Articles | Volume 2, issue 1
https://doi.org/10.5194/gchron-2-1-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-2-1-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
24 Jan 2020
Research article | Highlight paper |
| 24 Jan 2020
| 24 Jan 2020
Electron spin resonance (ESR) thermochronometry of the Hida range of the Japanese Alps: validation and future potential
Georgina E. King
CORRESPONDING AUTHOR
Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland
Sumiko Tsukamoto
Leibniz Institute for Applied Geophysics, Hanover, Germany
Frédéric Herman
Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland
Rabiul H. Biswas
Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland
Shigeru Sueoka
Tono Geoscience Center, Japan Atomic Energy Agency, Toki, Japan
Takahiro Tagami
Division of Earth and Planetary Sciences, Kyoto University, Kyoto,
Japan
Related authors
Christoph Schmidt, Théo Halter, Paul R. Hanson, Alexey Ulianov, Benita Putlitz, Georgina E. King, and Sebastian Kreutzer
Geochronology Discuss., https://doi.org/10.5194/gchron-2024-10, https://doi.org/10.5194/gchron-2024-10, 2024
Preprint under review for GChron
Short summary
Short summary
We study the use of zircons as dosimeters using modern techniques, highlighting their advantages such as time-invariant dose rates. We explore the correlation between zircon geochemistry and luminescence properties, observe fast zircon optically stimulated luminescence (OSL) bleaching rates, and assess the potential of auto-regeneration. Low OSL sensitivities require combining natural OSL and auto-regenerated thermoluminescence (TL), with the potential to enhance age accuracy and precision.
Melanie Bartz, Jasquelin Peña, Stéphanie Grand, and Georgina E. King
Geochronology, 5, 51–64, https://doi.org/10.5194/gchron-5-51-2023, https://doi.org/10.5194/gchron-5-51-2023, 2023
Short summary
Short summary
Chemical weathering alters the chemical composition of mineral grains, and it follows that luminescence dating signals may also be progressively modified. We artificially weathered feldspar samples under different chemical conditions to understand the effect of feldspar partial dissolution on their luminescence properties. Only minor changes were observed on luminescence dating properties, implying that chemical alteration of feldspar surfaces may not affect luminescence dating signals.
Joanne Elkadi, Benjamin Lehmann, Georgina E. King, Olivia Steinemann, Susan Ivy-Ochs, Marcus Christl, and Frédéric Herman
Earth Surf. Dynam., 10, 909–928, https://doi.org/10.5194/esurf-10-909-2022, https://doi.org/10.5194/esurf-10-909-2022, 2022
Short summary
Short summary
Glacial and non-glacial processes have left a strong imprint on the landscape of the European Alps, but further research is needed to better understand their long-term effects. We apply a new technique combining two methods for bedrock surface dating to calculate post-glacier erosion rates next to a Swiss glacier. Interestingly, the results suggest non-glacial erosion rates are higher than previously thought, but glacial erosion remains the most influential on landscape evolution.
Dominik Brill, Simon Matthias May, Nadia Mhammdi, Georgina King, Benjamin Lehmann, Christoph Burow, Dennis Wolf, Anja Zander, and Helmut Brückner
Earth Surf. Dynam., 9, 205–234, https://doi.org/10.5194/esurf-9-205-2021, https://doi.org/10.5194/esurf-9-205-2021, 2021
Short summary
Short summary
Wave-transported boulders are important records for storm and tsunami impact over geological timescales. Their use for hazard assessment requires chronological information. We investigated the potential of a new dating technique, luminescence rock surface exposure dating, for estimating transport ages of wave-emplaced boulders. Our results indicate that the new approach may provide chronological information on decadal to millennial timescales for boulders not datable by any other method so far.
Rabiul H. Biswas, Frédéric Herman, Georgina E. King, Benjamin Lehmann, and Ashok K. Singhvi
Clim. Past, 16, 2075–2093, https://doi.org/10.5194/cp-16-2075-2020, https://doi.org/10.5194/cp-16-2075-2020, 2020
Short summary
Short summary
A new approach to reconstruct the temporal variation of rock surface temperature using the thermoluminescence (TL) of feldspar is introduced. Multiple TL signals or thermometers in the range of 210 to 250 °C are sensitive to typical surface temperature fluctuations and can be used to constrain thermal histories of rocks over ~50 kyr. We show that it is possible to recover thermal histories of rocks using inverse modeling and with δ18O anomalies as a priori information.
