Morphology and Dynamics of a Major Anastomosing Channel System Riverine Plain, Australia

一个主要吻合通道的形态和动力学 河流平原系统，澳大利亚 墨累河具有水文、地貌、 沉积学的兴趣，因为它接近卡德尔断层 它分叉了，一条主要的水流在 澳大利亚东南部的冲积河流平原。 在这一领域 就有可能研究 发展封闭式渠道网络， 确定活动构造是否正在积极地导致 过带泛洪频率和信道问题 稳定 这项研究将确定如何形态和 河道内沉积体系的沉积特征不同 以及局部和区域构造效应的因素。

Morphology and Dynamics of a Major Anastomosing Channel System Riverine Plain, Australia The Murray River is of hydrologic, geomorphic and sedimentologic interest because as it approaches the Cadell Fault it bifurcates, and a major anastomosing-stream develops on the alluvial Riverine Plain of southeastern Australia. In this area it will be possible to study the characteristics of and reason for the deveolpment of anastomosing channel network and to determine if active tectonics is actively causing increased frequency of overband flooding and the problems of channel stability. The study will determine how the morphological and sedimentary character of anastomosing system differs in channels as well as factor in the local and regional tectonic effects.