly caused by slab avalanches elsewhere in the lower mantle on the breakup and assembly of supercontinents
The effects of mantle plumes possibly caused by slab avalanches elsewhere in the lower mantle on the breakup and assembly of supercontinents
U–Pb ages of 5,246 concordant detrital zircons from 40 of Earth's major rivers
U–Pb ages of 5,246 concordant detrital zircons from 40 of Earth's major rivers