Benjamin Lehmann, Frédéric Herman, Pierre G. Valla, Georgina E. King, and Rabiul H. Biswas
Earth Surf. Dynam., 7, 633–662, https://doi.org/10.5194/esurf-7-633-2019, https://doi.org/10.5194/esurf-7-633-2019, 2019
Short summary
Short summary
Assessing the impact of glaciation at the Earth's surface requires simultaneous quantification of the impact of climate variability on past glacier fluctuations and on bedrock erosion. Here we present a new approach for evaluating post-glacial bedrock surface erosion in mountainous environments by combining two different surface exposure dating methods. This approach can be used to estimate how bedrock erosion rates vary spatially and temporally since glacier retreat in an alpine environment.
Christoph Schmidt, Théo Halter, Paul R. Hanson, Alexey Ulianov, Benita Putlitz, Georgina E. King, and Sebastian Kreutzer
Geochronology Discuss., https://doi.org/10.5194/gchron-2024-10, https://doi.org/10.5194/gchron-2024-10, 2024
Preprint under review for GChron
Short summary
Short summary
We study the use of zircons as dosimeters using modern techniques, highlighting their advantages such as time-invariant dose rates. We explore the correlation between zircon geochemistry and luminescence properties, observe fast zircon optically stimulated luminescence (OSL) bleaching rates, and assess the potential of auto-regeneration. Low OSL sensitivities require combining natural OSL and auto-regenerated thermoluminescence (TL), with the potential to enhance age accuracy and precision.
Toru Nakajima, Shoma Fukuda, Shigeru Sueoka, Sota Niki, Tetsuo Kawakami, Tohru Danhara, and Takahiro Tagami
Geochronology Discuss., https://doi.org/10.5194/gchron-2024-2, https://doi.org/10.5194/gchron-2024-2, 2024
Preprint under review for GChron
Short summary
Short summary
Establishing an etching procedure for the monazite fission track (MFT) is essential for MFT dating. In this short communication, we have investigated the parameters governing the etching rate of MFT, in particular the effect of radiation damage. Our results show an inverse relationship between MFT etching time and the degree of radiation damage. We show that existing etching recipes may not sufficiently etch MFT of young monazite, advocating the importance of a revision of etching methods.
Ian Delaney, Leif Anderson, and Frédéric Herman
Earth Surf. Dynam., 11, 663–680, https://doi.org/10.5194/esurf-11-663-2023, https://doi.org/10.5194/esurf-11-663-2023, 2023
Short summary
Short summary
This paper presents a two-dimensional subglacial sediment transport model that evolves a sediment layer in response to subglacial sediment transport conditions. The model captures sediment transport in supply- and transport-limited regimes across a glacier's bed and considers both the creation and transport of sediment. Model outputs show how the spatial distribution of sediment and water below a glacier can impact the glacier's discharge of sediment and erosion of bedrock.
Ugo Nanni, Dirk Scherler, Francois Ayoub, Romain Millan, Frederic Herman, and Jean-Philippe Avouac
The Cryosphere, 17, 1567–1583, https://doi.org/10.5194/tc-17-1567-2023, https://doi.org/10.5194/tc-17-1567-2023, 2023
Short summary
Short summary
Surface melt is a major factor driving glacier movement. Using satellite images, we have tracked the movements of 38 glaciers in the Pamirs over 7 years, capturing their responses to rapid meteorological changes with unprecedented resolution. We show that in spring, glacier accelerations propagate upglacier, while in autumn, they propagate downglacier – all resulting from changes in meltwater input. This provides critical insights into the interplay between surface melt and glacier movement.
Melanie Bartz, Jasquelin Peña, Stéphanie Grand, and Georgina E. King
Geochronology, 5, 51–64, https://doi.org/10.5194/gchron-5-51-2023, https://doi.org/10.5194/gchron-5-51-2023, 2023
Short summary
Short summary
Chemical weathering alters the chemical composition of mineral grains, and it follows that luminescence dating signals may also be progressively modified. We artificially weathered feldspar samples under different chemical conditions to understand the effect of feldspar partial dissolution on their luminescence properties. Only minor changes were observed on luminescence dating properties, implying that chemical alteration of feldspar surfaces may not affect luminescence dating signals.
