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Subgrain boundary analyses in deformed orthopyroxene by TEM/STEM with EBSD-FIB sample preparation technique
Earth, Planets and Space volume 66, Article number: 84 (2014)
High-resolution structure analyses using electron beam techniques have been performed for the investigation of subgrain boundaries (SGBs) in deformed orthopyroxene (Opx) in mylonite from Hidaka Metamorphic Belt, Hokkaido, Japan, to understand ductile deformation mechanism of silicate minerals in shear zones. Scanning electron microscopy (SEM) and electron backscatter diffraction (EBSD) analysis of Opx porphyroclasts in the mylonitic rock indicated that the crystal orientation inside the Opx crystals gradually changes by rotation about the b-axis by SGBs and crystal folding. In order to observe the SGBs along the b-axis by transmission electron microscopy (TEM) or scanning TEM (STEM), the following sample preparation protocol was adopted. First, petrographic thin sections were slightly etched with hydrofluoric acid to identify SGBs in SEM. The Opx crystals whose b-axes were oriented close to the normal of the surface were identified by EBSD, and the areas containing SGBs were picked and thinned for (S) TEM analysis with a focused ion beam instrument with micro-sampling system. High-resolution TEM imaging of the SGBs in Opx revealed various boundary structures from a periodic array of dissociated (100)  edge dislocations to partially or completely incoherent crystals, depending on the misorientation angle. Atomic-resolution STEM imaging clearly confirmed the formation of clinopyroxene (Cpx) structure between the dissociated partial dislocations. Moreover, X-ray microanalysis in STEM revealed that the Cpx contains a considerable amount of calcium replacing iron. Such chemical inhomogeneity may limit glide motion of the dislocation and eventually the plastic deformation of the Opx porphyroclasts at a low temperature. Chemical profiles across the high-angle incoherent SGB also showed an enrichment of the latter in calcium at the boundary, suggesting that SGBs are an efficient diffusion pathway of calcium out of host Opx grain during cooling.
The interplay between deformation, grain size decrease, and mechanical weakening is considered as a major process to account for the localization of the ductile deformation of rocks in the shear zones (e.g., Boullier and Gueguen 1975; Rice 1976; Poirier 1980; Braun et al. 1999; Furusho and Kanagawa 1999; Precigout et al. 2007; Raimbourg et al. 2008). Though the operating microscopic mechanisms are not constant but depend on strain rate and temperature (Hirth and Tullis 1992; Poirier 1995), grain size reduction of constituting minerals involves the creation of a large area of grain boundaries (GBs) and is therefore ultimately controlled by GB structure and properties. One possible mechanism for the grain size reduction is the formation of subgrain boundaries (SGBs) and their evolution into general GBs with progressive misorientation angles between the two sides of the SGBs. From the observation of recrystallization textures, the transition from SGBs with regular arrays of dislocations within a single crystal to GBs incoherently separating two distinct crystals is often associated with a misorientation angle of 10° to 15° (e.g., Poirier and Nicolas 1975; White 1977; Guillopé and Poirier 1979; White and Mawer 1988), although for plagioclase, Fitz Gerald et al. (1983) proposed critical misorientation values below 5°. The general idea is that above a certain critical misorientation angle, dislocations should be too closely spaced for coherent crystal to be present between them (Read 1953). Such theoretical predictions can be evaluated by direct observations of the boundaries by transmission electron microscopy (TEM). Heinemann et al. (2005) followed, using high-resolution TEM (HRTEM), the evolution of synthetic SGBs in olivine with increasing misorientation. In natural orthopyroxene, although TEM works on dislocations and SGBs are plenty (e.g., Kohlstedt and Vander Sande 1973; McLaren and Etheridge 1976, 1980), there is no systematic investigation of the transition from SGBs to true GB which is the objective of the present work.
