The similarity in composition and amounts of detrital components to some modern big river sands (Potter, 1978) suggest that both the present and Paleozoic high stands of the continents largely produced the same types of debris (cf.,Potter, 1978)
The similarity in composition and amounts of detrital components to some modern big river sands (Potter, 1978) suggest thatboth the present and Paleozoic high stands of the continents largely produced the same types of debris (cf.,Potter, 1978)