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The amphibole structure was confirmed by electron diffraction and HRTEM imaging. The amphibole slabs are typically one to two unit cells thick parallel to b; in rare cases they reach a thickness of about 10 unit cells. In some cases, generally near the dinoenstatite lamellae tips, the amphibole slabs traverse the lamellae. Mostly, however, they run up to the lamellae boundaries and go around them, as typically observed during the hydration of complex exsolved pyroxenes [D. R. Veblen and P. R. Buseck, Am. Mineral. 65, 599 (1980), D. R. Veblen and D. L. Bish, ibid. 73, 677 (1988), K. J. T. Livi and D. R. Veblen, ibid. 74, 1070 (1989)].
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The amphibole structure was confirmed by electron diffraction and HRTEM imaging. The amphibole slabs are typically one to two unit cells thick parallel to b; in rare cases they reach a thickness of about 10 unit cells. In some cases, generally near the dinoenstatite lamellae tips, the amphibole slabs traverse the lamellae. Mostly, however, they run up to the lamellae boundaries and go around them, as typically observed during the hydration of complex exsolved pyroxenes [D. R. Veblen and P. R. Buseck, Am. Mineral. 65, 599 (1980), D. R. Veblen and D. L. Bish, ibid. 73, 677 (1988), K. J. T. Livi and D. R. Veblen, ibid. 74, 1070 (1989)].
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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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1/c transformation with an overstepping of the phase boundary by ∼1 GPa (14). The most striking differences between HTclen and HPclen are in density (Δp ∼ 3%) and in the different degree of kinking of the silicate tetrahedral chains [expressed macroscopically as different angles of monoclinicity (β) ∼110° in HTclen and ∼101° in Hpclen].
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The generally close association between the boundaries of strain domains and arrays of lattice fringe offsets within clinoenstatite lamellae suggests a relationship between them. Figure 1, B and C, and Fig. 2A show that the scale of strain inhomogeneity in the lamellae is grossly different from that in the host and that the latter is related to the presence of the lamellae. There are no similar strain effects in diopside crystals that lack clinoenstatite lamellae, nor are such effects present within or around amphibole lamellae. A natural explanation for these correlations and the strain itself is the possibility that the strain pattern is a consequence of the 3% volume expansion that accompanies the HPclen→Lclen inversion. Multiple nucleation sites of the stable phase along the host-daughter interface would lead to "puckering" of the lattice due to local anisotropic expansion in a lamella contained within an essentially rigid framework (its coherent boundaries with the host). The regions of greatest curvature could, in turn, prejudice nucleation of additional antiphase domains. This scenario, although not a proven process, is consistent with the available evidence and provides a reasonable explanation for the pattern of strain and its relationship to the antiphase boundaries.
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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
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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.
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