Joanne Elkadi, Benjamin Lehmann, Georgina E. King, Olivia Steinemann, Susan Ivy-Ochs, Marcus Christl, and Frédéric Herman
Earth Surf. Dynam., 10, 909–928, https://doi.org/10.5194/esurf-10-909-2022, https://doi.org/10.5194/esurf-10-909-2022, 2022
Short summary
Short summary
Glacial and non-glacial processes have left a strong imprint on the landscape of the European Alps, but further research is needed to better understand their long-term effects. We apply a new technique combining two methods for bedrock surface dating to calculate post-glacier erosion rates next to a Swiss glacier. Interestingly, the results suggest non-glacial erosion rates are higher than previously thought, but glacial erosion remains the most influential on landscape evolution.
Marcus Richter and Sumiko Tsukamoto
Geochronology, 4, 55–63, https://doi.org/10.5194/gchron-4-55-2022, https://doi.org/10.5194/gchron-4-55-2022, 2022
Short summary
Short summary
When using trapped-charge dating methods to determine the time of deposition of a sediment, it is of great importance to know whether the signal containing the age information has been completely erased before burial or if a residual signal is inherited. We examined the residual doses of the quartz ESR signals of young fluvial sediments from the Lower Rhine terraces with known luminescence ages. We found varying but large residuals, indicating an incomplete bleaching of the quartz ESR signals.
Sean D. Willett, Frédéric Herman, Matthew Fox, Nadja Stalder, Todd A. Ehlers, Ruohong Jiao, and Rong Yang
Earth Surf. Dynam., 9, 1153–1221, https://doi.org/10.5194/esurf-9-1153-2021, https://doi.org/10.5194/esurf-9-1153-2021, 2021
Short summary
Short summary
The cooling climate of the last few million years leading into the ice ages has been linked to increasing erosion rates by glaciers. One of the ways to measure this is through mineral cooling ages. In this paper, we investigate potential bias in these data and the methods used to analyse them. We find that the data are not themselves biased but that appropriate methods must be used. Past studies have used appropriate methods and are sound in methodology.
Dominik Brill, Simon Matthias May, Nadia Mhammdi, Georgina King, Benjamin Lehmann, Christoph Burow, Dennis Wolf, Anja Zander, and Helmut Brückner
Earth Surf. Dynam., 9, 205–234, https://doi.org/10.5194/esurf-9-205-2021, https://doi.org/10.5194/esurf-9-205-2021, 2021
Short summary
Short summary
Wave-transported boulders are important records for storm and tsunami impact over geological timescales. Their use for hazard assessment requires chronological information. We investigated the potential of a new dating technique, luminescence rock surface exposure dating, for estimating transport ages of wave-emplaced boulders. Our results indicate that the new approach may provide chronological information on decadal to millennial timescales for boulders not datable by any other method so far.
Rabiul H. Biswas, Frédéric Herman, Georgina E. King, Benjamin Lehmann, and Ashok K. Singhvi
Clim. Past, 16, 2075–2093, https://doi.org/10.5194/cp-16-2075-2020, https://doi.org/10.5194/cp-16-2075-2020, 2020
Short summary
Short summary
A new approach to reconstruct the temporal variation of rock surface temperature using the thermoluminescence (TL) of feldspar is introduced. Multiple TL signals or thermometers in the range of 210 to 250 °C are sensitive to typical surface temperature fluctuations and can be used to constrain thermal histories of rocks over ~50 kyr. We show that it is possible to recover thermal histories of rocks using inverse modeling and with δ18O anomalies as a priori information.
Benjamin Campforts, Veerle Vanacker, Frédéric Herman, Matthias Vanmaercke, Wolfgang Schwanghart, Gustavo E. Tenorio, Patrick Willems, and Gerard Govers
Earth Surf. Dynam., 8, 447–470, https://doi.org/10.5194/esurf-8-447-2020, https://doi.org/10.5194/esurf-8-447-2020, 2020
Short summary
Short summary
In this contribution, we explore the spatial determinants of bedrock river incision in the tropical Andes. The model results illustrate the problem of confounding between climatic and lithological variables, such as rock strength. Incorporating rock strength explicitly into river incision models strongly improves the explanatory power of all tested models and enables us to clarify the role of rainfall variability in controlling river incision rates.
