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- W3149332592 abstract "克莱矿物质由能追踪海洋的当前的变化并且表明同时期的 paleoclimatic 变化在大陆人来源区域占优势在华南海在东方 Asianmonsoon 进化的学习起了一个重要作用。作为输入源自陆地的事到北华南海的最重要的河之一，珀尔·里弗瓦斯不以前从泥土矿物学的观点注意了。这篇论文在从珍珠河排水盆收集的表面沉积在泥土矿物质上论述详细研究(包括在河口的所有三条主要隧道，各种各样的分支，和 Lingdingyang ) 由使用 X 光检查衍射(XRD ) 方法。结果显示泥土矿物质集合 consistsdominantly kaolinite (35%--65%) ，更小的许多绿泥石(20%--35%) 和 illite (12%--42%) ，并且很惊吓绿土出现(通常 <5%) 。他们的各自的分发不在整个 PearlRiver 排水盆介绍任何明显的差别。然而，下游珀尔·里弗托北华南海，泥土矿物质集合显著地变化：kaolinitedecreases 逐渐地，绿土和 illite 增加逐渐地。另外， illite 化学 indexstepsdown 和 illite 结晶度促进。这些变化显示 majorkaolinite，更小的 illite 和绿泥石的贡献，和到从珀尔河排水盆的北华南海的很少见的绿土。到北边缘的从珍珠河 is72% 的泥土矿物质的最大的贡献并且仅仅 15% 到华南海的北斜坡。在 glacials 和 interglacials， kaolinite 显示机械侵蚀的能力发生在珍珠河排水盆。" @default.
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- W3149332592 date "2007-01-01" @default.
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- W3149332592 title "Clay minerals in surface sediments of the Pearl River drainage basin and their contribution to the South China Sea" @default.
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