and the paleochannel that formed during regressive of sea level is the path of salt-water intrusion.
海退后陆源碎屑在滨海地区沉形成的古河道砂层。
and the paleochannel that formed during regressive of sea level is the path of salt-water intrusion.
海退后陆源碎屑在滨海地区沉形成的古河道砂层。
This article discusses and summarizes uraniferous characteristics of paleochannel depositional systems based on depositional characteristics of fluvial systems and geochemical behaviour of uranium.
本文通过对各类河流沉特的研究,结合铀的地球化学行为,探讨河流沉的赋铀性。
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