Ludovic Räss, Aleksandar Licul, Frédéric Herman, Yury Y. Podladchikov, and Jenny Suckale
Geosci. Model Dev., 13, 955–976, https://doi.org/10.5194/gmd-13-955-2020, https://doi.org/10.5194/gmd-13-955-2020, 2020
Short summary
Short summary
Accurate predictions of future sea level rise require numerical models that predict rapidly deforming ice. Localised ice deformation can be captured numerically only with high temporal and spatial resolution. This paper’s goal is to propose a parallel FastICE solver for modelling ice deformation. Our model is particularly useful for improving our process-based understanding of localised ice deformation. Our solver reaches a parallel efficiency of 99 % on GPU-based supercomputers.
Benjamin Lehmann, Frédéric Herman, Pierre G. Valla, Georgina E. King, and Rabiul H. Biswas
Earth Surf. Dynam., 7, 633–662, https://doi.org/10.5194/esurf-7-633-2019, https://doi.org/10.5194/esurf-7-633-2019, 2019
Short summary
Short summary
Assessing the impact of glaciation at the Earth's surface requires simultaneous quantification of the impact of climate variability on past glacier fluctuations and on bedrock erosion. Here we present a new approach for evaluating post-glacial bedrock surface erosion in mountainous environments by combining two different surface exposure dating methods. This approach can be used to estimate how bedrock erosion rates vary spatially and temporally since glacier retreat in an alpine environment.
Lionel Benoit, Aurelie Gourdon, Raphaël Vallat, Inigo Irarrazaval, Mathieu Gravey, Benjamin Lehmann, Günther Prasicek, Dominik Gräff, Frederic Herman, and Gregoire Mariethoz
Earth Syst. Sci. Data, 11, 579–588, https://doi.org/10.5194/essd-11-579-2019, https://doi.org/10.5194/essd-11-579-2019, 2019
Short summary
Short summary
This dataset provides a collection of 10 cm resolution orthomosaics and digital elevation models of the Gornergletscher glacial system (Switzerland). Raw data have been acquired every 2 weeks by intensive UAV surveys and cover the summer 2017. A careful photogrammetric processing ensures the geometrical coherence of the whole dataset.
Raphaël Normand, Guy Simpson, Frédéric Herman, Rabiul Haque Biswas, Abbas Bahroudi, and Bastian Schneider
Earth Surf. Dynam., 7, 321–344, https://doi.org/10.5194/esurf-7-321-2019, https://doi.org/10.5194/esurf-7-321-2019, 2019
Short summary
Short summary
We studied and mapped uplifted marine terraces in southern Iran that are part of the Makran subduction zone. Our results show that most exposed terraces were formed in the last 35 000–250 000 years. Based on their altitude and the paleo sea-level, we derive surface uplift rates of 0.05–5 mm yr−1. The marine terraces, tilted with a short wavelength of 20–30 km, indicate a heterogeneous accumulation of deformation in the overriding plate.
Linda Taft, Uwe Wiechert, Christian Albrecht, Christian Leipe, Sumiko Tsukamoto, Thomas Wilke, Hucai Zhang, and Frank Riedel
Clim. Past Discuss., https://doi.org/10.5194/cp-2019-23, https://doi.org/10.5194/cp-2019-23, 2019
Preprint withdrawn
Antoine Cogez, Frédéric Herman, Éric Pelt, Thierry Reuschlé, Gilles Morvan, Christopher M. Darvill, Kevin P. Norton, Marcus Christl, Lena Märki, and François Chabaux
Earth Surf. Dynam., 6, 121–140, https://doi.org/10.5194/esurf-6-121-2018, https://doi.org/10.5194/esurf-6-121-2018, 2018
Short summary
Short summary
Sediments produced by glaciers are transported by rivers and wind toward the ocean. During their journey, these sediments are weathered, and we know that this has an impact on climate. One key factor is time, but the duration of this journey is largely unknown. We were able to measure the average time that sediment spends only in the glacial area. This time is 100–200 kyr, which is long and allows a lot of processes to act on sediments during their journey.
