Relevant bibliographies by topics / Archaeological geology Archaeological dating

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Archaeological geology Archaeological dating'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Archaeological geology Archaeological dating"

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Susino, George J. "Optical dating and lithic microwaste—Archaeological applications." Quaternary Geochronology 5, no. 2-3 (2010): 306–10. http://dx.doi.org/10.1016/j.quageo.2009.02.008.

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Bevan, B. W. "Archaeological Dating from Magnetic Maps: Some Failures." Journal of Environmental & Engineering Geophysics 14, no. 3 (2009): 129–44. http://dx.doi.org/10.2113/jeeg14.3.129.

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Abeyratne, Mohan. "TL dating of Sri Lankan archaeological sites." Quaternary Science Reviews 13, no. 5-7 (1994): 585–88. http://dx.doi.org/10.1016/0277-3791(94)90081-7.

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Bruins, Hendrik J., Johannes van der Plicht, and J. Alexander MacGillivray. "The Minoan Santorini Eruption and Tsunami Deposits in Palaikastro (Crete): Dating by Geology, Archaeology, 14C, and Egyptian Chronology." Radiocarbon 51, no. 2 (2009): 397–411. http://dx.doi.org/10.1017/s003382220005579x.

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Deposits from the Minoan Santorini (Thera) eruption in the eastern Mediterranean region constitute the most important regional stratigraphic marker in the chronological perplexity of the 2nd millennium BCE. Extensive tsunami deposits were discovered in Crete at the Minoan archaeological site of Palaikastro, containing reworked volcanic Santorini ash. Hence, airborne deposition of volcanic ash, probably during the 1st (Plinian) eruption phase, preceded the tsunami, which was apparently generated during the 3rd or 4th phase of the eruption, based on evidence from Thera. Average radiocarbon dates (uncalibrated) of animal bones in the Palaikastro tsunami deposits along the coast (3350 ± 25 BP) and at the inland archaeological site (3352 ± 23 BP) are astoundingly similar to the average 14C date for the Minoan Santorini eruption at Akrotiri on Thera (3350 ± 10 BP). The wiggle-matched 14C date of the eruption in calendar years is 1627–1600 cal BCE. Late Minoan IA pottery is the youngest element in the Palaikastro tsunami deposits, fitting with the LM IA archaeological date for the Santorini eruption, conventionally linked at ~1500 BCE with Dynasty XVIII of the historical Egyptian chronology. The reasons for the discrepancy of 100–150 yr between 14C dating and Egyptian chronology for part of the 2nd millennium BCE are unknown. 14C dates from Tell el-Dabca in the eastern Nile Delta show that the 14C age of the Santorini eruption matches with 14C results from 18th Dynasty strata C3 and C2, thereby confirming grosso modo the conventional archaeo-historical correlations between the Aegean and Egypt. We propose that a dual dating system is used in parallel: (1) archaeological material-cultural correlations linked to Egyptian chronology; (2) 14C dating. Mixing of dates from the 2 systems may lead to erroneous archaeological and historical correlations. A “calibration curve” should be established between Egyptian chronology and 14C dating for the 2nd millennium BCE, which may also assist to resolve the cause of the discrepancy.
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Dye, Tom. "Apparent Ages of Marine Shells: Implications for Archaeological Dating in Hawai'i." Radiocarbon 36, no. 1 (1994): 51–57. http://dx.doi.org/10.1017/s0033822200014326.

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The conventional 14C ages of 8 marine shells of known age and 11 marine shells stratigraphically associated with dated wood charcoal show considerable variation from expected ages. One source of this variation is seashore geology; comparison of 6 AMS dates on 3 species of shallow-water, herbivorous gastropod shells from Pleistocene limestone and Holocene volcanic coasts shows that shells from Pleistocene limestone coasts can have apparent, or reservoir, 14C ages up to 620 yr greater than shells of the same species from volcanic coasts. The relatively great variation in apparent ages of Hawaiian marine shells poses problems for their use in dating archaeological sites. For best results, an archaeological marine shell should be sourced to a particular local environment, and the apparent age of shells in that environment determined by dating well-provenienced shells of known age.
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Marcos, Celia, María de Uribe-Zorita, Pedro Álvarez-Lloret, Alaa Adawy, Patricia Fernández, and Pablo Arias. "Quartz Crystallite Size and Moganite Content as Indicators of the Mineralogical Maturity of the Carboniferous Chert: The Case of Cherts from Eastern Asturias (Spain)." Minerals 11, no. 6 (2021): 611. http://dx.doi.org/10.3390/min11060611.

