Staff Profile

Laboratory manager for the optically stimulated luminescence dating OSL and environmental gamma spectrometry labs. Research contributions: Peer-reviewed papers. Frouin, M. An improved radiofluorescence single-aliquot regenerative dose protocol for K-feldspars. Quaternary Geochronology. Poujol, A. A new insight from the Holocene deformations observed along the Southern Rif front. Ritz, J. Quaternary International ,

Luminescence Chronology of Terrace Development in the Upper Paraná River, Southeast Brazil

Fluvial sequences, particularly terrace staircases, represent archives of Quaternary palaeoclimatic fluctuation and can serve as stratigraphical frameworks for geochronology and for correlation with other depositional environments, in particular, the global marine oxygen isotope record. Fluvial lithostratigraphical frameworks also provide contexts for records, from fossils and artefacts, of faunal evolution and human occupation; conversely, both records can be means of relative dating of riverine sequences.

Three fluvial sequences are examined as case studies. First is the Severn-Avon system in the English Midlands, which has biostratgraphical evidence and an amino acid geochronology, together with marker inputs from three different glaciations.

While the geomorphology of the Solo River terrace and faunal correlations [9], positions of Homo erectus fossil material and dated pumices.

To browse Academia. Skip to main content. Log In Sign Up. Download Free PDF. Gang Hu. Jia-fu Zhang. Luminescence dating of the Yellow River terraces in the Hukou area, China. This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues.

Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article e. Based on the heights of strath above the modern Yellow River level and the strath River incision rate ages, the mean incision rates between different terrace levels were calculated to be 0.

All rights reserved. Introduction a terrace sequence for the whole canyon is established only by connecting the terrace remnants observed in different sites along The Yellow River is the second largest river of China after the the canyon, by strath heights and ages.

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These river terraces records tectonic uplift in the Mut basin. (OSL) dating of the fluvial sediments of the youngest terrace (T16) provides a.

Toggle navigation. Have you forgotten your login? Journal articles. Brocard 1 Pieter van der Beek 2 D. Brocard 1 AuthorId : Author. Pieter van der Beek 2 AuthorId : Author. Hide details. Abstract : Studying river long-profile development as a response to tectonic and climatic controls requires reliable age-dating of paleo-profile remnants preserved as river terraces.

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Study on the estimation method of uplift during the late quaternary by using river terraces. Strategy of terrace correlation and a case study on stratigraphy of river terraces. There are a few uplift data during the late Quaternary obtained by using river terraces than those by using marine terraces , because it is difficult to date a river terrace whose age is older than the marine oxygen isotope stage 6.

In this paper, at first, we reviewed the terrace correlation method, and we proposed our viewpoint of terrace correlation which is based on relationship between geomorphologic features of terraces and geology that consist of terraces. Next, we did the case study on terrace stratigraphy in the Kawasaki Basin, Miyagi pref.

Geomorphological correlation of the tectonically displaced Tejo river terraces (​Gavião-Chamusca area, Portugal) supported by luminescence dating. Research​.

Numerical Modeling: In this this study, we developed a new method to track landscape change in numerical models using a vector-based tracking method, rather than the more typical method of a grid which biases simulation results. In Limaye and Lamb [], we demonstrate the utility of the new framework for three topics of relevance to reservoir exploration: 1 floodplain evolution with sand, mud and variable bank heights; stratigraphic architecture of stacked channel bodies; and the evolution of bedrock river valleys.

In Limaye and Lamb [], we explore the key parameters that control whether incising meandering rivers bevel wide valleys with terraces or become entrenched into canyons. Finally in Limaye and Lamb [in review, Journal of Geophysical Research], we show that terrace formation regularly occurs by meandering rivers in the absence of external changes in climate or tectonics Fig.

We explore the frequency and geometry of autogenic terraces and discuss how they may overlap and be distinguished from climate-change driven terraces Fig 2. Example numerical simulation where river terraces are highlighted in color in planview left and appear as benches stranded above the valley floor in cross section right. These terraces formed in the absence of external perturbations in climate and tectonics.

Field Application: We have developed an automated, objective computer algorithm for detecting river terraces that can be applied to digital elevation data from natural landscapes and data generated in our simulated landscapes.

Researchers determine age for last known settlement by a direct ancestor to modern humans

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archaeology from river terrace deposits Lubbock gave the discovery a later date.