M. Fox, F. Herman, S. D. Willett, and D. A. May
Earth Surf. Dynam., 2, 47–65, https://doi.org/10.5194/esurf-2-47-2014, https://doi.org/10.5194/esurf-2-47-2014, 2014
Related subject area
Electron spin resonance dating
Investigation of quartz electron spin resonance residual signals in the last glacial and early Holocene fluvial deposits from the Lower Rhine
Marcus Richter and Sumiko Tsukamoto
Geochronology, 4, 55–63, https://doi.org/10.5194/gchron-4-55-2022, https://doi.org/10.5194/gchron-4-55-2022, 2022
Short summary
Short summary
When using trapped-charge dating methods to determine the time of deposition of a sediment, it is of great importance to know whether the signal containing the age information has been completely erased before burial or if a residual signal is inherited. We examined the residual doses of the quartz ESR signals of young fluvial sediments from the Lower Rhine terraces with known luminescence ages. We found varying but large residuals, indicating an incomplete bleaching of the quartz ESR signals.
Cited articles
Auclair, M., Lamothe, M., and Huot, S.: Measurement of anomalous fading for
feldspar IRSL using SAR, Rad. Meas., 37, 487–492,
https://doi.org/10.1016/S1350-4487(03)00018-0, 2003.
Balescu, S. and Lamothe, M.: Comparison of TL and IRSL age estimates of
feldspar coarse grains from waterlain sediments, Quaternary Sci. Rev., 13,
437–444, https://doi.org/10.1016/0277-3791(94)90056-6, 1994.
Bell, W. T.: Alpha dose attenuation in quartz grains for thermoluminescence
dating, Anc. Tl, 12, 4–8, 1980.
Biswas, R., Herman, F., King, G. E., and Braun, J.: Thermoluminescence of
feldspar as a multi-thermochronometer to constrain the temporal variation of
rock exhumation in the recent past, Earth Planet Sci. Lett., 495, 56–68,
https://doi.org/10.1016/j.epsl.2018.04.030, 2018.
Buscombe, D.: Transferable wavelet method for grain-size distribution from
images of sediment surfaces and thin sections, and other natural granular
patterns, Sedimentology, 60, 1709–1732,
https://doi.org/10.1016/j.sedgeo.2008.06.007, 2013.
Coyle, D. A., Wagner, G. A., Hejl, E., Brown, R., and Van den Haute, P.:
The Cretaceous and younger thermal history of the KTB site (Germany):
apatite fission-track data from the Vorbohrung, Geol. Rundschau, 86, 203–209, https://doi.org/10.1007/s005310050132, 1997.
Durcan, J. A., King, G. E., and Duller, G. A. T.: DRAC: Dose Rate and Age
Calculator for trapped charge dating, Quaternary Geochr., 28, 54–61,
https://doi.org/10.1016/j.quageo.2015.03.012, 2015.
Duval, M.: Dose response curve of the ESR signal of the Aluminum center in
quartz grains extracted from sediment, Anc. TL, 30, 41–49, 2012.
Duval, M. and Guilarte, V.: ESR dosimetry of optically bleached quartz
grains extracted from Plio-Quaternary sediment: evaluating some key aspects
of the ESR signals associated to the Ti-centers, Rad. Meas., 78, 28–41,
https://doi.org/10.1016/j.radmeas.2014.10.002, 2015.
Grün, R.: Electron spin resonance (ESR) dating, Quternary Int., 1, 65–109, https://doi.org/10.1016/1040-6182(89)90010-4, 1989.
Grün, R. and Rhodes, E. J.: On the selection of dose points for saturating
exponential ESR/TL dose response curves, Anc. TL 9, 40–46, 1991.
Grün, R., Tani, A., Gurbanov, A., Koshchug, D., Williams, I., and
Braun, J.: A new method for the estimation of cooling and denudation rates
using paramagnetic centers in quartz: A case study on the Eldzhurtinskiy
Granite, Caucasus, J. Geophys. Res.-Solid Earth, 104, 17531–17549,
https://doi.org/10.1029/1999JB900173, 1999.
