Use of lead isotopic ratios to discriminate glass samples in forensic science

2011 ◽  
Vol 26 (2) ◽  
pp. 325-333 ◽  
Author(s):  
Knut-Endre Sjåstad ◽  
Siri Lene Simonsen ◽  
Tom Andersen
1995 ◽  
Vol 311 (2) ◽  
pp. 141-151 ◽  
Author(s):  
W. Chisholm ◽  
K.J.R. Rosman ◽  
C.F. Boutron ◽  
J.P. Candelone ◽  
S. Hong

Chemosphere ◽  
2018 ◽  
Vol 197 ◽  
pp. 152-164 ◽  
Author(s):  
Avijit Das ◽  
Subhra Sarita Patel ◽  
Rajeev Kumar ◽  
K.V.S.S. Krishna ◽  
Saikat Dutta ◽  
...  

Talanta ◽  
2013 ◽  
Vol 105 ◽  
pp. 158-166 ◽  
Author(s):  
Agnieszka Martyna ◽  
Knut-Endre Sjastad ◽  
Grzegorz Zadora ◽  
Daniel Ramos

1973 ◽  
Vol 10 (12) ◽  
pp. 1782-1789 ◽  
Author(s):  
G. L. Cumming ◽  
P. J. Gudjurgis

Isotope analyses on leads in iron sulfides and trace galenas from two deposits (Big Ledge, British Columbia and Quemont Mine, Quebec) suggest that variations in the isotopic composition may be influenced by postmineralization alteration of ore. It is postulated that when the ore has been subject to regional metamorphism after emplacement, the metamorphism has homogenized the lead isotope ratios throughout the ore body as appears to have happened at Big Ledge, whereas, if postore activity is limited to minor hydrothermal alteration, as at Quemont, then the lead may be left with a wide range of isotopic composition.


1987 ◽  
Vol 24 (10) ◽  
pp. 2089-2098 ◽  
Author(s):  
John N. Aleinikoff ◽  
Cynthia Dusel-Bacon ◽  
Helen L. Foster ◽  
Warren J. Nokleberg

Common lead isotopic compositions have been determined on feldspars from meta-igneous rocks from nine tectono-stratigraphic terranes or subterranes in east-central Alaska. Most of the terranes have distinct and well-defined signatures in terms of isotopic composition; thus, most can be distinguished on conventional lead isotopic diagrams. Lead isotopic ratios provide evidence for (1) possible sources for the igneous rocks, (2) time of metamorphism, (3) correlation of terrane fragments, and (4) delineation of juxtaposed terranes. Determination of lead isotopic ratios from igneous rocks can be useful in characterizing tectono-stratigraphic terranes (as to mantle or crustal origin) and in correlation, particularly where terrane relationships are enigmatic.


2018 ◽  
Vol 25 (26) ◽  
pp. 26653-26668 ◽  
Author(s):  
Sandrine Chifflet ◽  
David Amouroux ◽  
Sylvain Bérail ◽  
Julien Barre ◽  
Thuoc Chu Van ◽  
...  

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