
52 行 Strontium decay mostly in its neighbours: yttrium (lower neighbour) and rubidium (upper neighbour). The longest-lived of these isotopes, and the most relevantly studied are 90 Sr with a half-life of 28.9 years and 85 Sr with a half-life of 64.853 days. Of importance are also strontium-89 (89 Sr) with a half-life of 50.57 days. They decay with:



03.11.2011 Oxygen isotope data are very useful in determining the source rocks of granitic magmas, particularly when used in combination with Sr, Pb, and Nd isotope studies. For example, unusually high δ 18 O values in magmas (δ 18 O> +8) require the involvement of some precursor parent material that at some time in the past resided on or near the Earth's surface, either as sedimentary rocks or as ...

Strontium isotopes of sulfate minerals in VMS deposits (e.g., barite, carbonate, gypsum, and anhydrite) and in altered whole rocks invariably record a mixture of Sr derived from seawater and Sr leached from the underlying volcanic rocks, as well as variation in the isotopic composition of seawater Sr over time.

The element strontium has four naturally occurring isotopes – all are stable: 84Sr, 86Sr, 87Sr, and 88Sr. Only 87Sr is radiogenic – produced by the β-decay of 87Rb with a half-life of 48.8 billion years.

For example, very old rocks, such as granites and shales, have higher strontium 87 to 86 ratios than younger rocks. So the main type or types of rocks underlying where you live, referred to as bedrock, will give you a strontium isotope signature that varies from geographic areas composed of different bedrock. This figure shows the strontium-87 to 86 values of bedrock from the United States ...

The Rb-Sr dating method has been used extensively in dating terrestrial and lunar rocks, and meteorites. If the initial amount of Sr is known or can be extrapolated, the age can be determined by measurement of the Rb and Sr concentrations and the Sr/ Sr ratio. The dates indicate the true age of the minerals only if the rocks have not been subsequently altered. The important concept in isotopic tracing is that Sr derived from any mineral through weathering reactio

Naturat variations of strontium isotopes in continental granites {dots) and ocean basahs over geological time (after Faure Powell, 1972). o 0~ 00.. z.O00 - 0.735 - 0.730 0.725,_ 0.720 0.715 "5. 0.710 - 0.705 0.700 3000 2000 1000 Present Time in millions of years It is important to note that the strontium values fbr continental granites are linearly correlated with geological age.

The 87Sr enrichment is high in old continental rocks (granites) and low 87/86 ratios are found in the mantle and rocks derived from it (basalts). Therefore the Sr isotope

Oxygen and strontium isotope data for 25 late Caledonian granite plutons emplaced between ∼435 and 390 Myr indicate that the parent magmas were hybrids, derived from partial fusion of mantle ...

Strontiumisotope, das Erdalkalimetall Strontium besitzt vier natürlich vorkommende stabile Isotope: 88 Sr (ca. 82,58%), 87 Sr (ca. 7,00%), 86 Sr (ca. 9,86%), 84 Sr (ca. 0,56%). Die genauen Anteile der jeweiligen Isotope hängen von der Häufigkeit des radiogenen 87 Sr ab, welches z.T. aus dem β--Zerfall des 87 Rb entstanden ist (Halbwertszeit=4,88Â10 10 Jahre).

Strontium Isotope Geology by G. Faure, 9783642653698, available at Book Depository with free delivery worldwide.

Additional Physical Format: Online version: Faure, Gunter. Strontium isotope geology. Berlin, New York, Springer-Verlag, 1972 (OCoLC)655706293: Material Type:

OSTI.GOV Journal Article: A CONSIDERATION ON THE INITIAL STRONTIUM ISOTOPIC COMPOSITION IN GRANITES. A CONSIDERATION ON THE INITIAL STRONTIUM ISOTOPIC COMPOSITION IN GRANITES. (in Japanese) Full Record; Other Related Research; Authors: Kagami, H. Publication Date: Wed Jan 01 00:00:00 EST 1969 Research Org.: Tokyo Univ. Sponsoring Org.:

The element strontium has four naturally occurring isotopes – all are stable: 84 Sr, 86 Sr, 87 Sr, and 88 Sr. Only 87 Sr is radiogenic – produced by the β-decay of 87 Rb with a half-life of 48.8 billion years. In geologic and environmental investigations, the ratio of 87 Sr/ 86 Sr is typically used because of their similar abundances – 7% and 10%, respectively.