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Chert samples from different coastal and inland outcrops in the Eastern Asturias (Spain) were mineralogically investigated for the first time for archaeological purposes. X-ray diffraction, X-ray fluorescence, transmission electron microscopy, infrared and Raman spectroscopy and total organic carbon techniques were used. The low content of moganite, since its detection by X-ray diffraction is practically imperceptible, and the crystallite size (over 1000 Å) of the quartz in these cherts would be indicative of its maturity and could potentially be used for dating chert-tools recovered from archaeological sites. Also, this information can constitute essential data to differentiate the cherts and compare them with those used in archaeological tools. However, neither composition nor crystallite size would allow distinguishing between coastal and inland chert outcrops belonging to the same geological formations.
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Bruins, Hendrik J., and Johannes van der Plicht. "The Minoan Santorini Eruption and its14C Position in Archaeological Strata: Preliminary Comparison Between Ashkelon and Tell El-Dabca." Radiocarbon 59, no. 5 (2017): 1295–307. http://dx.doi.org/10.1017/rdc.2017.88.

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ABSTRACTThe volcanic mega event of the Minoan Santorini eruption constitutes a time anchor in the 2nd millennium BCE that is inherently independent of archaeology and political history. It was a geological event. Yet the dimension of time in geology is not different than in archaeology or human history. Why then does archaeological dating usually place the Minoan Santorini eruption in the 18th Dynasty around 1500 BCE, whilst radiocarbon dating of the volcanic event at Akrotiri (Thera) yielded a calibrated age of 1646–1603 cal BCE, a difference of more than a century? The crux of the problem lies apparently in the correlation between archaeological strata and political history. We present radiocarbon dates of Ashkelon Phases 10 and 11 in comparison to Tell el-Dabca and the Santorini eruption, based only on14C dating. Tell el-Dabca Phase D/2 is slightly older than the volcanic event. But Phase D/1 or Phase C/2-3 could have witnessed the eruption. Ashkelon Phase 11 has similar radiocarbon dates as Tell el-Dabca Phases E/2, E/1 and D/3, all being significantly older than the Minoan eruption. It seems that the duration of Ashkelon Phase 10 includes the temporal occurrence of the Minoan Santorini eruption within the Second Intermediate Period.
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Stright, Melanie J. "Evaluation of archaeological site potential on the Gulf of Mexico continental shelf using high‐resolution seismic data." GEOPHYSICS 51, no. 3 (1986): 605–22. http://dx.doi.org/10.1190/1.1442115.

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Prehistoric archaeological sites dating between 12 000 B.P. and 6 000 B.P. are expected on that portion of the Gulf of Mexico continental shelf which was subaerially exposed at 12 000 B.P. Although the archaeological sites are too small and their contrast to the surrounding sediments is insufficient to be resolved by high‐resolution seismic profilers, geomorphic features, such as fluvial channels, bays, lakes, etc., with which these sites are frequently associated are easily detected with seismic methods. High‐resolution seismic reflection data from the Gulf of Mexico have produced evidence of relict fluvial systems with well‐preserved terraces, point bars, and levee ridges, occurring within 9.0 m or less of the present seafloor. Regional studies which detail the late Pleistocene and Holocene geology of the Gulf of Mexico, and published sea level curves, indicate that these fluvial features date from the late Wisconsin and early Holocene periods when prehistoric man’s presence in the Gulf Coast Region is well documented. Verifying the presence of archaeological sites in association with these fluvial features will require physical and chemical analysis of sediment cores from each location. The Minerals Management Service is presently conducting an archaeological study designed to investigate relict fluvial features similar to those discussed in this paper. The physical and chemical analyses of the sedimentary cores collected during this study are presently incomplete; however, initial inspection of the cores indicates the presence of well‐preserved lithosomes. The preservation potential of any archaeological sites occurring within these lithosomes also would be excellent.
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RITTENOUR, TAMMY M. "Luminescence dating of fluvial deposits: applications to geomorphic, palaeoseismic and archaeological research." Boreas 37, no. 4 (2008): 613–35. http://dx.doi.org/10.1111/j.1502-3885.2008.00056.x.

