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Geomorphologic evidence of phased uplift of the northeastern Qinghai-Tibet Plateau since 1. million years ago

Science china {1. {2. 2004年第9期47卷 822-833页

作者： lu huayu1, wang xiaoyong1, an zhisheng1,{3., zhu rixiang3. ma haizhou2. li zhen4. tan hongbing2.& wang {13. 1. state key laboratory of loess and quaternary Geology, institute of earth environment, Chinese academy of sciences, xi’an 710075 china 2. Qinghai {23. of Salt Lakes, Chinese academy of sciences. xining 810008, china 3. {23. of Geology and Geophysics, Chinese academy of sciences, Beijing 100029, china 4. Department of Geography, Qinghai Normal University, xining 810008, china Chinese Acad Sci Inst Earth Environm State Key Lab Loess & Quaternary Geol Xian 710075 Peoples R China Chinese Acad Sci Qinghai Inst Salt Lakes Xining 810008 Peoples R China Chinese Acad Sci Inst Geol & Geophys Beijing 100029 Peoples R China Qinghai Normal Univ Dept Geog Xining 810008 Peoples R China

A typical sequence of fluvial terraces and aeo{1.an deposits overlying these ter- races were multidiscip{1.nary investigated. New evidences for up{1.ft process of the northeastern Qinghai-Tibetan Plateau in the past 1. m... 详细信息

A typical sequence of fluvial terraces and aeolian deposits overlying these ter- races were multidisciplinary investigated. New evidences for uplift process of the northeastern Qinghai-Tibetan Plateau in the past 14 million years were obtained. At least 11 river terraces along Huangshui, the first-class tributary of Yellow River, at the xining-Huzhu region are identi- fied. While the first one (T1) is classified as an accumulation terrace, the others are all basement river terraces, which consist of the Tertiary sandstone and siltstone bedrock, fluvial gravel and pebbles and the overlying aeolian loess-Red Clay deposit. Samples from the aeolian deposits were examined for paleomagnetic stratigraphic reconstruction (10{12. samples), luminescence dating (16 samples), magnetic susceptibility and grain-size distribution (more than 4000 sam- ples). The luminescence dating and stratigraphic correlation suggest that terraces of Tll, T10, T8, T7, T{12. T2. T1 were formed at 14, 11.{12. 1.55, 1.2. 0.15, 0.07 and 0.01 million years ago, re- spectively. Sedimentological analysis and geomorphological observation indicate that formation and evolution of these terraces were mainly driven by tectonic uplift. Therefore, the terrace se- quence provides an ideal geological record, of the uplift process of the northeastern during the past 14 million years, and the timings of the terraces formation are regarded as the timings of tectonic uplift. The significant uplifting events took place at 14, 11.{12. 1.2.and 0.15 mil- lion years ago, respectively. The fluvial incision at the xining-Huzhu region is less than 100 m during a period of ~12.million years in the Miocene era (between the Tll and T9), while the Huangshui River had incised 4{12. m during the past 1.2.million years (from T7 to the present floodplain). The river incision process clearly demonstrates that accelerated rising of the north- eastern Qinghai-Tibet Plateau during the late Cenozoic, and provides new evidence of previous thoughts

关键词： river terrace, tectonic uplift, loess-Red Clay, the past 1. million years, northeastern Qinghai-Tibet Plateau.

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