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Volumn 284, Issue 5411, 1999, Pages 128-132

Clinoenstatite in Alpe Arami peridotite: Additional evidence of very high pressure

Author keywords

[No Author keywords available]

Indexed keywords

MINERAL;

EID: 0033515829     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.284.5411.128     Document Type: Article
Times cited : (121)

References (75)
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    • note
    • Viewed down b, brightfield images and darkfield images with h + k = even show very similar mottling of contrast within clinoenstatite lamellae; the size, shape, and orientation of contrast domains are the same. Figure 3 shows that this mottling is primarily due to inhomogeneous elastic distortion. For example, the (100) fringes in the brightest region of Fig. 3 are rotated clockwise relative to the domains on either side of it. There are no crystal defects associated with the boundaries of the bright region. In addition, the fringe terminations do not show long-range strain fields; they do not represent dislocations. Therefore, the fringe offsets are growth features; symmetry rules forbid them to be a consequence of elastic strain.
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    • This work was partially supported by NSF grants EAR94-13517 and EAR96-283432. We thank R. J. Angel, F. E. Brenker, W. G. Ernst, B. Hacker, G. Nord, C. Prewitt, P. Robinson, N. L. Ross, T. Sharp, H. L. M. van Roermund, A. B. Woodland, and two anonymous reviewers for helpful discussions and suggestions
    • This work was partially supported by NSF grants EAR94-13517 and EAR96-283432. We thank R. J. Angel, F. E. Brenker, W. G. Ernst, B. Hacker, G. Nord, C. Prewitt, P. Robinson, N. L. Ross, T. Sharp, H. L. M. van Roermund, A. B. Woodland, and two anonymous reviewers for helpful discussions and suggestions.


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