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Journal articles on the topic 'Cosmogenic'

Author: Grafiati

Published: 4 June 2021

Last updated: 20 February 2023

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1

Cockburn, Hermione A. P., and Michael A. Summerfield. "Geomorphological applications of cosmogenic isotope analysis." Progress in Physical Geography: Earth and Environment 28, no. 1 (2004): 1–42. http://dx.doi.org/10.1191/0309133304pp395oa.

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Cosmogenic isotope analysis involves the measurement of cosmogenic nuclides that have accumulated in the upper few metres of the Earth’s surface as a result of interactions between cosmic rays and target elements. The concentrations of these cosmogenic nuclides can provide quantitative estimates of the timing and rate of geomorphic processes. In dating applications the concentration of cosmogenic nuclides is interpreted as reflecting the time elapsed since a surface exposure event. However, over most of the Earth’s surface for most of the time the landsurface experiences incremental denudation

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2

Renne, Paul R., Kenneth A. Farley, Tim A. Becker, and Warren D. Sharp. "Terrestrial cosmogenic argon." Earth and Planetary Science Letters 188, no. 3-4 (2001): 435–40. http://dx.doi.org/10.1016/s0012-821x(01)00336-3.

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3

Damon, Paul E. "Cosmogenic Isotope Paleogeophysics - Paleoastrophysics and Natural Variation of Cosmogenic Isotopes." Radiocarbon 34, no. 2 (1992): vii—viii. http://dx.doi.org/10.1017/s0033822200013606.

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4

Veselova, Larysa, Khaini-Kamal Kasymkhanova, Umut Kozhakhmetova, et al. "Exomorphogenesis of Cosmogenic Ring Structures of Kazakhstan." Journal of Landscape Ecology 12, no. 1 (2019): 49–58. http://dx.doi.org/10.2478/jlecol-2019-0004.

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Abstract The use of materials for remote sensing of the Earth made it possible to identify a new type of crustal structures and features of their expression in relief. These are ring structures that complicate the structure of the studied structures of a linear type. As a result of the study of the morphology, geological and tectonic structure of ring structures, it was established that they represent formations of various origins: pluton-volcanic, cosmogenic, and anthropogenic. Cosmogenic structures of different ages and differ in various degrees of transformation. The relief of the identifie

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5

Ritter, Benedikt, Andreas Vogt, and Tibor J. Dunai. "Technical Note: Noble gas extraction procedure and performance of the Cologne Helix MC Plus multi-collector noble gas mass spectrometer for cosmogenic neon isotope analysis." Geochronology 3, no. 2 (2021): 421–31. http://dx.doi.org/10.5194/gchron-3-421-2021.

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Abstract. We established a new laboratory for noble gas mass spectrometry that is dedicated to the development and application to cosmogenic nuclides at the University of Cologne (Germany). At the core of the laboratory are a state-of-the-art high-mass-resolution multicollector Helix MC Plus (Thermo Fisher Scientific) noble gas mass spectrometer and a novel custom-designed automated extraction line. The mass spectrometer is equipped with five combined Faraday multiplier collectors, with 1012 and 1013 Ω pre-amplifiers for faraday collectors. We describe the extraction line and the automated pro

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6

Fabel, Derek, and Jon Harbor. "The use of in-situ produced cosmogenic radionuclides in glaciology and glacial geomorphology." Annals of Glaciology 28 (1999): 103–10. http://dx.doi.org/10.3189/172756499781821968.

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AbstractThe usefulness of in-situ produced cosmogenic radionuclides in constraining glacial chronologies through exposure-age dating has been demonstrated in numerous studies. However, an understanding of cosmogenic radionuclide techniques and their uncertainties opens up a wide range of other potential applications in glaciology and glacial geomorphology. Recently developed applications include: estimation of spatial and temporal variations in the depth of glacial erosion from cosmogenic radionuclide inheritance, which provides important constraints on process-based erosion models; and burial

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7

Tremblay, Marissa M., David L. Shuster, Matteo Spagnolo, Hans Renssen, and Adriano Ribolini. "Temperatures recorded by cosmogenic noble gases since the last glacial maximum in the Maritime Alps." Quaternary Research 91, no. 2 (2018): 829–47. http://dx.doi.org/10.1017/qua.2018.109.

