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作 者:郭汝军 李长安[1,2] 李亚伟 张岱 孙习林[1] 魏传义[1] 苏建超 冷勇辉 Guo Rujuna;Li Chang’an;Li Yawei;Zhang Dai;Sun Xilin;Wei Chuanyi;Su Jianchao;Leng Yonghui(School of Earth Sciences,China University of Geosciences(Wuhan),Wuhan 430074,China;State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences(Wuhan),Wuhan 430074,China)
机构地区:[1]中国地质大学(武汉)地球科学学院,武汉430074 [2]中国地质大学(武汉).生物地质与环境地质国家重点实验室,武汉430074
出 处:《地质科技情报》2019年第4期175-180,共6页Geological Science and Technology Information
基 金:国家自然科学基金项目“江汉盆地宜昌冲积扇物源解析与区域地貌演化”(41671011)
摘 要:长江的发育演化尤其是东西贯通的时限问题,是百余年来地学界的焦点问题,金沙江水系的演化重组是长江演化中的关键一环。基于填充海拔的模型模拟以及物源示踪的梳理结果,讨论了金沙江在夷平面上南流汇入红河的可能性。结果显示当海拔填充至2 000~2 200 m时,金沙江水系格局发生重大变化,表现为金沙江在金江街一改东流之势,沿宾川盆地汇入古红河;古雅砻江在攀枝花附近转而向西,沿金沙江河谷经宾川盆地流入古红河,形成古红河的一级支流。推断哀牢山-红河断裂带、程海-宾川断裂带的活动及山体隆升特别是鸡足山的隆升可能阻断了上述南流泄口,切断了金沙江与红河的联系,从而形成今日江水东流的水系格局,这为古金沙江南流路径的研究提供了新的思路和方向。The Yangtze River originates from the Tibetan Plateau and flows into the Pacific Ocean.Its formation and evolution,especially the timing of the connection of the Three Gorges,have been the world interests of researchers for more than 100 years,while the recombination of Jinsha River is a critical part for this interest.This paper discusses the possibility of the south flow of Jinsha River into the Red River on the planation surface based on the simulation of the filling elevation model and the results of the tracing of the source.This study reveals that when the planation surface of 2 000 m and 2 200 m altitude exists in Yunnan Plateau,the Jinsha River can flow southward.The upper Jinsha River flows southward from the Shigu town,and flows through the western side of the Jianchuan Basin,while the lower Jinsha River flows southward from Binchuan Town.The activities of Ailao Mountain-Red River Fault and Chenghai-Binchuan fault combined with the uplift of mountains have broken the connection between Jinsha River and Red River,and resulted in current river systems in SE margin of Tibetan Plateau.
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