Academic literature on the topic 'Mono Lake excursion'

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Journal articles on the topic "Mono Lake excursion"

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Kent, D. V., S. R. Hemming, and B. D. Turrin. "Laschamp Excursion at Mono Lake?" Earth and Planetary Science Letters 197, no. 3-4 (April 2002): 151–64. http://dx.doi.org/10.1016/s0012-821x(02)00474-0.

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Liddicoat, Joseph C. "Mono Lake Excursion in Mono Basin, California, and at Carson Sink and Pyramid Lake, Nevada." Geophysical Journal International 108, no. 2 (February 1992): 442–52. http://dx.doi.org/10.1111/j.1365-246x.1992.tb04627.x.

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Benson, Larry, Joseph Liddicoat, Joseph Smoot, Andrei Sarna-Wojcicki, Robert Negrini, and Steve Lund. "Age of the Mono Lake excursion and associated tephra." Quaternary Science Reviews 22, no. 2-4 (February 2003): 135–40. http://dx.doi.org/10.1016/s0277-3791(02)00249-4.

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Liddicoat, Joseph C. "Research Note Mono Lake Excursion In the Lahontan Basin, Nevada." Geophysical Journal International 125, no. 2 (May 1996): 630–35. http://dx.doi.org/10.1111/j.1365-246x.1996.tb00025.x.

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Negrini, Robert M., Daniel T. McCuan, Robert A. Horton, James D. Lopez, William S. Cassata, James E. T. Channell, Kenneth L. Verosub, et al. "Nongeocentric axial dipole field behavior during the Mono Lake excursion." Journal of Geophysical Research: Solid Earth 119, no. 4 (April 2014): 2567–81. http://dx.doi.org/10.1002/2013jb010846.

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Voelker, Antje H. L., Pieter M. Grootes, Marie-Josee Nadeau, and Michael Sarnthein. "Radiocarbon Levels in the Iceland Sea from 25–53 kyr and their Link to the Earth's Magnetic Field Intensity." Radiocarbon 42, no. 3 (2000): 437–52. http://dx.doi.org/10.1017/s0033822200030368.

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By correlating the climate records and radiocarbon ages of the planktonic foraminifera N. pachyderma(s) of deep-sea core PS2644 from the Iceland Sea with the annual-layer chronology of the GISP2 ice core, we obtained 80 marine 14C calibration points for the interval 11.4-53.3 ka cal BP. Between 27 and 54 ka cal BP the continuous record of 14C/cal age differences reveals three intervals of highly increased 14C concentrations coincident with low values of paleomagnetic field intensity, two of which are attributed to the geomagnetic Mono Lake and Laschamp excursions (33.5-34.5 ka cal BP with maximum 550 marine δ14C, and 40.3-41.7 ka cal BP with maximum 1215 marine δ14C, respectively). A third maximum (marine δ14C: 755) is observed around 38 ka cal BP and attributed to the geomagnetic intensity minimum following the Laschamp excursion. During all three events the A14C values increase rapidly with maximum values occurring at the end of the respective geomagnetic intensity minimum. During the Mono Lake Event, however, our A14C values seem to underestimate the atmospheric level, if compared to the 36Cl flux measured in the GRIP ice core (Wagner et al. 2000) and other records. As this excursion coincides with a meltwater event in core PS2644, the underestimation is probably caused by an increased planktonic reservoir age. The same effect also occurs from 38.5 to 40 ka cal BP when the meltwater lid of Heinrich Event 4 affected the planktonic record.
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Mankinen, Edward A., and Carl M. Wentworth. "Mono Lake excursion recorded in sediment of the Santa Clara Valley, California." Geochemistry, Geophysics, Geosystems 5, no. 2 (February 2004): n/a. http://dx.doi.org/10.1029/2003gc000592.

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Brown, Maxwell, Monika Korte, Richard Holme, Ingo Wardinski, and Sydney Gunnarson. "Earth’s magnetic field is probably not reversing." Proceedings of the National Academy of Sciences 115, no. 20 (April 30, 2018): 5111–16. http://dx.doi.org/10.1073/pnas.1722110115.

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The geomagnetic field has been decaying at a rate of ∼5% per century from at least 1840, with indirect observations suggesting a decay since 1600 or even earlier. This has led to the assertion that the geomagnetic field may be undergoing a reversal or an excursion. We have derived a model of the geomagnetic field spanning 30–50 ka, constructed to study the behavior of the two most recent excursions: the Laschamp and Mono Lake, centered at 41 and 34 ka, respectively. Here, we show that neither excursion demonstrates field evolution similar to current changes in the geomagnetic field. At earlier times, centered at 49 and 46 ka, the field is comparable to today’s field, with an intensity structure similar to today’s South Atlantic Anomaly (SAA); however, neither of these SAA-like fields develop into an excursion or reversal. This suggests that the current weakened field will also recover without an extreme event such as an excursion or reversal. The SAA-like field structure at 46 ka appears to be coeval with published increases in geomagnetically modulated beryllium and chlorine nuclide production, despite the global dipole field not weakening significantly in our model during this time. This agreement suggests a greater complexity in the relationship between cosmogenic nuclide production and the geomagnetic field than is commonly assumed.
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Ticich, T., L. Lundberg, D. K. Pal, C. M. Smith, G. F. Herzog, R. K. Moniot, C. Tuniz, W. Savin, T. H. Kruse, and J. C. Liddicoat. "10Be contents of Mono Lake sediments: search for enhancement during a geomagnetic excursion." Geophysical Journal International 87, no. 2 (November 1, 1986): 487–92. http://dx.doi.org/10.1111/j.1365-246x.1986.tb06633.x.

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Cassidy, John, and Mimi J. Hill. "Absolute palaeointensity study of the Mono Lake excursion recorded by New Zealand basalts." Physics of the Earth and Planetary Interiors 172, no. 3-4 (February 2009): 225–34. http://dx.doi.org/10.1016/j.pepi.2008.09.018.

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Book chapters on the topic "Mono Lake excursion"

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Krainov, M. A., E. V. Bezrukova, A. A. Shchetnikov, and A. Yu Peskov. "Evidence for the Existence of the Gothenburg and Mono Lake Excursions Based on Paleomagnetic Data from Baunt Lake Sediments (Northern Transbaikalia)." In Springer Geophysics, 55–65. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90437-5_5.

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Conference papers on the topic "Mono Lake excursion"

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Herrero-Bervera, Emilio, and Brian R. Jicha. "FULL VECTOR AND 40AR/39AR STUDY OF AN EXCURSION RECORDED BY THE KAUPO FLOW, HONOLULU VOLCANIC SERIES, OAHU, HAWAII, USA: A VOLCANIC RECORD OF THE MONO LAKE EXCURSION." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363149.

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