Dietary exposure levels to <sup>134</sup>Cs, <sup>137</sup>Cs, <sup>90</sup>Sr, and <sup>239+240</sup>Pu in Japan after the Fukushima Daiichi Nuclear Power Plant accident: a duplicate portion study for fiscal years 2012-2014. [PDF]
Terada H+6 more
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Primordial neon and the deep mantle origin of kimberlites. [PDF]
Giuliani A+10 more
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Trans-Saharan migratory patterns in Vanessa cardui and evidence for a southward leapfrog migration. [PDF]
Reich MS+12 more
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Thoron, radon and microbial community as supportive indicators of seismic activity in groundwater. [PDF]
Kim J, Kim H, Kaown D, Lee KK.
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Family relations of Moche elite burials on the North Coast of Peru (~500 CE): Analyses of the Señora de Cao and relatives. [PDF]
Quilter J+9 more
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The character of Lake Kishkensor contamination in the area of underground nuclear explosions at the Semipalatinsk Test Site territory. [PDF]
Aidarkhanova A+7 more
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Local agricultural transition, crisis and migration in the Southern Andes
Rascovan N+38 more
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High-Resolution Stratigraphy with Strontium Isotopes [PDF]
The isotopic ratio of strontium-87 to strontium-86 shows no detectable variation in present-day ocean water but changes slowly over millions of years. The strontium contained in carbonate shells of marine organisms records the ratio of strontium-87 to strontium-86 of the oceans at the time that the shells form. Sedimentary rocks composed of accumulated
Donald J. DePaolo, Bonnye L. Ingram
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Dating phosphogenesis with strontium isotopes
Geochimica et Cosmochimica Acta, 1990Authigenic and replacement francolites in modern phosphorite have values of {sup 87}Sr/{sup 86}Sr within error of that of modern marine Sr (0.70916 {plus minus} 2). During the phosphatisation of carbonate, Sr is not inherited from the carbonate but is totally exchanged with Sr in ambient water. The {sup 87}Sr/{sup 86}Sr in shallow marine pore waters is
P. J. Hamilton+4 more
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Strontium and Neodymium Isotopes
2019The chapter presents data on Rb–Sr and Sm–Nd TIMS analysis of pyroxenes, plagioclases, gross samples of igneous rocks and sulphide ores. In most Sm–Nd analyses of minerals, the isotope system (pyroxene–plagioclase) does not reflect the age of intrusions and shows a rejuvenated or aged isochronous age.
Boris Belyatsky+3 more
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