通过对埋藏古树、泥炭、以及海相贝壳测年资料进行搜集和整理,结果表明:长江下游地区6000 a BP以来古洪水的发生与气候变化有着密切的联系。由于长江下游地区地势低平这一地貌特点,使得海面变化对于研究区洪水发生有着重要的影响,气候变化导致的海面上升对长江下游河段径流的顶托作用导致河流上溯以及地面排水不畅,致使洪水发生频率加大以及洪水危害的程度加强,出现“小水大灾”的现象,长江三角洲地区古洪水发生频率与美洲地区古洪水发生频率的对比研究表明,长江三角地区乃至整个长江流域在大的气候变化趋势上与全球其它地区是相似的,既有全球气候变化特点的同时又具有区域响应的特点,这对于未来研究区洪水发生的预测有着重要意义。 相似文献
Many light rare earth deposits, such as Maoniuping, Dalucao, Panzhihua deposits, are collectively distributed in Panxi rift of Sichuan Province, China, and closely associated with the aegirine quartz syenite-carbonatite complex. Carbon and oxygen isotope studies demonstrate that the carbonatites in the complex are of typical igneous origin related to mantle processes. Electronic microprobe studies show that the fluid-melt inclusions found in the complex are enriched in light rare earth elements (LREE), which suggests that the magma was rich in LREE and could serve as the ore source for the regional LREE mineralization. Both the aegirine quartz syenite-carbonatite complex and the LREE mineralization found therein were derived from the mantle. The rare gas isotope analyses also support that there is a genetic association between the LREE mineralization and mantle processes.