Scientists have long debated the idea that global climate changes have forced river erosion rates to increase over the past five million years. Rittenour and colleagues from the U. Using relatively new dating techniques, we were able, for the first time, to establish ages for river deposits that span these key time periods of global climate change. Skip to main content. You are here News. United States of America. How climatic change impacts on river erosion.

Sebastien Huot

Vertical velocities obtained from uplifted river terrace dating near mountain fronts are commonly converted into overthrusting slip rates assuming simple geometry of the fault at depth. However, the lack of information on the dip angle of these shallow structures can lead to misinterpretation in the accommodation of convergence, and thus to erroneous conclusions on the transfer of shortening to the emergent thrust faults.

Here, to assess the impact of fault geometry, we focus on the eastern Himalayan region in the south Central Bhutan, where the topographic frontal thrust TFT has been already documented by GPS, paleoseismic, geomorphic and geological studies. This study is based on high-resolution near-surface geophysical investigations, including electrical resistivity, seismic and gravity measurements. Using a similar stochastic inversion approach for all data sets, new quantitative constraints on both fault geometry and petrophysical parameters are obtained to image shallow depths, in the upper ca.

This suggests that, in the study area, significant deformation partitioning on several faults including TFT and the Main Boundary Thrust cannot be ruled out.

A Ma chronology and incision rate assessment of the NW Iberian Miño River terraces based on 10Be and luminescence dating. W. Viveen, R. Braucher.

In this study, the formation ages of the Yellow River terraces in the Baode area in China were determined by dating fluvial deposits overlying bedrock straths using optically stimulated luminescence OSL dating techniques. Seven terraces from the lowest terrace T1 to the highest terrace T7 in the study area were recognized, and they are characterized by thick fluvial terrace deposits overlaid by loess sediments. Twenty-five samples from nine terrace sections were dated to about ka.

The OSL ages ka of the fluvial samples from higher terraces T3-T6 seem to be reliable based on their luminescence properties and stratigraphic consistency, but the geomorphologic and stratigraphic evidence show that these ages should be underestimated, because they are generally similar to those of the samples from the lower terrace T2.

The formation ages of the terrace straths and treads for the T1 terrace were deduced to be about 44 ka and 36 ka, respectively, based on the deposition rates of the fluvial terrace deposits, and the T2 terrace has the same strath and tread formation age of about ka. The incision rate was calculated to be about 0.

River terraces (tectonic–climatic interaction)

All publications more feeds DOI: BibTeX file. Fluvial terraces are widespread geomorphic features, which formed dominantly during the Quaternary.

Ji jun li. Fashion stopped for a visit the yellow river terraces: quaternary river arun, china: l. Dating of Read Full Article role of ohakea terrace sequence of​.

All publications more feeds DOI: BibTeX file. This paper deals with the analysis of hillslope sediments and of fluvial terraces and how they are used as paleoenvironmental archives for obtaining new information on the landscape evolution in a small dry valley in the headwaters of the Main River in northern Bavaria, Germany.

Both, traditional geomorphologic approaches, such as field observations and qualitative petrographic analyses of fluvial gravels, and modern numerical dating techniques, are applied. Qualitative petrographic analyses were used as a tool to identify the origin of fluvial terrace gravels and to draw conclusions on the genesis of the particular terrace aggradation.

Lowland River Terraces

Immediate download. Please login to continue. Long term fluvial incision spanning the Late Cenozoic is recorded in many fluvial systems around the world by terrace landform sequences. The incision manifests itself as inset sequences of river terraces which form terrace staircases. The timing of the onset of incision and the rate incision then proceeds at is poorly constrained due to the difficulties in dating river terraces.

Absolute dating of river terraces can yield long-term incision rates, clarify the role of climate in setting times of aggradation and incision, and establish the rates of.

Enter your mobile number or email address below and we’ll send you a link to download the free Kindle App. Then you can start reading Kindle books on your smartphone, tablet, or computer – no Kindle device required. To get the free app, enter your mobile phone number. Would you like to tell us about a lower price? If you are a seller for this product, would you like to suggest updates through seller support? Thermoluminescence TL , Optically Stimulated Luminescence OSL and Electron Spin Resonance ESR dating, collectively known as Luminescence dating has emerged as a technique by itself to directly determine the age not only of ancient pottery, bricks and terracotta but also the burial age of the main mineral constituents in unheated Quaternary Sediments.

Luminescence dating has a proud history of association with archaeology, beginning almost more than half a century ago.

Terrace Formation

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