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AbstractWhile proxy records have been used to reconstruct late Quaternary climate parameters throughout the European Alps, our knowledge of deglacial climate conditions in the Maritime Alps is limited. Here, we report temperatures recorded by a new and independent geochemical technique—cosmogenic noble gas paleothermometry—in the Maritime Alps since the last glacial maximum. We measured cosmogenic 3He in quartz from boulders in nested moraines in the Gesso Valley, Italy. Paired with cosmogenic 10Be measurements and 3He diffusion experiments on quartz from the same boulders, the cosmogenic 3He

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8

Gosse, John C., Robert C. Reedy, Charles D. Harrington, and Jane Poths. "Overview of the Workshop on Secular Variations in Production Rates of Cosmogenic Nuclides on Earth." Radiocarbon 38, no. 1 (1996): 135–47. http://dx.doi.org/10.1017/s0033822200061580.

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Measurements of cosmogenic nuclides made in situ in the Earth's surface are being used to help resolve a wide range of geologic and chronologic questions. Cosmogenic nuclides (3He, 10Be, 14C, 21Ne, 26Al 36C1 are presently used) can reveal rock exposure history information leading to estimates of timing of surface forming events, rates and styles of erosion, and timing and durations of episodes of burial. Depending on the problems being tackled, a significant source of error (±10–25%) for any cosmogenic nuclide method is the present uncertainty in the spatial and temporal variability of the rat

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9

Cebrián, Susana. "Cosmogenic activation of materials." International Journal of Modern Physics A 32, no. 30 (2017): 1743006. http://dx.doi.org/10.1142/s0217751x17430060.

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Experiments looking for rare events like the direct detection of dark matter particles, neutrino interactions or the nuclear double beta decay are operated deep underground to suppress the effect of cosmic rays. But, the production of radioactive isotopes in materials due to previous exposure to cosmic rays is a hazard when ultra-low background conditions are required. In this context, the generation of long-lived products by cosmic nucleons has been studied for many detector media and for other materials commonly used. Here, the main results obtained on the quantification of activation yields

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10

Ahlers, Markus. "High-energy Cosmogenic Neutrinos." Physics Procedia 61 (2015): 392–98. http://dx.doi.org/10.1016/j.phpro.2014.12.080.

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11

Handwerger, D. A., T. E. Cerling, and R. L. Bruhn. "Cosmogenic in carbonate rocks." Geomorphology 27, no. 1-2 (1999): 13–24. http://dx.doi.org/10.1016/s0169-555x(98)00087-7.

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12

Blard, Pierre-Henri, Maarten Lupker, and Moïse Rousseau. "Paired-cosmogenic nuclide paleoaltimetry." Earth and Planetary Science Letters 515 (June 2019): 271–82. http://dx.doi.org/10.1016/j.epsl.2019.03.005.

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13

Herpers, U., S. Vogt, K. Bremer, et al. "Cosmogenic nuclides in eucrites." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 52, no. 3-4 (1990): 612–17. http://dx.doi.org/10.1016/0168-583x(90)90485-d.

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14

Tremblay, Marissa M., David L. Shuster, and Greg Balco. "Cosmogenic noble gas paleothermometry." Earth and Planetary Science Letters 400 (August 2014): 195–205. http://dx.doi.org/10.1016/j.epsl.2014.05.040.

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15

Bhandari, N., J. N. Goswami, R. Jha, D. Sengupta, and P. N. Shukla. "Cosmogenic effects in shergottites." Geochimica et Cosmochimica Acta 50, no. 6 (1986): 1023–30. http://dx.doi.org/10.1016/0016-7037(86)90383-2.

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16

Briner, Jason P., Gifford H. Miller, P. Thompson Davis, and Robert C. Finkel. "Cosmogenic exposure dating in arctic glacial landscapes: implications for the glacial history of northeastern Baffin Island, Arctic Canada." Canadian Journal of Earth Sciences 42, no. 1 (2005): 67–84. http://dx.doi.org/10.1139/e04-102.

