台湾浊水溪辫状河与扇三角洲沉积特征分析

来源 :2015全国沉积学大会 | 被引量 : 0次 | 上传用户：cqwzhy1990

【摘要】

：

台湾是非常年轻的造山带,是近500Ma 年来由欧亚板块、冲绳板块和菲律宾板块挤压而不断隆升的岛屿.构造活动非常活动,地震时常发生,处在东亚季风带,同时又受到台风强烈影响等,使得台湾成全球产沙量最高的区域.境内河流源短、坡降大,受台风强降雨影响显著,常形成泥石流和高悬沙浓度的洪水,塑造了特色的山地型河流沉积地貌.

【作者】

：

范代读刘祖乾

【机构】

：

同济大学海洋地质国家重点实验室,上海200092;长江大学地球科学学院,湖北武汉 430100 台

【出处】

：

2015全国沉积学大会

【发表日期】

：

2015年5期

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台湾浊水溪辫状河与扇三角洲沉积特征分析

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