Neutron activation-induced beta autoradiography as a technique for locating minor phases in thin section; application to rare earth element and platinum-group element mineral analysis

1984 ◽  
Vol 79 (4) ◽  
pp. 738-747 ◽  
Author(s):  
Philip J. Potts
1993 ◽  
Vol 57 (389) ◽  
pp. 607-611 ◽  
Author(s):  
Ken Shibata ◽  
Hikari Kamioka ◽  
Felix V. Kaminsky ◽  
Vassili I. Koptil ◽  
Darcy P. Svisero

AbstractCarbonado and yakutite are both porous aggregates of polycrystalline micrometre-size diamond, with very different characters from those of monocrystalline diamond. The genesis of carbonado is very controversial, whereas yakutite is thought to have been formed by meteorite impact. Neutron activation analyses of trace elements in carbonado and yakutite indicate that their rare earth element (REE) abundance patterns have common characteristics: heavy REEs are not much depleted and a negative Eu anomaly is observed. These patterns are quite different from those of kimberlite and monocrystalline diamond and are similar to those of crustal materials such as shale, supporting the hypothesis of a crustal origin for carbonado and yakutite.


2003 ◽  
Vol 258 (3) ◽  
pp. 531-535 ◽  
Author(s):  
S. M. B. Oliveira ◽  
F. E. Larizzatti ◽  
D. I. T. Fávaro ◽  
S. R. D. Moreira ◽  
B. P. Mazzilli ◽  
...  

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