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Cosmogenic exposure dating and detailed glacial-terrain mapping from the Clyde Foreland, Baffin Island, Arctic Canada, reveal new information about the extent and dynamics of the northeastern sector of the Laurentide Ice Sheet (LIS) during the last glacial maximum (LGM). The Clyde Foreland is composed of two distinct landscape zones: (1) glacially scoured terrain proximal to the major sources of Laurentide ice that flowed onto the foreland, and (2) ice distal unscoured sectors of the foreland. Both zones are draped with erratics and dissected by meltwater channels, indicating past ice cover. W

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17

Lal, Devendra, and A. J. T. Jull. "Cosmogenic Nuclides in Ice Sheets." Radiocarbon 34, no. 2 (1992): 227–33. http://dx.doi.org/10.1017/s0033822200013667.

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We discuss the nature of the twofold record of cosmogenic nuclides in ice sheets, of nuclei produced in the atmosphere, and of nuclei produced in situ due to interactions of cosmic-ray particles with oxygen nuclei in ice. We show that a wealth of geophysical information, in principle, can be derived from a suitable combination of nuclides in ice deposited at different latitudes. Such knowledge includes temporal changes in the cosmic-ray flux, in the geomagnetic field and in climate. The rate of deposition of cosmogenic atmospheric nuclei in ice depends on the global cosmic-ray flux and a host

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18

Campbell, Mae Kate, Paul R. Bierman, Amanda H. Schmidt, et al. "Cosmogenic nuclide and solute flux data from central Cuban rivers emphasize the importance of both physical and chemical mass loss from tropical landscapes." Geochronology 4, no. 2 (2022): 435–53. http://dx.doi.org/10.5194/gchron-4-435-2022.

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Abstract. We use 25 new measurements of in situ produced cosmogenic 26Al and 10Be in river sand, paired with estimates of dissolved load flux in river water, to characterize the processes and pace of landscape change in central Cuba. Long-term erosion rates inferred from 10Be concentrations in quartz extracted from central Cuban river sand range from 3.4–189 Mg km−2 yr−1 (mean 59, median 45). Dissolved loads (10–176 Mg km−2 yr−1; mean 92, median 97), calculated from stream solute concentrations and modeled runoff, exceed measured cosmogenic-10Be-derived erosion rates in 18 of 23 basins. This d

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19

Wittkowski, David, and Karl-Heinz Kampert. "On the flux of high-energy cosmogenic neutrinos and the influence of the extragalactic magnetic field." Monthly Notices of the Royal Astronomical Society: Letters 488, no. 1 (2019): L119—L122. http://dx.doi.org/10.1093/mnrasl/slz083.

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ABSTRACT Cosmogenic neutrinos originate from interactions of cosmic rays propagating through the universe with cosmic background photons. Since both high-energy cosmic rays and cosmic background photons exist, the existence of high-energy cosmogenic neutrinos is certain. However, their flux has not been measured so far. Therefore, we calculated the flux of high-energy cosmogenic neutrinos arriving at the Earth on the basis of elaborate 4D simulations that take into account three spatial degrees of freedom and the cosmological time-evolution of the universe. Our predictions for this neutrino fl

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20

Alcalá-Reygosa, J. "El Último Máximo Glaciar local y la deglaciación de la Zona Volcánica Central Andina: El caso del volcán HualcaHualca y del altiplano de Patapampa (Sur de Perú)." Cuadernos de Investigación Geográfica 43, no. 2 (2017): 649. http://dx.doi.org/10.18172/cig.3231.

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The aim of this study is to constrain the timing of the deglaciation process since the Last Local Glacial Maximum in HualcaHualca volcano and Patapampa Altiplano, located in the Andean Central Volcanic Zone. Nine 36Cl cosmogenic surface exposure dating of moraine boulders as well as polished and striated bedrock surfaces are presented. The 36Cl cosmogenic exposure ages indicate that the glaciers reached their maximum extent at ~ 17 - 16 ka on the HualcaHualca volcano during the Heinrich 1 event and the Tauca paleolake cycle. Since then glaciers began to retreat until ~ 12 ka, when they went th

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21

Blinov, A. V., and M. N. Kremliovskij. "Reflection of Solar Activity Dynamics in Radionuclide Data." Radiocarbon 34, no. 2 (1992): 207–12. http://dx.doi.org/10.1017/s0033822200013631.