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Matchan, Erin L., David Phillips, Fred Jourdan, and Korien Oostingh. "Early human occupation of southeastern Australia: New insights from 40Ar/39Ar dating of young volcanoes." Geology 48, no. 4 (2020): 390–94. http://dx.doi.org/10.1130/g47166.1.

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Abstract In Australia, the onset of human occupation (≥65 ka?) and dispersion across the continent are the subjects of intense debate and are critical to understanding global human migration routes. New-generation multi-collector mass spectrometers capable of high-precision 40Ar/39Ar dating of young (<500 ka) samples provide unprecedented opportunities to improve temporal constraints of archaeological events. In southeastern Australia, a novel approach to improving understanding of occupation involves dating key volcanic eruptions in the region, referenced to stone artifacts and Aboriginal oral traditions. The current study focuses on two monogenetic volcanoes in the Newer Volcanic Province of southeastern Australia: Budj Bim (previously Mount Eccles) and Tower Hill. Budj Bim and its surrounding lava landforms are of great cultural significance and feature prominently in the oral traditions of the Gunditjmara people. Tower Hill is of archaeological significance due to the occurrence of a stone tool beneath tephra. 40Ar/39Ar eruption ages of 36.9 ± 3.1 ka (95% confidence interval) and 36.8 ± 3.8 ka (2σ) were determined for the Budj Bim and Tower Hill volcanic complexes, respectively. The Tower Hill eruption age is a minimum age constraint for human presence in Victoria, consistent with published optically stimulated luminescence and 14C age constraints for the earliest known occupation sites in Tasmania, New South Wales, and South Australia. If aspects of oral traditions pertaining to Budj Bim or its surrounding lava landforms reflect volcanic activity, this could be interpreted as evidence for these being some of the oldest oral traditions in existence.
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Dissertations / Theses on the topic "Archaeological geology Archaeological dating"

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Ward, Ingrid Alexandra Kirsten. "Hidden in the sands of time geoarchaeology of sandstone landscapes in the Keep River region, Northern Territory, Australia /." Access electonically, 2003. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20041014.103128/index.html.

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Pienaar, Marc. "Dating the stone age at Rose Cottage Cave South Africa : an exercise in optically dating cave sediments." Pretoria : [s.n.], 2005. http://upetd.up.ac.za/thesis/available/etd-06052007-084723.

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Mihindukulasooriya, Lorita N. "Environmental changes associated with Native American land use practices a geoarcheological investigation of an Appalachian watershed /." Ohio : Ohio University, 2009. http://www.ohiolink.edu/etd/view.cgi?ohiou1258061703.

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Dean, Jeffrey S. Robinson William J. "Southwest Archaeological Tree-Ring Dating." Laboratory of Tree-Ring Research, University of Arizona (Tucson, AZ), 1991. http://hdl.handle.net/10150/303522.

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Wheeler, G. C. W. S. "Luminescence studies relevant to archaeological dating." Thesis, University of Oxford, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.670305.

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Barrett, Gerard Thomas. "Rehydroxylation dating : assessment for archaeological application." Thesis, Queen's University Belfast, 2015. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.695220.

