Vertical and fold-axis parallel extension within a slate belt in a transpressive setting, northern Appalachians

1995 ◽  
Vol 17 (3) ◽  
pp. 329-343 ◽  
Author(s):  
Donna Kirkwood ◽  
Michel Malo ◽  
Pierre St-Julien ◽  
Pierre Therrien
Geotectonics ◽  
2020 ◽  
Vol 54 (2) ◽  
pp. 256-265
Author(s):  
L. A. Peñafiel ◽  
P. S. B. Reyes ◽  
F. J. Alcalá ◽  
M. R. Ramírez ◽  
A. Cabero

Author(s):  
Ann N. Campbell ◽  
Martin J. Carr ◽  
John B. VanderSandet

The microstructure of 25-500 μm-thick, pure-Ni films formed by chemical vapor deposition on copper substrates at 180°C is complex, consisting of areas of a fine, heavily faulted structure and of relatively larger grains, 1-3 μm in diameter. The large grains have a <110> axis parallel to the growth direction and are frequently twinned. Pentagonal arrangements of the large grains, Figure 1, were commonly observed by transmission electron microscopy. Similar microstructural features have been reported to form during vapor deposition of other FCC metals, and have been shown to possess a true five-fold axis developed by twinning and distorting small crystals.


2004 ◽  
Vol 811 ◽  
Author(s):  
A. R. Kortan ◽  
M. Hong ◽  
J. Kwo ◽  
P. Chang ◽  
C. P. Chen ◽  
...  

ABSTRACTWe have characterized the structure of the epitaxial Sc2O3 films grown on a α-Al2O3 (111) substrate using molecular beam epitaxy (MBE) techniques. The Sc2O3 films grow in the bulk bixbyite phase with a very uniform thickness, and a high structural perfection. They grow with their cubic (111) axis parallel to the rhombohedral (111) axis of the sapphire substrate. The in-plane orientation of the films, however, is rotated by ±30 degrees with respect to the substrate rhombohedral axes. This is explained by the presence of two equivalent orientations of the 3-fold axis of the film on the quasi 6-fold surface of the substrate.


2000 ◽  
Vol 15 (7) ◽  
pp. 1570-1575
Author(s):  
Koichiro Fukuda

Crystals of merwinite were prepared at 1550 °C from chemical reagents, and their intracrystalline microstructures were examined by the combined use of x-ray diffraction and optical microscopy. The crystals were composed of pseudomerohedral twins. The adjacent twin domains were related by the pseudosymmetry two-fold axis parallel to ⟨011⟩with the composition surface {811} The overall twin structure was constructed by introducing the pseudo-symmetry three-fold axis normal to (100), which must originally be a symmetry element of the former high-symmetry phase. The transition from the primitive trigonal (point group 3m) to the primitive monoclinic (space group P21/a) was accompanied by the combination of reducing the order of the point group and the change in the size of the unit cell. The order of the point group was reduced from 12 to 4, resulting in three twin domains with six different interfaces. This accounted for the experimentally observed microstructure consisting of repeated lamella twins in several orientations. Because the unit lattice translation would be lost during the transition, the formation of antiphase domains was expected. The lost translation vectors were 1/2[011], 1/2[100], and 1/2[111] resulting in four antiphase domains. As a result, the total number of domains possible in the transition was 3 × 4 = 12.


2021 ◽  
Author(s):  
Aurélie Labeur ◽  
Nicolas E. Beaudoin ◽  
Olivier Lacombe ◽  
Guilhem Hoareau ◽  
Lorenzo Petraccini ◽  
...  