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Variability of solar magnetic activity manifested within sunspot cycles demonstrates features of chaotic behavior. We have analyzed cosmogenic nuclide proxy records for the presence of the solar activity signals. We have applied numerical methods of nonlinear dynamics to the data showing the contribution of the chaotic component. We have also formulated what kind of cosmogenic nuclide data sets are needed for investigations on solar activity.

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22

Mancuso, S., C. Taricco, P. Colombetti, S. Rubinetti, N. Sinha, and N. Bhandari. "Long-term evolution of the heliospheric magnetic field inferred from cosmogenic 44Ti activity in meteorites." Astronomy & Astrophysics 610 (February 2018): A28. http://dx.doi.org/10.1051/0004-6361/201730392.

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Typical reconstructions of historic heliospheric magnetic field (HMF) BHMF are based on the analysis of the sunspot activity, geomagnetic data or on measurement of cosmogenic isotopes stored in terrestrial reservoirs like trees (14C) and ice cores (10Be). The various reconstructions of BHMF are however discordant both in strength and trend. Cosmogenic isotopes, which are produced by galactic cosmic rays impacting on meteoroids and whose production rate is modulated by the varying HMF convected outward by the solar wind, may offer an alternative tool for the investigation of the HMF in the past

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23

Shinoki, Masataka. "Measurement of cosmogenic neutron production in SK-Gd." Journal of Physics: Conference Series 2156, no. 1 (2021): 012187. http://dx.doi.org/10.1088/1742-6596/2156/1/012187.

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Abstract The Super-Kamiokande-Gd (SK-Gd) experiment has started after adding the gadolinium (Gd) into ultra-pure water in the SK detector. SK-Gd dramatically improves the sensitivity to supernova relic neutrino searches by tagging neutrons. Cosmic-ray muons penetrating into the SK detector induce hadronic showers. Such muon often break oxygen nuclei in water and produce unstable radioactive isotopes and neutrons, which are major background sources for supernova relic neutrino searches. On the other hand, the cosmogenic neutrons produced by muons can be used for the detector calibration source.

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24

Oura, Y., M. Honda, M. Ebihara, K. Bajo, and K. Nagao. "Cosmogenic 45Sc in Gibeon iron meteorite by radioanalytical neutron activation analysis." Proceedings in Radiochemistry 1, no. 1 (2011): 383–86. http://dx.doi.org/10.1524/rcpr.2011.0068.

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Abstract Cosmogenic nuclides in many fragments of Gibeon iron meteorite have been studied by Honda and co-workers. They observed that their concentrations varied by 5 orders and found that Gibeon gives two different exposure ages using pair of stable noble gas isotopes and radinuclide. To assess one possible cause for the difference, namely loss of partial noble gases due to atmospheric heating of the incoming meteoroid, concentrations of non-volatile and stable cosmogenic 45Sc of Gibeon were determined by radiochemical neutron activation analysis (RNAA). For RNAA, a radiochemical procedure us

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25

MacCormack, Patricia. "Cosmogenic Acceleration: Futurity and Ethics." Philosophical Literary Journal Logos 28, no. 2 (2018): 67–77. http://dx.doi.org/10.22394/0869-5377-2018-2-67-77.

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26

Vogt, S., G. F. Herzog, and R. C. Reedy. "Cosmogenic nuclides in extraterrestrial materials." Reviews of Geophysics 28, no. 3 (1990): 253. http://dx.doi.org/10.1029/rg028i003p00253.

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27

Marrero, Shasta M., Fred M. Phillips, Marc W. Caffee, and John C. Gosse. "CRONUS-Earth cosmogenic 36Cl calibration." Quaternary Geochronology 31 (February 2016): 199–219. http://dx.doi.org/10.1016/j.quageo.2015.10.002.

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28

Balco, Greg. "Improving cosmogenic-nuclide burial dating." Quaternary International 279-280 (November 2012): 35. http://dx.doi.org/10.1016/j.quaint.2012.07.152.