Generally, rocks or minerals are initially characterized by making a petrographic thin section of rocks polished to a thickness of 30 μm on a glass slide and observing them with polarized light microscopy and/or scanning electron microscopy (SEM). For detailed characterizations of the minerals using TEM, a sample preparation technique for the TEM observation at specific areas in the petrographic thin sections, for instance those containing SGBs in the present case, is necessary. In the past, it was almost impossible or required tremendous efforts to prepare such TEM specimens, especially in case that the density of SGBs is low. However, this problem has been solved by the invention and commercialization of the focused ion beam (FIB) instruments with the micro-sampling function (Kamino et al. 2005) and, for more specific TEM specimens, with the assist of electron backscatter diffraction (EBSD) analysis in a SEM. Recently, we reported and discussed the SGB structures in naturally deformed orthopyroxene ((Mg, Fe)SiO3, hereafter abbreviated as Opx) porphyroclasts in sheared metamorphic rock, by preparing TEM specimens from petrographic thin sections using FIB and EBSD (Raimbourg et al. 2011). Following this previous work, the present study describes the result of scanning TEM (STEM) microanalysis to show the local chemical segregation at the SGBs, as well as the description of the sample preparation procedure. Finally, we discuss the implication of such chemical heterogeneities for the process of exsolution and the mobility of dislocations, using observations of microstructures in deformed Opx porphyroclasts.
The geological setting of the specimen rock, a mylonite from Hidaka Main Zone within Hidaka Metamorphic Belt, Hokkaido, Japan, was described in detail in previous papers (Raimbourg et al. 2008, 2011). In the mylonite, the predominant Opx porphyroclasts are up to a few millimeters in size and embedded in a foliated matrix of small (approximately 50 μm) plagioclase grains (Figure 1). Petrographic thin sections were prepared in the plane parallel to the shear direction and perpendicular to the foliation. The surfaces of the sections were polished with diamond paste then colloidal silica, and then chemical etching of the surface was carried out with hydrofluoric (HF) acid following the method described in Wegner and Christie (1985), the latter to enhance SEM imaging of SGBs and Ca-rich clinopyroxene (Cpx) lamellae exsolved in Opx along the (100) plane.
Crystal bending and/or distribution of SGBs inside Opx grains was first characterized with crystal orientation maps obtained by using a HKL Channel 5 EBSD system (Oxford Instruments, Abingdon, UK) attached to a JSM-7000 F field emission (FE)-SEM (JEOL Ltd., Tokyo, Japan). High-resolution imaging of the etched surface and determination of the crystal orientation for the FIB sample preparation were performed using a S-4500 FE-SEM (Hitachi High-technologies, Tokyo, Japan) equipped with a Noran PhaseID EBSD system (Thermo Fisher Scientific Inc., Waltham, MA, USA). The areas containing SGBs were transferred and etched to electron transparency using a Hitachi FB-2100 FIB instrument with the micro-sampling system. As described below, it is desirable that the specimens can be oriented in (S) TEM so that the incident electron beam is parallel to the b-axis, to which the SGBs are expected to be parallel. This was satisfied by using EBSD data. First, the EBSD pattern was acquired from the surface area of interest (Figure 2a), and the inclination of the b-axis from the surface normal was determined (Figure 2b, c). A ‘plan-view specimen’ was made by attaching the crystal fragment cut by FIB orthogonally to a crescent-shaped copper mesh for TEM, with the micro-sampling system. In this case, if the inclination of the b-axis was less than approximately 15° which is the maximum tilt angle in (S) TEM, no care was necessary, but if it was over 15°, the fragment was attached obliquely to counter the inclination (Figure 2d).
TEM observation of the SGBs was performed using JEOL JEM-2010 UHR with the spherical aberration coefficient (Cs) of the objective lens of 0.5 mm, operated at 200 kV. Low-magnification TEM images and selected-area electron diffraction patterns were recorded using an ESW-500 W side-mount charge-coupled device (CCD) camera (Gatan Inc., Pleasanton, CA, USA). HRTEM images were recorded using a Gatan MSC 622 bottom-mount CCD camera. Elemental line profiles around dislocations and SGBs were obtained in a JEOL JEM-2800 F STEM operated at 200 kV with a Noran NSS energy dispersive X-ray spectroscopy (EDS) analysis system (Thermo Fisher Scientific Inc., Waltham, MA, USA). To achieve the atomic-scale STEM imaging of high-angle annular dark-field (HAADF), we used a JEOL ARM-200 F STEM with a cold-type field emission gun operated at 200 kV and spherical aberration corrector (Cs-corrector) for the probe-forming lens. The noisy contrast in the STEM-HAADF images was removed using a Wiener filter (Marks 1996; Kilaas 1998) developed by K. Ishizuka (HREM-Filters Pro, HREM Research Inc., Higashimatsuyama, Japan) and implemented with Gatan DigitalMicrograph on the original images (Kogure and Okunishi 2010).