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Investigations are carried out into the mass gain behaviour of fired clay ceramics following drying (130°C) and reheating (SOO°C), and the application of these mass gain properties to the dating of archaeological ceramics using a modified rehydroxylation dating (RHX) methodology, a component based approach. Gravimetric analysis is conducted using a temperature and humidity controlled glove box arrangement (featuring a top-loading balance) on eighteen samples of varied known ages and contexts; this occurs following transfer from environmentally controlled chambers where subsamples of these samples are aged at three temperatures (2S0C, 3SoC, 45°C) following drying and reheating. The sample set consists principally of post-medieval bricks, but also includes some post-medieval pottery as ·well as both Etruscan and Roman ceramics. A suite of techniques are applied to characterise these ceramics, including XRO, FTIR, p-XRF, thin-section petrography, BET analysis, TG-MS and permeametry. Significant findings are presented related to the drying of samples, the causes of poor mass gain behaviour, the mass gain behaviour following drying at 130°C and the chemisorption processes involved, the relationship between the mass gain behaviour following heating at 130°C and SOO°C, the appropriate models and descriptors of this behaviour, as well as the relationship Of the mass gain behaviour to the chemical, mineralogical, and structural properties of the ceramic involved. For RHX dating, a component based approach is presented and applied. The results are inconclusive, with the estimated ages of most samples generally far too large, neither confirming the effectiveness of a component based approach nor the use of a tA1/4 or tA1/n model. The effects of a range of factors (uncertainties, contamination, mineral alteration, short term heating effect) on the estimated ages are examined and discussed.
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Karlsberg, Angela Jane. "Flexible Bayesian methods for archaeological dating." Thesis, University of Sheffield, 2006. http://etheses.whiterose.ac.uk/12848/.

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Statistical models for the calibration of both independent and related groups of radiocarbon determinations are now well established and there exists a number of software packages such as BCal, OxCal and CALIB that can perform the necessary calculations to implement them. When devising new statistical models it is important to understand the motivations and needs of the archaeologists. When researchers select samples for radiocarbon dating, they are often not interested in when a specific plant or animal died. Instead, they want to use the radiocarbon evidence to help them to learn about the dates of other events, which cannot be dated directly but which are of greater historical or archaeological significance (e.g. the founding of a site). Our initial research focuses on formulating prior distributions that reliably represent a priori information relating to the rate of deposition of dateable material within an archaeological time period or phase. In archaeology, a phase is defined to be a collection of excavated material (context or layers) bounded early and late by events that are of archaeological importance. Current software for estimating boundary dates only allows for one possible type of a priori distribution, which assumes that material suitable for dating was deposited at a uniform rate between the start and end points of the phase. Although this model has been useful for many real problems, researchers have become increasingly aware of its limitations. We therefore propose a family of alternative prior models (with properties tailored to particular problems within archaeological research) which includes the uniform as a special case and allows for more realistic and robust modelling of the deposition process. We illustrate, via two case studies, the difference in archaeological conclusions drawn from the data when implementing both uniform and non-uniform prior deposition models. The second area of research, that we take the first steps towards tackling, is spatiotemporal modelling of archaeological calibration problems. This area of research is of particular interest to those studying the response of plants and animals, including humans, to climate change. In archaeological problems our temporal information typically arises from radiocarbon dating, which leads to estimated rather than exactly known calendar dates. Many of these problems have some form of spatial structure yet it is very rare that the spatial structure is formally accounted for. The combination of temporal uncertainty and spatial structure means that we cannot use standard models to tackle archaeological problems of this kind. Alongside this, our knowledge of past landscapes is generally very poor as they were often very different from modern ones; this limits the amount of spatial detail that can be included in the modelling. In this thesis we aim to make reliable inferences in spatio-temporal problems by carefully devising a model that takes account of the temporal uncertainty as well as incorporating spatial structure, to provide probabilistic solutions to the questions posed. We illustrate the properties of both the conventional models and the spatio-temporal models using a case study relating to the radiocarbon evidence for the Late glacial reoccupation of NW Europe.
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Rees-Jones, Julie. "Optical dating of selected British archaeological sediments." Thesis, University of Oxford, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.295369.

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Clark, Robert James. "Photostimulated luminescence as an archaeological dating tool." Thesis, University of Glasgow, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243957.

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Mabry, Jonathan Blum. "Alluvial cycles and early agricultural settlement phases in the Jordan Valley." Diss., The University of Arizona, 1992. http://hdl.handle.net/10150/186086.