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29

Stanev, Todor. "Cosmogenic neutrinos and gamma rays." Comptes Rendus Physique 15, no. 4 (2014): 349–56. http://dx.doi.org/10.1016/j.crhy.2014.02.013.

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30

GORHAM, PETER W. "THE ANITA COSMOGENIC NEUTRINO EXPERIMENT." International Journal of Modern Physics A 21, supp01 (2006): 158–62. http://dx.doi.org/10.1142/s0217751x06033556.

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We report on new limits on cosmic neutrino fluxes from the flight of the Antarctic Impulsive Transient Antenna (ANITA) prototype, dubbed ANITA-lite, which completed an 18.4 day flight of a long-duration balloon (LDB) payload in early 2004.

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31

Rodés, Ángel, and Daniel L. Evans. "Cosmogenic soil production rate calculator." MethodsX 7 (2020): 100753. http://dx.doi.org/10.1016/j.mex.2019.11.026.

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32

Clark, Douglas H., Paul R. Bierman, and Patrick Larsen. "Improving in Situ Cosmogenic Chronometers." Quaternary Research 44, no. 3 (1995): 367–77. http://dx.doi.org/10.1006/qres.1995.1081.

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33

Briner, Jason P., Caleb K. Walcott, Joerg M. Schaefer, et al. "Drill-site selection for cosmogenic-nuclide exposure dating of the bed of the Greenland Ice Sheet." Cryosphere 16, no. 10 (2022): 3933–48. http://dx.doi.org/10.5194/tc-16-3933-2022.

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Abstract. Direct observations of the size of the Greenland Ice Sheet during Quaternary interglaciations are sparse yet valuable for testing numerical models of ice-sheet history and sea level contribution. Recent measurements of cosmogenic nuclides in bedrock from beneath the Greenland Ice Sheet collected during past deep-drilling campaigns reveal that the ice sheet was significantly smaller, and perhaps largely absent, sometime during the past 1.1 million years. These discoveries from decades-old basal samples motivate new, targeted sampling for cosmogenic-nuclide analysis beneath the ice she

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34

Dehnert, Andreas, and Christian Schlüchter. "Sediment burial dating using terrestrial cosmogenic nuclides." E&G Quaternary Science Journal 57, no. 1/2 (2008): 210–25. http://dx.doi.org/10.3285/eg.57.1-2.8.

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Abstract. Burial dating using in situ produced terrestrial cosmogenic nuclides is a relatively new method to date sediments and quantify geomorphological processes such as erosion, accumulation and river incision. Burial dating utilises the decay of previously in situ produced cosmogenic nuclides and can be applied to sedimentary deposits such as cave fillings, alluvial fans, river terraces, delta deposits, and dunes. Using the established 10Be/26Al nuclide pair allows numerical dating of quartz bearing material from ~100 ka to 5 Ma, where other dateable material is often unavailable. To date,

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35

Wang, Yanyan, and Sean D. Willett. "Escarpment retreat rates derived from detrital cosmogenic nuclide concentrations." Earth Surface Dynamics 9, no. 5 (2021): 1301–22. http://dx.doi.org/10.5194/esurf-9-1301-2021.

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Abstract. High-relief great escarpments at passive margins present a paradoxical combination of high-relief topography but low erosion rates suggesting low rates of landscape change. However, vertical erosion rates do not offer a straightforward metric of horizontal escarpment retreat rates, so we attempt to address this problem in this paper. We show that detrital cosmogenic nuclide concentrations can be interpreted as a directionally dependent mass flux to characterize patterns of non-vertical landscape evolution, e.g., an escarpment characterized by horizontal retreat. We present two method

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36

Applegate, P. J., N. M. Urban, K. Keller, and R. B. Alley. "Modeling the statistical distributions of cosmogenic exposure dates from moraines." Geoscientific Model Development Discussions 2, no. 2 (2009): 1407–46. http://dx.doi.org/10.5194/gmdd-2-1407-2009.