Guérin, G., Mercier, N., and Adamiec, G.: Dose-rate conversion factors:
update, Anc. TL, 29, 5–8, 2011.
Guérin, G., Mercier, N., Nathan, R., Adamiec, G., and Lefrais, Y.: On
the use of the infinite matrix assumption and associated concepts: a
critical review, Rad. Meas., 47, 778–785,
https://doi.org/10.1016/j.radmeas.2012.04.004, 2012.
Guralnik, B., Jain, M., Herman, F., Ankjærgaard, C., Murray, A. S.,
Valla, P. G., Preusser, F., King, G. E., Chen, R., Lowick, S. E., Kook, M.,
and Rhodes, E. J.: OSL-thermochronology of feldspar from the KTB borehole,
Germany, Earth Planet Sci. Lett. 423, 232–243,
https://doi.org/10.1016/j.epsl.2015.04.032, 2015.
Herman, F. and King, G. E.: Luminescence Thermochronometry: Investigating
the Link between Mountain Erosion, Tectonics and Climate, Elements, 14,
33–38, https://doi.org/10.2138/gselements.14.1.33, 2018.
Herman, F., Rhodes, E. J., Braun, J., and Heiniger, L.: Uniform erosion rates
and relief amplitude during glacial cycles in the Southern Alps of New
Zealand, as revealed from OSL-thermochronology, Earth Planet Sci. Lett.
297, 183–189, https://doi.org/10.1016/j.epsl.2010.06.019, 2010.
Huntley, D. J.: An explanation of the power-law decay of luminescence, J.
Phys.: Cond. Mat., 18, 1359–1365, https://doi.org/10.1088/0953-8984/18/4/020, 2006.
Huntley, D. J. and Baril, M. R.: The K content of the K-feldspars being
measured in optical dating or in thermoluminescence dating, Anc. TL, 15, 11–13, 1997.
Ikeya, M.: ESR studies of geothermal boring cores at Hachobara power
station, Japanese J. Appl. Phys., 22, p. L763,
https://doi.org/10.1143/JJAP.22.L763, 1983.
Ikeya, M.: New applications of electron spin resonance: dating, dosimetry
and microscopy, World Scientific, 1993.
Isoya, J., Weil, J. A., and Davis, P. H.: EPR of atomic hydrogen 1H and 2H
in α-quartz, J. Phys. Chem. Solids, 44, 335–343,
https://doi.org/10.1016/0022-3697(83)90102-6, 1983.
Ito, H., Yamada, R., Tamura, A., Arai, S., Horie, K., and Hokada, T.:
Earth's youngest exposed granite and its tectonic implications: the 10–0.8
Ma Kurobegawa Granite, Sci. Rep., 3, 1306,
https://doi.org/10.1038/srep01306, 2013.
Ito, H., Spencer, C. J., Danišík, M., and Hoiland, C.
W.: Magmatic tempo of Earth's youngest exposed plutons as revealed by
detrital zircon U-Pb geochronology, Sci. Rep., 7, 12457,
https://doi.org/10.1038/s41598-017-12790-w, 2017.
Kars, R. H., Wallinga, J., and Cohen, K. M.: A new approach towards anomalous
fading-correction for feldspar IRSL dating-tests on samples in field
saturation, Rad. Meas., 43, 786–790,
https://doi.org/10.1016/j.radmeas.2008.01.021, 2008.
King, G. E., Guralnik, B., Valla, P. G., and Herman, F.: Trapped-charge
thermochronometry and thermometry: A status review, Chem. Geol., 446, 3–17,
https://doi.org/10.1016/j.chemgeo.2016.08.023, 2016a.
King, G. E., Herman, F., and Guralnik, B.: Northward migration of the
eastern Himalayan syntaxis revealed by OSL
thermochronometry, Science, 353, 800–804, 10.1126/science.aaf2637,
2016b.
King, G. E., Herman, F., Lambert, R., Valla, P. G., and Guralnik, B.:
Multi-OSL-thermochronometry of feldspar, Quaternary Geochr., 33, 76–87,
https://doi.org/10.1016/j.quageo.2016.01.004, 2016c.