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The parallel development of archaeology and Quaternary geology in several regions of the world is reviewed, and common problems in dating and correlating alluvial sequences are discussed. Buried archaeological remains and radiometric dates provide a chronological framework for the sequence of Late Quaternary alluvial deposits in the central Jordan Rift. While previous studies emphasized a simple, two-stage model of Late Quaternary alluvial deposition, regional comparisons of the geomorphological contexts of archaeological sites of different ages indicate complex, multiple depositional and erosional cycles. These cycles were influenced by tectonism, climatic changes, human land use, and natural geomorphic thresholds, sometimes in combination. The stratigraphy and chronology of early agricultural settlements in the valley are summarized, and investigations at a protohistoric agricultural town are described. Major regional shifts in prehistoric and protohistoric patterns of agriculture and settlement are interpreted in terms of the impacts of changes in alluvial regimes. These correlations have implications for models of agricultural origins, and the stability and resilience of sedentary settlements in dry lands.
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Books on the topic "Archaeological geology Archaeological dating"

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Age determination of young rocks and artifacts: Physical and chemical clocks in Quaternary geology and archaeology. Springer, 1998.

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Wagner, Günther A. Altersbestimmung von jungen Gesteinen und Artefakten: Physikalische und chemische Uhren in Quartärgeologie und Archäologie. F. Enke, 1995.

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Levi, K. G. Radiouglerodnai︠a︡ khronologii︠a︡ prirodnykh i sot︠s︡ialʹnykh fenomenov Severnogo polusharii︠a︡: Monografii︠a︡ : v trekh tomakh. Irkutskiĭ gos. universitet, 2011.

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Fuchs, Markus. Die OSL-Datierung von Arch ̈aosedimenten zur Rekonstruktion anthropogen bedingter Sedimentumlagerung: Geoarch ̈aologische Untersuchungen im Becken von Phlious; NE-Peloponnes, Griechenland. Ibidem-Verlag, 2001.

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Pravěké kulturní souvrství jako archeologický pramen =: Urgeschichtliche Kulturschicht als archäologische Quelle. Archeologický ústav Akademie věd České republiky, 2008.

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Obsidian and ancient manufactured glasses. University of New Mexico Press, 2012.

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Radiocarbon dating: An archaeological perspective. Academic Press, 1987.

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Techniques in archaeological geology. Springer, 2003.

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Garrison, Ervan. Techniques in Archaeological Geology. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-30232-4.

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Garrison, Ervan G. Techniques in Archaeological Geology. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05163-4.

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Book chapters on the topic "Archaeological geology Archaeological dating"

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Garrison, Ervan G. "Petrography for Archaeological Geology." In Natural Science in Archaeology. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05163-4_6.

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Garrison, Ervan G. "Statistics in Archaeological Geology." In Natural Science in Archaeology. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05163-4_8.

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Garrison, Ervan. "Statistics in Archaeological Geology." In Natural Science in Archaeology. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-30232-4_10.

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Garrison, Ervan. "Petrography for Archaeological Geology." In Natural Science in Archaeology. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-30232-4_6.

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Feathers, James. "Luminescence Dating of Archaeological Sediments." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_55.

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Feathers, James. "Dating Techniques in Archaeological Science." In Encyclopedia of Global Archaeology. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-51726-1_326-2.

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Liritzis, Ioannis, Ashok Kumar Singhvi, James K. Feathers, et al. "Luminescence Dating of Archaeological Materials." In Luminescence Dating in Archaeology, Anthropology, and Geoarchaeology. Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-00170-8_4.

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Feathers, James K. "Dating Techniques in Archaeological Science." In Encyclopedia of Global Archaeology. Springer New York, 2014. http://dx.doi.org/10.1007/978-1-4419-0465-2_326.

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Feathers, James K. "Luminescence Dating of Archaeological Sediments." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6326-5_55-1.

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Feathers, James. "Luminescence Dating of Archaeological Sediments." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6326-5_55-2.

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Conference papers on the topic "Archaeological geology Archaeological dating"

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Carlotto, Mark J. "Archaeological dating using a data fusion approach." In Signal Processing, Sensor/Information Fusion, and Target Recognition XXVIII, edited by Lynne L. Grewe, Erik P. Blasch, and Ivan Kadar. SPIE, 2019. http://dx.doi.org/10.1117/12.2520130.