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Abstract. Cosmogenic exposure dating provides a method for estimating the ages of glacial moraines deposited in the last ~105 years. Cosmic rays break atoms in surface rocks at predictable rates. Thus, the ages of moraines are directly related to the concentrations of cosmic ray-produced nuclides in rocks on the moraine surfaces, under ideal circumstances. However, many geomorphic processes may interfere with cosmogenic exposure dating. Because of these processes, boulders sometimes arrive at the moraines with preexisting concentrations of cosmogenic nuclides, or else the boulders are partly s

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37

Ivy-Ochs, Susan, and Florian Kober. "Surface exposure dating with cosmogenic nuclides." E&G Quaternary Science Journal 57, no. 1/2 (2008): 179–209. http://dx.doi.org/10.3285/eg.57.1-2.7.

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Abstract. In the last decades surface exposure dating using cosmogenic nuclides has emerged as a powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic nuclides are produced in rocks and sediment due to reactions induced by cosmic rays. Landforms ranging in age from a few hundred years to tens of millions of years can be dated (depending on rock or landform weathering rates) by measuring nuclide concentrations. In this paper the history and theory of surface exposure dating are reviewed followed by an extensive outline of the fields of application of the method.

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38

Allam, Diana, Yasmine Sabry Hegazi, Mohamed Atef Abo-Ashour, and Mahmoud Fathi Elalfi. "Cosmogenic Pattern Language: Toward an Architectural Language Based on the Cosmogenic Patterns of Pre-Modernism." Nexus Network Journal 23, no. 3 (2021): 689–716. http://dx.doi.org/10.1007/s00004-021-00547-y.

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39

Györe, Domokos, Luigia Di Nicola, David Currie, and Finlay M. Stuart. "New System for Measuring Cosmogenic Ne in Terrestrial and Extra-Terrestrial Rocks." Geosciences 11, no. 8 (2021): 353. http://dx.doi.org/10.3390/geosciences11080353.

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Cosmogenic Ne isotopes are used for constraining the timing and rate of cosmological and Earth surface processes. We combined an automated gas extraction (laser) and purification system with a Thermo Fisher ARGUS VI mass spectrometer for high through-put, high precision Ne isotope analysis. For extra-terrestrial material with high cosmogenic Ne concentrations, we used multi-collection on Faraday detectors. Multiple measurements (n = 26) of 1.67 × 10−8 cm3 air-derived 20Ne yielded an uncertainty of 0.32%, and 21Ne/20Ne = 0.17% and 22Ne/20Ne = 0.09%. We reproduced the isotope composition of cosm

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40

Ninglian, Wang, Yao Tandong, Qin Dahe, et al. "New evidence for enhanced cosmogenic isotope production rate in the atmosphere ∼37 ka BP." Annals of Glaciology 29 (1999): 136–40. http://dx.doi.org/10.3189/172756499781821076.

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AbstractA 36C1 peak has been found at about 37 ka BP in the Guliya ice core, drilled from the Qinghai-Tibetan Plateau. This peak is indicative of enhanced cosmogenic isotope production in the atmosphere, rather than a change in accumulation rate. Comparison with the records of 10Be and 36C1 in ice cores from Antarctica and Greenland indicates that peaks of the cosmogenic isotopes are global, and that they can be used as time markers for dating ice cores. Interestingly, the 37 ka BP global event coincided with a cold period.

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41

Rovey, Charles W., and Greg Balco. "Periglacial Climate at the 2.5 Ma Onset of Northern Hemisphere Glaciation Inferred from the Whippoorwill Formation, Northern Missouri, USA." Quaternary Research 73, no. 1 (2010): 151–61. http://dx.doi.org/10.1016/j.yqres.2009.09.002.

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The Whippoorwill Formation is a gleyed diamicton that is present locally within bedrock depressions beneath the oldest glacial till in northern Missouri, USA. Stratigraphy, paleomagnetism, and cosmogenic–nuclide burial ages show that it was deposited between the Matuyama–Gauss magnetostratigraphic boundary at 2.58 Ma and the first advance of the Laurentide ice sheet into Missouri at 2.47 ± 0.19 Ma. High cosmogenic–nuclide concentrations also show that the constituents of the Whippoorwill Formation experienced long exposure at a stable landscape surface with erosion rates of 1–2 m/Ma. However,

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42

Akcar, Naki, Susan Ivy-Ochs, and Christian Schlüchter. "Application of in-situ produced terrestrial cosmogenic nuclides to archaeology: A schematic review." E&G Quaternary Science Journal 57, no. 1/2 (2008): 226–38. http://dx.doi.org/10.3285/eg.57.1-2.9.

