Relationship between density and velocity of elastic waves in Jordanian sedimentary rocks
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Abstract
Creation of complex geophysical models of the Earth's crust and upper mantle of separate regions is one of the urgent problems of modern geophysics. Modeling data allow us to obtain not only additional information about the structure of the lithosphere as a whole, but also to establish a connection between the peculiarities of the deep structure of the territory and the formation and location of mineral deposits.
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