There are many works on fractionation of isotopes of Fe, Si, Mg (e.g. (Goel et al., 2012; Huang et al., 2009; Lacks et al., 2012; Wu et al., 2018; Zhu et al., 2015)), calcium (e.g.(Wang (王阳 ...

Naturat variations of strontium isotopes in continental granites {dots) and ocean basahs over geological time (after Faure Powell, 1972). o 0~ 00 .. z.O00 - 0.735 - 0.730 0.725 ,_ 0.720 0.715 "5 . 0.710 - 0.705 0.700 3000 2000 1000 Present Time in millions of years It is important to note that the strontium values fbr continental granites are linearly correlated with geological age. This ...

The rubidium-strontium pair is often used for dating and has a non-radiogenic isotope, strontium-86, which can be used as a check on original concentrations of the isotopes. This process is often used along with potassium-argon dating on the same rocks. The ratios of rubidium-87 and strontium-87 to the strontium-86 found in different parts of a rock sample can be plotted against each other in ...

Il arrive que le strontium soit un élément majeur de certains minéraux, c'est le cas notamment du carbonate de strontium de formule SrCO 3 (strontianite) ou du sulfate de strontium SrSO 4 . Ces deux éléments existent dans la nature sous la forme de plusieurs isotopes , deux pour le rubidium, 85 Rb et 87 Rb et quatre pour le strontium, 84 Sr, 86 Sr , 87 Sr et 88 Sr. Seul l'un d'entre eux ...

Strontium Isotope Geology by G. Faure, 9783642653698, available at Book Depository with free delivery worldwide.

There are many works on fractionation of isotopes of Fe, Si, Mg (e.g. (Goel et al., 2012; Huang et al., 2009; Lacks et al., 2012; Wu et al., 2018; Zhu et al., 2015)), calcium (e.g.(Wang (王阳 ...

Strontium 90 Sr ist eines der energiereichsten, langlebigen Isotope, die Betastrahlung aussenden. Weiter verstärkt wird die Strahlung durch das Yittrium 90 Y dessen Zerfallsenergie ca. 4 mal so hoch ist wie die des Strontiumisotops. Daher wird es in Isotopenbatterien verwendet. 90 Sr entsteht in Kernreaktoren und bei Atombombenexplosionen.

Strontium Isotope Analysis Strontium isotopic ratios are widely used as tracers in geological processes and as indicators of provenance in an archaeological context. A significant fraction of the Earth’s 87 Sr is not primordial, but is produced by the decay of 87 Rb.

Geology and Strontium Isotopes in the Danube Gorges. The geology of the region is remarkably complex ().The route of the Danube, connecting the Carpathian and the Dacian Basins through the Danube Gorges, is composed of three smaller valleys and four gorges (42, 43).The rock formations of the Danube Gorges themselves are dominated by limestone massifs with typical karst topography in the

Strontium hat vier stabile, natürlich vorkommende Isotope: 84 Sr (0,56 %), 86 Sr (9,86 %), 87 Sr (7,0 %) und 88 Sr (82,58 %). 87 Sr entsteht beim β − -Zerfall des Rubidium -Isotops 87 Rb mit einer Halbwertszeit von 4,81 10 10 a.

Naturally occurring isotopes of elements like strontium have proved to be good tools for tracing the past and for monitoring of processes in the present. The spread and variation in 87Sr/86Sr ratios make Sr isotopes a powerful tool when it comes to detecting trends in the soil-vegetation system. There is also a great potential in combining different parameters like soil, water, biological ...

strontium isotopes” in reference to 87Sr/86Sr values so as to distinguish this kind of data from recent paleodietary research (Knudson et al. 2010) that utilizes stable d88Sr/86Sr signatures. M. Baskaran (ed.), Handbook of Environmental Isotope Geochemistry, Advances in Isotope Geochemistry,

There are four natural isotopes of Sr, 3 non- radiogenic (84Sr,86Sr, and88Sr) and 1 radiogenic, the product of radioactive decay.

Ces deux éléments existent dans la nature sous la forme de plusieurs isotopes, deux pour le rubidium, 85 Rb et 87 Rb et quatre pour le strontium, 84 Sr, 86 Sr, 87 Sr et 88 Sr. Seul l'un d'entre eux, le 87 Rb, est radioactif. Il se désintègre en 87 Sr qui, lui, est un isotope stable du