Participation of the R-centres in the sensitization of the OSL signal

Advanced Search Abstract The Colorado Plateau presents a contrast between deep and seemingly recent erosion and apparently only mild late Cenozoic tectonic activity. Researchers have recently proposed multiple sources of epeirogenic uplift and intriguing patterns of differential incision, yet little or no quantitative constraints exist in the heart of the plateau to test these ideas. Here, we use both optically stimulated luminescence OSL and uranium-series dating to delimit the record of fluvial strath terraces at Crystal Geyser in southeastern Utah, where the Little Grand Wash fault crosses the Green River in the broad Mancos Shale badlands of the central plateau. Results indicate there has been no deformation of terraces or surface rupture of the fault in the past k. The Little Grand Wash fault may have initiated during Early Tertiary Laramide tectonism, but it contrasts with related structures of the ancestral Paradox Basin that are presently active due to salt dissolution and focused differential erosion. We also hypothesize there may be a Pliocene component of fault slip in the region linked to broad-wavelength erosional unloading, domal rebound, and extension. An apparent rapid decrease in incision rates just upstream through Desolation Canyon suggests the Green River here may have recently experienced an upstream-migrating wave of incision. Overall erosion of the region is linked to a pulse of late Cenozoic incision driven by the integration and base-level drop of the Colorado River off the southwestern margin of the plateau to the Gulf of California Lucchitta, ; Pederson et al. That plateau margin in the western Grand Canyon area is the focus of scientific controversy because of its complex and long paleocanyon-cutting history spanning the Cenozoic cf. However, the southwest margin contrasts with the core of the Colorado Plateau physiographic province, including our study area, which has a notably younger and more active record of erosion and landscape evolution Hoffman et al.

Optically stimulated luminescence dating of artifacts … – NOPR

The spatial distribution of radon along lines traversing the fault zones revealed anomalies, clearly connected to the local tectonic structure. Specifically, increased radon signals evolved on the radon background level, in the vicinity of the faults’ axes and the signal-to-background ratio ranged from 2 to The consistency of this pattern confirms that the radon technique is powerful in the detection and mapping of active fault zones.

The loess stratigraphic boundary at the Pleistocene/Holocene transition defined by the magnetic susceptibility (MS) has previously been assumed to be synchronous with the Marine Isotope Stage (MIS) 2/1 boundary, and approximately time-synchronous at different sections across the Chinese Loess.

To study dosimetry of patients during the external radiotherapy of head and neck cancers from different hospitals of the northeastern region NER of India. Dosimetry was carried out at 8 eight anatomical points to these patients, namely, target entrance and exit points , forehead, chest, abdomen, gonad, arm, and leg respectively by thermoluminescence TL as well as optically stimulated luminescence OSL dosimeters.

Patient dosimetry was found to vary with an average of 1. Maximum dose received from a stray radiation is about 1. Survey of patient dosimetry for head and neck cancer patients undergoing external radiotherapy treatment: A study from northeastern hospitals of India. J Can Res Ther ;5: However, there is always a chance of second cancer occurring after radiotherapy for a variety of cancers among long-term survivors.

Research and Analytical Facilities

Links The principles of Luminescence Dating Luminescence dating is used to identify when a sample was last exposed to daylight or extreme heat by estimating the amount of ionising radiation absorbed since burial or firing. This equation very simply expresses the calculations necessary, but it is important to be aware of the factors influencing the two values used.

Heterogeneous sediments and radioactive disequilibria will increase errors on Dr, while incomplete bleaching of the sample prior to burial, anomalous fading in feldspars, and the estimation of past sediment moisture content may all also add to increased errors.

luminescence analyses were carried out on a Riso Automated OSL Dating System Model TL/OSL-DAB/C, equipped with blue and infrared diodes, using the Single Aliquot Regenerative Dose (SAR) technique (Murray and Wintle, ).

Van Dissen, Nicola J. Mark Henderson Part 1: Step 1 Chemical Treatment Samples had their outer surfaces removed. Of this removed outer scrapings, g was weighed and dried in an oven in preparation for gamma spectrometer analysis. A plastic cube was then filled with remaining scrapings in preparation for water content measurment. This was carried out overnight until all carbonate was removed by the reaction. The next step involved ml CBD solution 71 g sodium citrate, 8. After every chemical treatment procedure distilled water was used to wash the sample several times.

This slurry was placed into an ultrasonic bath and mechanically agitated for 1 hour. Preparation of Measurement of Dose Rate The dry, ground and homogenised sample material were weighed and sealed in air tight perspex containers and stored for at least four weeks. This storage time minimizes the loss of the short lived noble gas Rn and allows Ra to reach equilibrium with its daughters Pb and Bi.

Measurements Luminescence age was determined by two factors: These 39 disks together with nine non-irradiated disks total of 48 disks were stored for four weeks to relax the crystal lattice after irradiation. After storage, the 48 disks were preheated for five minutes at oC, then were measured using a Riso TL-DA reader with infrared diodes at nm used to deliver a stimulated beam at the room temperature for s.