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Kossolapov, Alexander J., Alexander P. Ivanov, and Pavel B. Kuznetsov. "Helium radiogenic clock for dating of archaeological gold." In Photonics West '98 Electronic Imaging, edited by Walter McCrone, Duane R. Chartier, and Richard J. Weiss. SPIE, 1998. http://dx.doi.org/10.1117/12.308588.

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Sixun, Yuan, Li Kun, Yuan Jiarong, et al. "Applications of AMS radiocarbon dating in Chinese archaeological studies." In The fourteenth international conference on the application of accelerators in research and industry. AIP, 1997. http://dx.doi.org/10.1063/1.52566.

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Rittenour, Tammy M. "LUMINESCENCE DATING: SHEDDING LIGHT ON COMPLEX SOIL AND ARCHAEOLOGICAL SITE FORMATION." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323170.

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Martinez-Sacristan, Hernando. "ARCHAEOLOGICAL RESEARCH IN CAVES HELPS GEOLOGY: FAR FROM RHETORIC, CLOSER TO REALITY." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312986.

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Gaza, O., T. B. Sava, C. A. Simion, C. S. Tuta, D. G. Pacesila, and D. V. Mosu. "Radiocarbon dating of single amino acids isolated by HPLC method from archaeological bones samples." In EXOTIC NUCLEI AND NUCLEAR/PARTICLE ASTROPHYSICS (VII). PHYSICS WITH SMALL ACCELERATORS: Proceedings of the Carpathian Summer School of Physics 2018 (CSSP18). Author(s), 2019. http://dx.doi.org/10.1063/1.5091646.

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Niespolo, Elizabeth, Warren Sharp, Warren Sharp, et al. "U-TH BURIAL DATING OF OSTRICH EGGSHELLS: A NOVEL APPROACH TO DATING AFRICAN ARCHAEOLOGICAL SEQUENCES BEYOND THE 14C LIMIT." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-307769.

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Stillinger, Michele D., Joshua M. Feinberg, James W. Hardin, and Jeffrey A. Blakely. "THE NEAR EASTERN ARCHAEOMAGNETIC DATING CURVE (NEAC): A COMPLEMENTARY GEOCHRONOMETER FOR BUILDING ROBUST ARCHAEOLOGICAL CHRONOLOGIES." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-279688.

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Molodin, V., L. Mylnikova, D. Nenakhov, S. Reinhold, E. Parkhomchuk та V. Parkhomchuk. "ИСПОЛЬЗОВАНИЕ УСТАНОВКИ «УСКОРИТЕЛЬНЫЙ МАСС-СПЕКТРОМЕТР ИЯФ СО РАН» ДЛЯ РАДИОУГЛЕРОДНОГО ДАТИРОВАНИЯ КОМПЛЕКСОВ ЭПОХИ РАННЕГО НЕОЛИТА ПАМЯТНИКА ТАРТАС-1 (СРЕДНЕЕ ПРИОМЬЕ)". У Радиоуглерод в археологии и палеоэкологии: прошлое, настоящее, будущее. Материалы международной конференции, посвященной 80-летию старшего научного сотрудника ИИМК РАН, кандидата химических наук Ганны Ивановны Зайцевой. Samara State University of Social Sciences and Education, 2020. http://dx.doi.org/10.31600/978-5-91867-213-6-57-58.