Results and discussion
Electron microscopy observations
Figure 3 is an example of EBSD analysis of deformed Opx, showing the progressive rotation of the crystal about the b-axis. As reported in Raimbourg et al. (2011), this rotation is mainly attained by (100)  dislocations in Opx. In some samples, dislocations are distributed relatively homogeneously, while in others, they organize in two ways: almost periodically arranged roughly along the (001) plane to form SGBs with misorientation up to a few degrees, and accumulated on the (100) boundaries between the exsolved Ca-rich Cpx lamellae and Opx matrix (Raimbourg et al. 2011). Chemical etching with HF on the polished surface of Opx revealed the trenched Ca-rich Cpx lamellae and arrays of the etched dislocations (Figure 4a). Moreover, occasionally the lamellae are sharply bent, as seen in Figure 4b, indicating the location of higher-angle SGBs which may be semi- or incoherent.
HRTEM images of several SGBs along the b-axis with various misorientation angles are presented in Figure 5. The details of these images have been also described in Raimbourg et al. (2011). If the misorientation angle is small, the boundary consists of the periodic array of the (100)  dislocation (Figure 5a), which must correspond to the lined etch pits in Figure 3a. The HRTEM image of the single dislocation (Figure 5b) generally shows a pair of dark areas and h 00 lattice fringes between them, with the periodicity of a half (approximately 4.6 Å) of that in the surrounding Opx (approximately 9.2 Å). This feature is interpreted as the dissociation of the (100)  dislocation into two partial dislocations and formation of clinopyroxene (Cpx) between them, as proposed by several previous works (e.g., Coe and Kirby 1975; McLaren and Etheridge 1976). The Cs-corrected STEM-HAADF image of the dislocation confirmed the formation of Cpx (Figure 6). In the image, the octahedral sites show the brightest spots as Z-contrast and the unit cells of Cpx and Opx can be drawn according to their locations. As is well known, the unit cell of Opx can be expressed as the two Cpx cells with twin relation about the (100) plane (Ito 1950). The STEM-HAADF image in Figure 6 clearly shows the relation between the Opx and Cpx structure around the dislocation. The image also contains the core regions of the partial dislocations as surrounded by the white circles, where the bright spots for the octahedral sites are horizontally obscured, indicating unaligned octahedral cations along the b-axis.
On the other hand, the SGB feature with a misorientation of 7° is considerably different. The HRTEM image of the SGB (Figure 5c) shows regions indicated with white arrows, where the lattice fringes are obscure, arranged almost periodically along the boundary. On the contrary, the lattice fringes between these obscure regions are clear and connected across the boundary, suggesting that the Opx structure is still continuous. The averaged spacing between the adjacent regions in Figure 5c is roughly 50 Å. If we apply Frank's formula (Frank 1951), the Burgers vector around the region is 6 Å, which is close to the c-length (5.2 Å). Hence, the obscure regions are probably considered as the dislocation core of the (100)  dislocation without dissociation. In other words, with such a misorientation angle, SGB is ‘semi-coherent’ with the (100)  dislocation cores along the boundary. Finally, the HRTEM image of SGB with a misorientation of 21° (Figure 5d) indicates the terminated lattice fringes at the boundary, and amorphous-like contrast of less than 1 nm thick between the fringes of Opx on both sides of the boundary. Moreover, the electron diffraction patterns (not shown) indicate that the b-axes of the Opx crystals on both sides are not exactly common but deviate from each other by a few tens of degrees, which results in the slightly different HRTEM contrasts between both sides of the boundary in Figure 5d. Accordingly, this SGB is considered incoherent with no structural continuity of Opx across the boundary.
The compositions in the immediate vicinity of the dislocation and SGBs were also analyzed by STEM-EDS (Figures 7 and 8). The elemental profiles along the a-axis and across the dislocation (Figure 7a) showed the accumulation of Ca and deficiency of Fe at the Cpx at the dislocation, consistent with the substitution of Ca for Fe in the Cpx structure (Figure 7b). The wollastonite component reaches roughly 15 to 20 at.% at the maximum of the Ca profile, suggesting that Cpx at the dislocation should be called augite compositionally. The chemical composition at the dislocation core did not show a distinct difference from the surroundings. The chemical composition at the high-angle SGB in Figure 5d was analyzed in a similar way (Figure 8). Ca was definitely detected at the boundary, while Si is deficient compared to the surrounding Opx. Combined with the HRTEM image (Figure 5d), calcium-rich and silicon-deficient material with thickness of a few atomic layers may exist at the boundary.
