Tectonica Placilor 6d151t
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-Placile tectonice sunt deplasate de curentii magmatici in diferite directii, aceasta deplasare a placilor sta la baza formarii reliefului si anume megarelief ului si a reliefului de pe continente. -In bazinele oceanice s-au format fisuri care poarta numele de rifturi.Prin rift uri magma iese pe fundalul oceanului, se depune lateral,magma se intareste si formeaza ridicaturi numite dorsale.
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