Japan Geoscience Union Meeting 2014

Presentation information

International Session (Oral)

Symbol M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS01_29PM1] Land-ocean linkages in East Asian marginal seas

Tue. Apr 29, 2014 2:15 PM - 4:00 PM 314 (3F)

Convener:*Ryuji Tada(Department of Earth and Planetary Science, Graduate School of Science, The Univeristy of Tokyo), Murray, Richard W(Boston University), Chair:Takuya Sagawa(Faculty of Sciences, Kyushu University), Yoshimi Kubota(National Museum of Nature and Science)

2:30 PM - 2:50 PM

[MIS01-02] Pre-Miocene Birth of the Yangtze River

*Hongbo ZHENG1, Peter CLIFT1, Ping WANG1, Ryuji TADA1, Juntao JIA1, Mengying HE1, Fred JOURDAN1 (1.Nanjing Normal University)

Keywords:Yangtze River, birth, Tibetan Plateau, drainage capture, Asian monsoon

The development of fluvial systems in East Asia is closely linked to the evolving topography following India-Eurasia collision. Despite this, the age of the Yangtze River system has been strongly debated, with estimates ranging from 40?45 Ma, to a more recent initiation around 2 Ma. Here, we present new 40Ar/39Ar ages from basalts interbedded with fluvial sediments from the lower reaches of the Yangtze together with detrital zircon U/Pb ages from sand grains within these sediments. We show that a river containing sediments indistinguishable from the modern river was established before ~23 Ma. We argue that the connection through the Three Gorges must post-date 36.5 Ma because of evaporite and lacustrine sedimentation in the Jianghan Basin before that time. We propose that the present Yangtze River system formed in response to regional extension throughout eastern China, synchronous with the start of strike-slip tectonism and surface uplift in eastern Tibet and fed by strengthened rains caused by the newly intensified summer monsoon. Birth of the eastward flowing Yangtze River around the Oligocene/Miocene boundary changed largely the 'source to sink' regime in the East Asia-West Pacific region