King, G. E., Burow, C., Roberts, H. M. R., and Pearce, N. J. P.: Age
determination using feldspar: evaluating fading-correction model
performance, Rad. Meas., 119, 55–73, https://doi.org/10.1016/j.radmeas.2018.07.013,
2018.
King, G. E., Tsukamoto, S., Herman, F., Biswas, R. H., Sueoka, S., and Tagami, T.: ESR-thermochronometry of the Hida range of the Japanese Alps: Validation and future potential, Data set, Geochronology, Zenodo, https://doi.org/10.5281/zenodo.3548747, 2019.
Lambert, R.: Investigating thermal decay in K-feldspar for the application
of IRSL thermochronometry on the Mont Blanc massif, Unpublished PhD Thesis,
University of Lausanne, Switzerland, 2018.
Li, B. and Li, S. H.: Luminescence dating of K-feldspar from sediments: a
protocol without anomalous fading correction, Quaternary Geochr., 6, 468–479,
https://doi.org/10.1016/j.quageo.2011.05.001, 2011.
Li, B. and Li, S. H.: The effect of band-tail states on the thermal
stability of the infrared stimulated luminescence from K-feldspar, J.
Lum., 136, 5–10, https://doi.org/10.1016/j.jlumin.2012.08.043, 2013.
Murray, A. S. and Wintle, A. G.: Luminescence dating of quartz using an improved
single-aliquot regenerative-dose protocol, Rad. Meas. 32, 57–73,
https://doi.org/10.1016/S1350-4487(99)00253-X, 2000.
Nuttall, R. H. D. and Weil, J. A.: The magnetic properties of the oxygen–hole
aluminum centers in crystalline SiO2. I.[AlO4]o, Can. J. Phys., 59, 1696–1708, https://doi.org/10.1139/p81-249, 1981.
Oppermann, F. and Tsukamoto, S.: A portable system of X-ray irradiation and
heating for electron spin resonance (ESR) dating, Anc. TL, 33, 11–15, 2015.
Poolton, N. R. J., Kars, R. H., Wallinga, J., and Bos, A. J. J.: Direct evidence
for the participation of band-tails and excited-state tunnelling in the
luminescence of irradiated feldspars, J. Phys.: Cond. Mat., 21,
485505, https://doi.org/10.1088/0953-8984/21/48/485505, 2009.
Press, W. H.: Numerical Recipes 3rd Edition: the Art of Scientific
Computing, Cambridge University Press, 2007.
Rees-Jones, J.: Optical dating of young sediments using fine-grain quartz,
Anc. TL, 13, 9–14, 1995.
Richter, M., Tsukamoto, S., and Long, H.: ESR dating of Chinese loess using the
quartz Ti centre: A comparison with independent age control, Quaternary Int.,
https://doi.org/10.1016/j.quaint.2019.04.003, in press, 2019.
Rink, W. J.: Electron spin resonance (ESR) dating and ESR applications in
Quaternary science and archaeometry, Rad. Meas., 27, 975–1025,
https://doi.org/10.1016/S1350-4487(97)00219-9, 1997.
Rinneberg, H. and Weil, J. A.: EPR Studies of Ti3+-H+ Centers in X-Irradiated α-Quartz, The J. Chem. Phys., 56,
2019–2028, https://doi.org/10.1063/1.1677493, 1972.
Scherer, T., Agel, A., and Hafner S. S.: Determination of uplift rates using ESR
investigations of quartz, KTB Rep. 93-2. Kontinentales Tiefbohrprogram der
Bundesrepublic Deutschland Niedersächs. Landesamt Bodenforsch.,
Hannover, 121–124, 1993.
Scherer, T., Plötze, M., and Hafner, S. S.: Paramagnetic defects of quartz
in KTB and a drilling profile from Eldzhurtinskiy Granite, Russia. KTB Rep.
94-2. B25, Kontinentales Tiefbohrprogram der Bundesrepublic Deutschland
Niedersächs, Landesamt Bodenforsch., Hannover, 1994.
Spencer, C. J., Danišík, M., Ito, H., Hoiland, C., Tapster, S.,
Jeon, H., McDonald, B., and Evans, N. J.: Rapid exhumation of Earth's
youngest exposed granites driven by subduction of an oceanic arc, Geophys.