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Abstract. The wide applicability of in-situ produced Terrestrial Cosmogenic Nuclides (TCNs) to geological problems and experiences in development and testing gained over the past decade is encouraging for its application to archaeological questions, where there is a distinct need for an additional independent dating tool beyond the limits of radiocarbon (~ 40 ka). Just as TCNs are applicable to a broader time period with considerable precision in archaeology, so also are they applicable to all lithologies. Application of TCNs to archaeological problems is relatively simple: either surface expo

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43

Cerling, T. E. "Dating Geomorphologic Surfaces Using Cosmogenic 3He." Quaternary Research 33, no. 2 (1990): 148–56. http://dx.doi.org/10.1016/0033-5894(90)90015-d.

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AbstractCosmogenically produced 3He in rocks can be used to date geomorphologic surfaces. Using the Late Pleistocene Bonneville flood event, the subsequent development of the Provo shoreline, and associated volcanic rocks, a production rate of 432 atoms/g/yr in olivine is determined for 38°56′ N latitude (present geomagnetic latitude 46.5°) at 1445 m altitude integrated over the last 14,400 years. Measurements of cosmogenic helium in flood deposits, on river-scoured surfaces, and lava flows show that it is possible to date directly large-scale events such as volcanic eruptions and catastrophic

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44

Riihimaki, C. A., and J. C. Libarkin. "Terrestrial Cosmogenic Nuclides as Paleoaltimetric Proxies." Reviews in Mineralogy and Geochemistry 66, no. 1 (2007): 269–78. http://dx.doi.org/10.2138/rmg.2007.66.11.

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45

Fodor, Z., S. D. Katz, A. Ringwald, and H. Tu. "Bounds on the cosmogenic neutrino flux." Journal of Cosmology and Astroparticle Physics 2003, no. 11 (2003): 015. http://dx.doi.org/10.1088/1475-7516/2003/11/015.

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46

LAI, KWANG-CHANG, GUEY-LIN LIN, TSUNG-CHE LIU, JIWOO NAM, and CHI-CHIN CHEN. "COSMOGENIC TAU NEUTRINO INDUCED RADIO EMISSION." International Journal of Modern Physics: Conference Series 01 (January 2011): 157–62. http://dx.doi.org/10.1142/s2010194511000213.

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Cosmogenic neutrinos1 are expected from ultrahigh energy cosmic rays undergoing the GZK process2,3 and anticipated to be observed by detection of the air showers from the decays of tau leptons. We use CORSIKA simulated shower structure to Calculate the coherent geosynchrotron radio emissions of the tau decay showers above 1017 eV. We present the pattern and spectrum of the radio waves and discuss their detections by radio antennae.

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Gornostaeva, T. A., A. V. Mokhov, P. M. Kartashov, and O. A. Bogatikov. "Cosmogenic Substances in the Zhamanshin Crater." Doklady Earth Sciences 478, no. 2 (2018): 204–7. http://dx.doi.org/10.1134/s1028334x18020034.

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Belov, V. A. "EXO-200 results and cosmogenic backgrounds." Journal of Physics: Conference Series 798 (January 2017): 012102. http://dx.doi.org/10.1088/1742-6596/798/1/012102.

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Amidon, William H., Daniel Hobbs, and Scott A. Hynek. "Retention of cosmogenic 3He in calcite." Quaternary Geochronology 27 (April 2015): 172–84. http://dx.doi.org/10.1016/j.quageo.2015.03.004.

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Cerling, T. E., and H. Craig. "Geomorphology and In-Situ Cosmogenic Isotopes." Annual Review of Earth and Planetary Sciences 22, no. 1 (1994): 273–317. http://dx.doi.org/10.1146/annurev.ea.22.050194.001421.

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