The Risø TL/OSL reader

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OSL dating of two samples indicated absolute ages ranging from ± to ± ka. Deposits of stage V occur in the distal portion of the palaeocliff. The mean width of these deposits is m and the length is about 6 km, with beach ridges trending in the NW–SE direction.

Arctic, Antarctic, and Alpine Research Accepted: Moreover, climate reconstruction in New Zealand provides insight into the amount of climate change that occurred in the Southwest Pacific where zonal circulation is an important integrator of the climate signal. The MIS 4 advance was fractionally larger and is dated by a former ice-marginal lacustrine deposit minimum age with a basal Optically Stimulated Luminescence OSL sediment deposition age of Our findings and a growing number of publications indicate that many temperate valley glaciers reacted differently to the major ice sheets during the Last Glacial Cycle, reaching their maximum extent during MIS 4 rather than during peak global ice volume during MIS 2.

Introduction New Zealand, together with Tasmania and South America, are the only regions to have experienced extensive Quaternary mid-latitude glaciation in the southern hemisphere. Many glaciers at this latitude are presently characterized by large mass balance gradients, high flow rates, and rapid responses to climatic change Woo and Fitzharris, They are excellent targets for glacier-climate reconstruction.

The extent and timing of glacial expansion during this period is well constrained in the central Southern Alps where three glacial advances of similar extent culminated at 28, In New Zealand, further evidence is required to reveal the extent and timing of these advances. Quantitative estimates of past terrestrial temperature and precipitation during the LGC in New Zealand are rare.

Estimates of equilibrium-line depression from glaciers in the Southern Alps range from to m above sea level a. Porter, ; Bacon et al.

Dating quaternary events by luminescence

If your browser does not support JavaScript, please read the page content below: These are discussed below. The estimation of De can be done using multiple aliquot MA , single aliquot SA or single grain SG techniques and in each case additive dose or regenerative dose procedures are used. In the additive dose procedures, several laboratory doses of varying magnitude are given additionally on top of the natural dose of a sample, on several identical subsamples of a natural sample so called aliquots.

The luminescence signal from the natural dose, as well as the natural plus added doses is plotted against the added doses zero added dose for the natural and the relation is fitted with a linear or exponential curve, which describes the growth of the luminescence signal with increasing dose growth curve.

Introduction. Optically stimulated luminescence (OSL) is one of a class of measurements known as stimulated phenomena. Such phenomena may be stimulated thermally or optically and the reader is referred to works by Aitken () and Botter-Jensen and others () for more detail.

Use of a new luminescence profile technique on the same rockfall furthermore outlines a window of time A. Our study illustrates novel and widely applicable approaches for dating rock art that do not require destructive sampling, and results suggest that Barrier Canyon rock art persisted across the transition from the late Archaic into the agrarian Fremont culture in the American Southwest. Abstract Rock art compels interest from both researchers and a broader public, inspiring many hypotheses about its cultural origin and meaning, but it is notoriously difficult to date numerically.

Barrier Canyon-style BCS pictographs of the Colorado Plateau are among the most debated examples; hypotheses about its age span the entire Holocene epoch and previous attempts at direct radiocarbon dating have failed. We provide multiple age constraints through the use of cross-cutting relations and new and broadly applicable approaches in optically stimulated luminescence dating at the Great Gallery panel, the type section of BCS art in Canyonlands National Park, southeastern Utah.

Results provide a maximum possible age, a minimum age, and an exposure time window for the creation of the Great Gallery panel, respectively. The only prior hypothesis not disproven is a late Archaic origin for BCS rock art, although our age result of A.

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We have a well equipped computer teaching laboratory, postgraduate and undergraduate physical geography laboratories, and image processing facilities which provide an important component for teaching and research in remote sensing and geographical information systems GIS. Geochemistry Laboratory B11j Our geochemistry lab is used for sample preparation and research into environmental science areas such as remediation, climate change and supporting undergraduate dissertations.

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Authenticity dating of ceramic objects uses both TL and OSL. another untranslated German paper).. p.. the lab needs mg of powder and only really looks for baseline signal. G.

During the last quarter century the Institute has expanded and grown into a Centre of Excellence in the Himalayan Geosciences with scientists and staff working in diverse fields probing deep earth structure and rocks of the mountains, glaciers, river systems, lakes, groundwater, landslides, etc. Sophisticated analytical facilities in the Institute are run by competent scientists and technical staff, generating data for Scientists of the Institute as well as for other Universities and organisations.

In the past WIHG has technically empowered several mega and small infrastructure projects relating to hydroelectricity, tunnels, railways, road alignments, groundwater and mineral wealth surveys etc. The institute’s well-equipped state of the art laboratories and other infrastructure are sound and ready to undertake consultancy projects related to: Selection of sites for Hydroelectric projects, buildings, infrastructures, dams, bridges, rail route or any other construction related activities in the Himalayan terrain.

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Optical Stimulated Luminescence (OSL) Dating in Geoarchaeological Research

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