Fonnation, evolution and environmental changes of the Gyirong Basin and uplift of the Himalaya

• 作 者: 王富葆 李升峰 申旭辉 张捷 阎革
• 机 构: DepartmentofGeo-OceanScience,NanjingUniversity,Nanjing210093,China,China
• 出 处: Science in China,Ser.D
• 发表日期: 1996年4期
• 关键词: uplift Fonnation Miocene tectonic glacial mudstone sedimentary Cenozoic reconstr

During the period from 7.0 to 1.7 Ma B. P., the Gyirong Basin formed in the Late Miocene was filled with more than 300m of fluvio-lacustrine sediments. Since 1.7Ma B. P., the Himalaya has been strongly rising and the basin dissected by the river on the so