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The Baraba Early Neolithic culture was allocated on the archaeological materials of Tartas-1 site. The set of radiocar- bon dates was received in the Curt-Engelhorn-Centre Archaeometry (Germany) and on the “Accelerator Mass Spec- trometer of the Budker Institute of Nuclear Physics SB RAS” (AMS BINP SB RAS, Russia). The radiocarbon calibration of this set of dates with 1-sigma and 2-sigma demonstrates the total correlation with the dates provided by the laboratory of Heidelberg University; several of them are even identical. Therefore, the correlation of dates received in the different laboratories reaffirms the dating of Tartas-1 site which is 7th millennium BCE. The Baraba archaeological culture has the same dating. The results were published (Molodin et al., 2019).
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Sapelko, S., D. Gerasimov, A. Kriiska та ін. "РАДИОУГЛЕРОДНОЕ ДАТИРОВАНИЕ В МЕЖДИСЦИПЛИНАРНЫХ АРХЕОЛОГИЧЕСКИХ И ПАЛЕОЛИМНОЛОГИЧЕСКИХ ИССЛЕДОВАНИЯХ НА Р. РОССОНЬ, НАРВСКО-ЛУЖСКАЯ НИЗМЕННОСТЬ". У Радиоуглерод в археологии и палеоэкологии: прошлое, настоящее, будущее. Материалы международной конференции, посвященной 80-летию старшего научного сотрудника ИИМК РАН, кандидата химических наук Ганны Ивановны Зайцевой. Samara State University of Social Sciences and Education, 2020. http://dx.doi.org/10.31600/978-5-91867-213-6-79-80.

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Multidisciplinary archaeological and paleolimnological studies at the Rosson River, the Narva-Luga Klint Bay made it possible to set the chronology nearby Rosson 9 settlement site and the paleoenvironment development in the Middle and Late Holocene. This study showed the possibility of the correct chronology setting of events during the radiocar- bon dating inversion.
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Reports on the topic "Archaeological geology Archaeological dating"

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Vakhnina, I. L., M. O. Sidorova, and Z. Y. Zharnikov. Potential Capacity of the Application of the Year-ring Analysis for Dating of Wooden Architecture and Archaeological Materials in Chita. ZO RGO notes, 2019. http://dx.doi.org/10.18411/2304-7356-2019-136-58-65.

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Downes, Jane, ed. Chalcolithic and Bronze Age Scotland: ScARF Panel Report. Society for Antiquaries of Scotland, 2012. http://dx.doi.org/10.9750/scarf.09.2012.184.

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The main recommendations of the panel report can be summarised under five key headings:  Building the Scottish Bronze Age: Narratives should be developed to account for the regional and chronological trends and diversity within Scotland at this time. A chronology Bronze Age Scotland: ScARF Panel Report iv based upon Scottish as well as external evidence, combining absolute dating (and the statistical modelling thereof) with re-examined typologies based on a variety of sources – material cultural, funerary, settlement, and environmental evidence – is required to construct a robust and up to date framework for advancing research.  Bronze Age people: How society was structured and demographic questions need to be imaginatively addressed including the degree of mobility (both short and long-distance communication), hierarchy, and the nature of the ‘family’ and the ‘individual’. A range of data and methodologies need to be employed in answering these questions, including harnessing experimental archaeology systematically to inform archaeologists of the practicalities of daily life, work and craft practices.  Environmental evidence and climate impact: The opportunity to study the effects of climatic and environmental change on past society is an important feature of this period, as both palaeoenvironmental and archaeological data can be of suitable chronological and spatial resolution to be compared. Palaeoenvironmental work should be more effectively integrated within Bronze Age research, and inter-disciplinary approaches promoted at all stages of research and project design. This should be a two-way process, with environmental science contributing to interpretation of prehistoric societies, and in turn, the value of archaeological data to broader palaeoenvironmental debates emphasised. Through effective collaboration questions such as the nature of settlement and land-use and how people coped with environmental and climate change can be addressed.  Artefacts in Context: The Scottish Chalcolithic and Bronze Age provide good evidence for resource exploitation and the use, manufacture and development of technology, with particularly rich evidence for manufacture. Research into these topics requires the application of innovative approaches in combination. This could include biographical approaches to artefacts or places, ethnographic perspectives, and scientific analysis of artefact composition. In order to achieve this there is a need for data collation, robust and sustainable databases and a review of the categories of data.  Wider Worlds: Research into the Scottish Bronze Age has a considerable amount to offer other European pasts, with a rich archaeological data set that includes intact settlement deposits, burials and metalwork of every stage of development that has been the subject of a long history of study. Research should operate over different scales of analysis, tracing connections and developments from the local and regional, to the international context. In this way, Scottish Bronze Age studies can contribute to broader questions relating both to the Bronze Age and to human society in general.
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Hunter, Fraser, and Martin Carruthers. Iron Age Scotland. Society for Antiquaries of Scotland, 2012. http://dx.doi.org/10.9750/scarf.09.2012.193.