&lt;p&gt;The timing and duration of fold-related deformation - including layer-parallel shortening (LPS) &amp;#8211; related to fold growth, are difficult to estimate because of a lack of data in most natural cases. We propose an original combination of direct and indirect dating methods to reconstruct the burial-deformation history of the Mesozoic carbonates that crop out in the Cingoli Anticline in the Umbria-Marche Apennine Ridge.&lt;/p&gt;&lt;p&gt;The Cingoli anticline displays an arcuate shape in map view, trending N140 in its northern part and N160 in its southern part). We first study the fracture-stylolite network to characterize the successive stages of deformation. Several sets of mesostructures were discriminated according to their orientation and relative chronology:&lt;/p&gt;&lt;ul&gt;&lt;li&gt;(i) N-S trending vertical joints (after unfolding), likely related to foreland flexure/forebulge development;&lt;/li&gt; &lt;li&gt;(ii) N045 trending vertical, bedding and fold-axis perpendicular joints/veins, associated with early folding stylolites with N045-oriented peaks and reverse faulting associated with a N045 &amp;#963;&lt;sub&gt;1&lt;/sub&gt; (after unfolding), reflecting LPS;&lt;/li&gt; &lt;li&gt;(iii) bedding-perpendicular and fold axis -parallel joints/veins, e., trending N140 in the northern part and N160 in the southern part of the anticline, reflecting outer-arc extension associated to strata curvature at fold hinge, the variation about 20&amp;#176; in orientation between the northern and southern parts of the fold being consistent with the arcuate shape of the anticline;&lt;/li&gt; &lt;li&gt;(iv) tectonic stylolites with horizontal peaks striking N045, along with conjugate vertical strike-slip faults, associated with a horizontal N045 contraction affecting the strata after the fold was locked, corresponding to the late stage of fold tightening (LSFT).&lt;/li&gt; &lt;/ul&gt;&lt;p&gt;These results suggest that the Cingoli anticline developed under a continuous N045 contraction and that its arcuate shape is likely primary and was achieved in relation to the reactivation of an N-S normal fault inherited from the Tethyan rifting, without any vertical-axis rotation of the fold axis.&lt;/p&gt;&lt;p&gt;We further reconstructed burial curves considering sedimentary formation thicknesses, corrected from physical and chemical compaction. We also quantified the vertical stress experienced by sedimentary stylolites from a roughness inversion technique, allowing derivation of the maximum depth experienced by the strata prior to contraction (using bedding-parallel sedimentary stylolites) and during exhumation (using horizontal sedimentary stylolites related to a post-folding compaction). Oxygen and carbon isotope ratios measured in tectonic vein cements point towards a locally-sourced fluid system with limited vertical migration at the scale of the carbonate core, enabling the use of the absolute temperatures obtained from CO&lt;sub&gt;2&lt;/sub&gt; clumped isotope (D&lt;sub&gt;47&lt;/sub&gt;) to reconstruct the depth during layer-parallel shortening and folding. The comparison of reconstructed depth at which each deformation phase occurred with the burial curve provides absolute timing for the development and exhumation of the Cingoli Anticline. Together with U-Pb ages of calcite vein cements and fault coatings from the nearby San Vicino Anticline, located west of the Cingoli Anticline, our data suggest that contraction started by ~8 Ma (LPS) and ended by ~3 Ma (LSFT), and that the growth of the Cingoli anticline lasted from ~5.5 to 4 Ma. &amp;#160;&lt;/p&gt;


Author(s):  
Rob. W. Glaisher ◽  
A.E.C. Spargo

Images of <11> oriented crystals with diamond structure (i.e. C,Si,Ge) are dominated by white spot contrast which, depending on thickness and defocus, can correspond to either atom-pair columns or tunnel sites. Olsen and Spence have demonstrated a method for identifying the correspondence which involves the assumed structure of a stacking fault and the preservation of point-group symmetries by correctly aligned and stigmated images. For an intrinsic stacking fault, a two-fold axis lies on a row of atoms (not tunnels) and the contrast (black/white) of the atoms is that of the {111} fringe containing the two-fold axis. The breakdown of Friedel's law renders this technique unsuitable for the related, but non-centrosymmetric binary compound sphalerite materials (e.g. GaAs, InP, CdTe). Under dynamical scattering conditions, Bijvoet related reflections (e.g. (111)/(111)) rapidly acquire relative phase differences deviating markedly from thin-crystal (kinematic) values, which alter the apparent location of the symmetry elements needed to identify the defect.


Author(s):  
Hamish L. Fraser

The topic of strain and lattice parameter measurements using CBED is discussed by reference to several examples. In this paper, only one of these examples is referenced because of the limitation of length. In this technique, scattering in the higher order Laue zones is used to determine local lattice parameters. Work (e.g. 1) has concentrated on a model strained-layer superlattice, namely Si/Gex-Si1-x. In bulk samples, the strain is expected to be tetragonal in nature with the unique axis parallel to [100], the growth direction. When CBED patterns are recorded from the alloy epi-layers, the symmetries exhibited by the patterns are not tetragonal, but are in fact distorted from this to lower symmetries. The spatial variation of the distortion close to a strained-layer interface has been assessed. This is most readily noted by consideration of Fig. 1(a-c), which show enlargements of CBED patterns for various locations and compositions of Ge. Thus, Fig. 1(a) was obtained with the electron beam positioned in the center of a 5Ge epilayer and the distortion is consistent with an orthorhombic distortion. When the beam is situated at about 150 nm from the interface, the same part of the CBED pattern is shown in Fig. 1(b); clearly, the symmetry exhibited by the mirror planes in Fig. 1 is broken. Finally, when the electron beam is positioned in the center of a 10Ge epilayer, the CBED pattern yields the result shown in Fig. 1(c). In this case, the break in the mirror symmetry is independent of distance form the heterointerface, as might be expected from the increase in the mismatch between 5 and 10%Ge, i.e. 0.2 to 0.4%, respectively. From computer simulation, Fig.2, the apparent monocline distortion corresponding to the 5Ge epilayer is quantified as a100 = 0.5443 nm, a010 = 0.5429 nm and a001 = 0.5440 nm (all ± 0.0001 nm), and α = β = 90°, γ = 89.96 ± 0.02°. These local symmetry changes are most likely due to surface relaxation phenomena.


Sign in / Sign up

Export Citation Format

Share Document