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Obduksioni

Obduksioni është rendi i të cilit shtresat gjeologjike mbivendosen mbi njëri-tjetrin. Ky term është gjithashtu një pjesë e rëndësishme e parimeve gjeologjike të Nicolaus Stenos, e cila thotë se shtresa e mbivendosur në krye të një shtrese tjetër është më e vogël.

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