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The main recommendations of the panel report can be summarised under five key headings:  Building blocks: The ultimate aim should be to build rich, detailed and testable narratives situated within a European context, and addressing phenomena from the longue durée to the short-term over international to local scales. Chronological control is essential to this and effective dating strategies are required to enable generation-level analysis. The ‘serendipity factor’ of archaeological work must be enhanced by recognising and getting the most out of information-rich sites as they appear. o There is a pressing need to revisit the archives of excavated sites to extract more information from existing resources, notably through dating programmes targeted at regional sequences – the Western Isles Atlantic roundhouse sequence is an obvious target. o Many areas still lack anything beyond the baldest of settlement sequences, with little understanding of the relations between key site types. There is a need to get at least basic sequences from many more areas, either from sustained regional programmes or targeted sampling exercises. o Much of the methodologically innovative work and new insights have come from long-running research excavations. Such large-scale research projects are an important element in developing new approaches to the Iron Age.  Daily life and practice: There remains great potential to improve the understanding of people’s lives in the Iron Age through fresh approaches to, and integration of, existing and newly-excavated data. o House use. Rigorous analysis and innovative approaches, including experimental archaeology, should be employed to get the most out of the understanding of daily life through the strengths of the Scottish record, such as deposits within buildings, organic preservation and waterlogging. o Material culture. Artefact studies have the potential to be far more integral to understandings of Iron Age societies, both from the rich assemblages of the Atlantic area and less-rich lowland finds. Key areas of concern are basic studies of material groups (including the function of everyday items such as stone and bone tools, and the nature of craft processes – iron, copper alloy, bone/antler and shale offer particularly good evidence). Other key topics are: the role of ‘art’ and other forms of decoration and comparative approaches to assemblages to obtain synthetic views of the uses of material culture. o Field to feast. Subsistence practices are a core area of research essential to understanding past society, but different strands of evidence need to be more fully integrated, with a ‘field to feast’ approach, from production to consumption. The working of agricultural systems is poorly understood, from agricultural processes to cooking practices and cuisine: integrated work between different specialisms would assist greatly. There is a need for conceptual as well as practical perspectives – e.g. how were wild resources conceived? o Ritual practice. There has been valuable work in identifying depositional practices, such as deposition of animals or querns, which are thought to relate to house-based ritual practices, but there is great potential for further pattern-spotting, synthesis and interpretation. Iron Age Scotland: ScARF Panel Report v  Landscapes and regions:  Concepts of ‘region’ or ‘province’, and how they changed over time, need to be critically explored, because they are contentious, poorly defined and highly variable. What did Iron Age people see as their geographical horizons, and how did this change?  Attempts to understand the Iron Age landscape require improved, integrated survey methodologies, as existing approaches are inevitably partial.  Aspects of the landscape’s physical form and cover should be investigated more fully, in terms of vegetation (known only in outline over most of the country) and sea level change in key areas such as the firths of Moray and Forth.  Landscapes beyond settlement merit further work, e.g. the use of the landscape for deposition of objects or people, and what this tells us of contemporary perceptions and beliefs.  Concepts of inherited landscapes (how Iron Age communities saw and used this longlived land) and socal resilience to issues such as climate change should be explored more fully.  Reconstructing Iron Age societies. The changing structure of society over space and time in this period remains poorly understood. Researchers should interrogate the data for better and more explicitly-expressed understandings of social structures and relations between people.  The wider context: Researchers need to engage with the big questions of change on a European level (and beyond). Relationships with neighbouring areas (e.g. England, Ireland) and analogies from other areas (e.g. Scandinavia and the Low Countries) can help inform Scottish studies. Key big topics are: o The nature and effect of the introduction of iron. o The social processes lying behind evidence for movement and contact. o Parallels and differences in social processes and developments. o The changing nature of houses and households over this period, including the role of ‘substantial houses’, from crannogs to brochs, the development and role of complex architecture, and the shift away from roundhouses. o The chronology, nature and meaning of hillforts and other enclosed settlements. o Relationships with the Roman world
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