Res. Lett., 46, 1259–1267, https://doi.org/10.1029/2018GL080579, 2019.
Sueoka, S., Tsutsumi, H., and Tagami, T.: New approach to resolve the amount
of Quaternary uplift and associated denudation of the mountain ranges in the
Japanese Islands, Geosc. Fron., 7, 197–210,
https://doi.org/10.1016/j.gsf.2015.06.005, 2016.
Tachiya, M. and Mozumder, A.: Decay of trapped electrons by tunnelling to
scavenger molecules in low temperature glasses, Chem. Phys. Lett. 28, 87–89, 1974.
Takahashi, M.: Tectonic Development of the Japanese Islands Controlled by
Philippine Sea Plate Motion, J. of Geography (Chigaku Zasshi) 115, 116–123,
https://doi.org/10.1016/0009-2614(74)80022-9, 2006 (in Japanese with English
Abstract).
Tissoux, H., Falguères, C., Voinchet, P., Toyoda, S., Bahain, J. J., and
Despriée, J.: Potential use of Ti-center in ESR dating of fluvial
sediment, Quaternary Geochr., 2, 367–372,
https://doi.org/10.1016/j.quageo.2006.04.006, 2007.
Townend, J. and Zoback, M. D.: Stress, strain, and mountain building in central
Japan, J. Geophys. Res.-Solid Earth (1978–2012), 111, B03411,
https://doi.org/10.1029/2005JB003759, 2006.
Toyoda, S. and Ikeya, M.: Thermal stabilities of paramagnetic defect and
impurity centers in quartz: Basis for ESR dating of thermal history, Geoch.
J., 25, 437–445, https://doi.org/10.2343/geochemj.25.437, 1991.
Tsukamoto, S., Toyoda, S., Tani, A., and Oppermann, F.: Single aliquot
regenerative dose method for ESR dating using X-ray irradiation and
preheat, Rad. Meas., 81, 9–15, https://doi.org/10.1016/j.radmeas.2015.01.018, 2015.
Tsukamoto, S., Long, H., Richter, M., Li, Y., King, G.E., He, Z., Yang, L.,
Zhang, J., and Lambert, R.: Quartz natural and laboratory ESR dose response
curves: A first attempt from Chinese loess, Rad. Meas., 120, 137–142,
https://doi.org/10.1016/j.radmeas.2018.09.008, 2018.
Valla, P. G., Lowick, S. E., Herman, F., Champagnac, J. D., Steer, P., and
Guralnik, B.: Exploring IRSL50 fading variability in bedrock feldspars and
implications for OSL thermochronometry, Quaternary Geoch., 36, 55–66,
https://doi.org/10.1016/j.quageo.2016.08.004, 2016.
Wheelock, B., Constable, S., and Key, K.: The advantages of logarithmically
scaled data for electromagnetic inversion, Geophys. J. Int., 201, 1765–1780,
https://doi.org/10.1093/gji/ggv107, 2015.
Woda, C. and Wagner, G. A.: Non-monotonic dose dependence of the Ge-and
Ti-centres in quartz, Rad. Meas., 42, 1441–1452,
https://doi.org/10.1016/j.radmeas.2007.03.003, 2007.
Yamada, R.: Cooling history analysis of granitic rock in the Northern Alps,
central Japan, The Earth Monthly, 21, 803–810, 1999 (in Japanese).
Yonekura, N., Kaizuga, S., Nogami, M., and Chinzei, K.: Introduction to
Japanese geomorphology, University of Tokyo Press, Tokyo, 2001 (in
Japanese).
Yuhara, K. and Yamamoto, T.: Thermal Effect of Water Flowing through
Fractures on the Cooling of Kurobe Jobu Railway Tunnel (Hot Tunnel), Central
Japan, J. Geothermal Res. Soc. of Japan, 5, 259–276, 1983.
Short summary
Rates of landscape evolution over the past million years are difficult to quantify. This study develops a technique which is able to measure changes in rock cooling rates (related to landscape evolution) over this timescale. The technique is based on the electron spin resonance dating of quartz minerals. Measurement protocols and new numerical models are proposed that describe these data, allowing for their translation into rock cooling rates.
Rates of landscape evolution over the past million years are difficult to quantify. This study...
