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Mathematical Modelling Of The Bridges Structural Monitoring I

8. REFERENCES Ajiboye O., 2010, Sensor Computation and Communication for Remote Structural Monitoring, . Chang, F.K., et all, 1999, Structural Health Monitoring, Proceedings of the 2 nd International Workshop on Structural Health Monitoring, Stanford, CA, USA . Dong Y., 2010, Bridges Structural Health Monitoring and Deterioration Detection, Synthesis of Knowledge and Technology, Alaska University Transportation Center, Fairbanks, AK 99775

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A new type of slumping-induced soft-sediment deformation structure: the envelope structure

character and physical basis, Vol. II. Elsevier, Amsterdam, 663 pp. Alsop, G.I., Marco, S., Weinberger, R. & Levi, T., 2016. Sedimentary and structural controls on seismogenic slumping within mass transport deposits from the Dead Sea Basin. Sedimentary Geology 344, 71–90. Bouma, A.H., 1962. Sedimentology of some Flysch Deposits: A Graphic Approach to Facies Interpretation . Elsevier, Amsterdam, 168 pp. Chough, S.K., 2013. Geology and Sedimentology of the Korean Peninsula . Elsevier, Amsterdam, 348 pp. Chough, S.K. & Sohn, Y.K., 2010. Tectonic

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Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)

.J., 1972. Bed-load sediments . Sedimentology 18, 159–219. Nemec, W. & Steel, R.J., 1988. What is a fan delta and how do we recognise it? [In:] Nemec, W. & Steel, R.J. (Eds): Fan Deltas: Sedimentology and Tectonic Settings . Blackie and Sons Ltd., London, 3–13. Orzechowski, Sz., 2007. Zaplecze osadnicze i podstawy surowcowe starożytnego hutnictwa świętokrzyskiego [Settlement base and raw material bases of the ancient Holy Cross Mountains metallurgy] . Kieleckie Towarzystwo Naukowe, Kielce, 392 pp. Piasta, S., 2012. Leksykon Suchedniowa [The lexicon

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A coarse Bayesian approach to evaluate luminescence ages

sampling manual (version ii). MRC Biostatistics Unit, Institute of Public Health, Cambridge, UK. [31] Steel D, 2001. Bayesian statistics in radiocarbon calibration. Philisophy of Sciences 68(3): S153–S164. [32] Van Strydonck M, Moor AD and Benazeth D, 2004. 14C dating compared to art historical dating of roman and coptic textiles from egypt. Radiocarbon 46: 231–244. [33] Wintle AG, 1973. Anomalous Fading of Thermoluminescence in Mineral Samples. Nature 245

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OSL dating of the late Quaternary slip rate on the Gyaring co Fault in central Tibet

landforms, we mainly sampled the uplifted side of the GCF and the abandoned western edges of alluvial fans and/or preserved river terrace risers. This approach reduces the possibility that later erosion may influence our results and interpretations. OSL dating was used to study the northern segment of the GCF at the Aerqingsang and Quba sites ( Fig. 1 ). Six samples were collected from the alluvial sediments. To avoid potential exposure to daylight whilst sampling, sediments for equivalent dose ( D e ) determination were only taken from the middle part of each steel

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Luminescence chronology of alluvial fan in North Bengal, India: Implications to tectonics and climate

steel disks of 10 mm diameter, the grains were mounted on the disks using Silko-Spray silicone oil. Standard SAR protocol (Murray and Wintle, 2000) was applied to obtain equivalent dose for each sample. The optical luminescence measurements were made on Lexsygsmart TL-OSL reader (Freiberg Instruments, Germany) at luminescence dating laboratory in IISER Kolkata. The instrument beta dose rate was calibrated using calibration quartz supplied from the Risoe National Laboratory, Denmark Technical University, Denmark. The instrument is equipped with blue light emitting LEDs

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Interpretation of soil erosion in a Polish loess area using OSL, 137Cs, 210Pbex, dendrochronology and micromorphology – case study: Biedrzykowice site (s Poland)

collected using a “Stiboka” motorized corer (inserting 10 cm diameter demountable steel tubes into the soil profiles) along five downslope transects from an agricultural field. The motorized sample corer allowed soil cores with a non-disturbed structure to be obtained. Core locations were recorded using an RTK GPS (Promark 220, about 0.1 m accuracy) and are presented in Fig. 1 . The soil cores were sectioned into 10 cm intervals. Additional cores were collected from undisturbed reference sites and sectioned at 2, 3 or 5 cm increments. Reference sites were selected as

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U-Pb geochronology, Sr-Nd geochemistry, petrogenesis and tectonic setting of Gandab volcanic rocks, northeastern Iran

the development of a magmatic arc ( Spies et al ., 1983 ; Shafii Moghadam et al ., 2014 ). Tertiary intrusive and volcanic rocks of Sabzevar zone have the characteristics of the calc-alkaline magmas. Furthermore, there are alkaline rocks in this zone. As shown in Fig. 1 , Gandab area is situated in the Sabzevar structural zone, and Sabzevar Torbat Jam subzone at north of the Daruneh fault (e.g. Ruttner and Stöcklin, 1967 ; Berberian and King, 1981 ; Alavi, 1991 ) located in the central part of the 1:100000 geological map of Kadkan sheet in northeast of Iran

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Experimental interactions of Slovak bentonites with metallic iron

References Arthur R., Apted M. & Stenhouse M. 2005: Comment on Long-Term Chemical and Mineralogical Stability of the Buffer. SKI Report 2005: 09, Swedish Nuclear Power Inspectorate , Stockholm, Sweden. Betancur J. D., Barrero C. A., Greneche J. M. & Goya G. F. 2004: The effect of water content on the magnetic and structural properties of goethite. J. Alloys. Compounds 369, 247-251. Börgesson L., Karnland O., Hökmark H. & Sellin P. 2002: Buffer and Safety Assessment for KBS-3H

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Quaternary alluvial fan systems of the Agri intermontane basin (southern Italy): tectonic and climatic controls

I. 1989: Climatic versus tectonic controls of fan sequences: lessons from the Dead Sea, Israel. J. Geol. Soc. London 146, 527-538. Frostick L.E. & Steel R.J. 1993: Tectonic signatures in sedimentary basin fill: an overview. Int. Ass. Sed., Spec. Publ. 20, 1-9. Giano S.I., Lapenna V., Piscitelli S. & Schiattarella M. 1997: New geological and geophysical data on the structural setting of the Quaternary continental deposits of the Agri high Valley (Basilicata). Quaternario 10, 591

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