Microdistribution of primordial noble gases in CM chondrites determined by in situ laser microprobe analysis: decipherment of nebular processes

1999 ◽  
Vol 63 (2) ◽  
pp. 241-255 ◽  
Author(s):  
Tomoki Nakamura ◽  
Keisuke Nagao ◽  
Nobuo Takaoka
1968 ◽  
Vol 22 (6) ◽  
pp. 758-760 ◽  
Author(s):  
Solomon F. Brokeshoulder ◽  
Farrel R. Robinson

Suitable microspectrochemical techniques have been devised for the laser microprobe made by the Jarrell—Ash Co. to detect beryllium in histologic structures. Density and type of tissue, thickness of the specimen, character of the embedding medium, concentration and localization of the element, and the penetrability of the laser beam must be considered in preparing biological specimens for chemical analysis by the microspectrochemical technique. Advantages of this technique are the identification of specific elements in situ and the correlation of the presence of the element with a specific histologic structure.


1998 ◽  
Vol 4 (S2) ◽  
pp. 278-279
Author(s):  
B.P. Bewlay ◽  
J.A. Sutliff

Directionally solidified in-situ composites based on niobium and niobium silicides, such as Nb5Si3 and Nb3Si, are presently under investigation as structural materials [1, 2], Alloying additions of elements such as Hf, Ti and Mo to these silicides are also being explored in order to increase strength and oxidation resistance. The present paper describes the effect of Hf, Mo and Ti additions on microstructure and microtexture of high temperature silcide-based in-situ composites.Alloys were prepared from high purity elements (>99.9%) using induction levitation melting in a segmented water-cooled copper crucible. The alloys were directionally solidified using the Czochralski method [2], Phase identification was performed using scanning electron microscopy, electron microprobe analysis (EMPA), and automated electron back scattering pattern (EBSP) analysis. Using EBSP, positive phase identification was accomplished by direct comparison of the location and character of the diffraction bands in the experimental pattern with those calculated from simulated patterns generated using the possible structure types.


Clay Minerals ◽  
1988 ◽  
Vol 23 (4) ◽  
pp. 423-437 ◽  
Author(s):  
P. Quantin ◽  
J. Gautheyrou ◽  
P. Lorenzoni

AbstractThe weathering of a trachytic pumice within a pyroclastic flow underlying an andic-brown soil on the volcano Vico has been studied. The main mineral formed is a spherical 10 Å halloysite which has been shown by SEM and in situ microprobe analysis to have formed directly from the glass. The major mineralogical characteristics as determined by XRD, IR, DTA, TEM and microdiffraction are typical of 10 Å halloysite. However, some minor mineralogical properties and the high Fe and K contents, suggest that it is an interstratification of 74% halloysite and 26% illite-smectite. The calculated formula of the hypothetical 2:1 minerals reveals an Fe- and K-rich clay, with high tetrahedral substitution, like an Fe-rich vermiculite, but the detailed structure of this mineral remains uncertain.


1993 ◽  
Vol 33 (1) ◽  
pp. 36-42 ◽  
Author(s):  
Mark A. Lovell ◽  
William D. Ehmann ◽  
William R. Markesbery

1995 ◽  
Vol 177 (1) ◽  
pp. 83-94 ◽  
Author(s):  
Theodore C. Iancu ◽  
Hanna Shiloh ◽  
Kishor B. Raja ◽  
Robert J. Simpson ◽  
Timothy J. Peters ◽  
...  

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