1998
DOI: 10.1524/9783486598858
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Einführung in die Kristallographie

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Cited by 72 publications
(38 citation statements)
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“…The honeycomb row end points are located along a tilt grain boundary, where slightly inclined superstructure rows meet. This tilt grain boundary in an epitaxial monolayer film is the two-dimensional analogy to the well-known tilt grain boundaries in three-dimensional crystals [262].…”
Section: Defect Structuressupporting
confidence: 52%
See 1 more Smart Citation
“…The honeycomb row end points are located along a tilt grain boundary, where slightly inclined superstructure rows meet. This tilt grain boundary in an epitaxial monolayer film is the two-dimensional analogy to the well-known tilt grain boundaries in three-dimensional crystals [262].…”
Section: Defect Structuressupporting
confidence: 52%
“…Here, the fast growing ( ) 21 1 planes eventually disappear and the slow growing stable ( ) 111 surface planes remain, leading to large triangular islands that expose only ( ) 111 facets, as indicated in Fig. 5.25 [262]. The formation of triangular shaped islands rotated by 180° indicates the existence of two in-plane orientations of Fe 3 O 4 (111) related by an 180° rotation about the [111] axes.…”
Section: (Iii) Fe 3 O 4 Island Growth Mechanismmentioning
confidence: 93%
“…Furthermore, these crystals were elongated along the crystallographic c-axis with (021) faces as endfaces, which terminate the crystal in this directon. Hence, from crystallographic reasoning, the (021) must be the fastest growing face when compared to the (110) and (100) face, and due to the low abundance of (100), this face must be faster growing than the (110) face (Kleber, 1990). One reason was reported by Weidler et al (1996), who attributed vicinal faces on the (100) to be responsible for a larger growth rate.…”
Section: Introductionmentioning
confidence: 99%
“…quartz, mica, etc.). Calcite and dolomite exhibit a pronounced anisotropy of the thermal expansion coefficient at different crystallographic directions (Kleber 1959) leading to stresses within the sample during heating ( Fig. 5a-d).…”
Section: Marble Weatheringmentioning
confidence: 99%