The formation of the polymetallic nodule belt in the CCZ is attributed to the effect of resources of plate tectonics and seafloor spreading, and the reworking of the late-stage supergene geological processes. 东太平洋CC区多金属结核矿带的形成应归于海底板块扩张活动的一种资源效应和经后期表生地质作用改造的结果。
Compared with zeolite, adsorption quantities of CCZ for three dyes were all improved. 与沸石相比,CCZ对三种染料的最大吸附量均有所提高。