Dislocation dissociation and associated chemical heterogeneity
Many TEM works (e.g., Green and Radcliffe 1972; Kohlstedt and Vander Sande 1973; Coe and Kirby 1975; McLaren and Etheridge 1976; Van Duysen et al. 1985; Nazé et al. 1987; Steuten and Van Roermund 1989) indicated that dislocations (100)  of Opx are dissociated. Furthermore, the presence of Cpx between the partial dislocations was also proposed (Coe and Kirby 1975; McLaren and Etheridge 1976; Nazé et al. 1987). In the present study, STEM-HAADF imaging (Figure 6) has clearly confirmed the presence of a Cpx structure. In addition, our EDS analysis has shown considerable chemical difference between the Cpx structure and surrounding Opx with enrichment in Ca and depletion in Fe for Cpx. This chemical heterogeneity may have a considerable influence on the plasticity of Opx porphyroclasts because the glide of the dislocation requires the chemical heterogeneity to be moved along. In other words, chemical diffusion of calcium and iron necessarily occurs as dislocation is gliding and therefore causes a potential limitation to this motion. This does not seem to be the case here, as the Opx porphyroclasts are strongly deformed (Raimbourg et al. 2008) showing that chemical diffusion is not a process which limits plastic deformation at granulite-facies conditions, i.e., at high temperature. However, the deactivation of dislocation slip with decreasing temperature may be the consequence of sluggish chemical diffusion. Besides, it is suspected that such a dislocation with the structure and chemistry close to Ca-rich Cpx can be nucleation sites of the Ca-rich exsolution lamellae, as suggested by White and Mawer (1988). Actually, the dense Ca-rich exsolution lamellae are found only in the strongly elongated porphyroclasts within the shear zones and absent in the surrounding undeformed porphyroclasts, indicating the interplay between deformation (by dislocation creep) and exsolution, which is also common in feldspar deformed at granulite grade conditions (White and Mawer 1988).
Flux of calcium in the SGBs and relevant recrystallization
Another accumulation of calcium has been also found in the high-angle incoherent SGB in Figure 5d (Figure 8). This result is the direct evidence for the hypothesis that such incoherent SGBs are the major diffusion pathways of calcium during deformation. Several macroscopic structures in the deformed Opx can be accounted for by this hypothesis (Figure 9). In Figure 9a, small Ca-rich Cpx grains other than the lamellae are developed along the high-angle SGB. Furthermore, the Cpx lamellae are absent around another high-angle SGB in Figure 9b, indicating the depletion of calcium in Opx around the SGB. On this example, a simple mass balance calculation shows that SGBs not only segregate Ca but also enhance Ca diffusion along the boundary. On the surface of the host Opx far from the SGB in Figure 9b, for instance, at the bottom-right of the figure, the density of Ca-rich exsolution lamellae is approximately 0.26 lines per micrometer if measured across the lamellae. The thickness of these lamellae is very variable, as can be seen in the various TEM pictures in Raimbourg et al. (2011), and we consider 10 nm as a minimum value. Consequently, the volume ratio of exsolution to Opx is more than 2.6 × 10−3. The area depleted of exsolution, on both sides of the SGB, has a minimum thickness of 10 μm in Figure 9b. Hence, if Ca in the area depleted of exsolution around the SGB is only accumulated and stored at the boundary, it should form Ca-rich exsolution of more than 26 nm thick at the boundary. The actual thickness of the Ca-rich region at SGBs is far smaller than this as shown in Figure 8, indicating that Ca has flown out of the host Opx along the SGB.
In parallel, the zones around the high-angle SGB free from exsolution lamellae are preferential sites for recrystallization of small grains (Figure 9c). The process of recrystallization definitely involves the formation of SGBs and their evolution into true GBs with increasing misorientation (Raimbourg et al. 2011). As described above, SGBs in Opx can be started by the regular arrangement of the (100)  dislocations. However, another slip system should be activated for the recrystallization shown in Figure 9c. Exsolution lamellae of Cpx densely distributed within Opx probably act as barriers to the glide of any dislocation except in the (100) plane (i.e., parallel to the lamellae), hence preventing recrystallization. Enhanced recrystallization at the SGB in Figure 9c may therefore be interpreted as the activation of multiple slip systems where exsolution lamellae are absent.
State-of-the-art electron beam analyses with atomic-scale resolution have imaged unit cell structure of the (100)  dislocation to form SGBs, as well as high-angle incoherent SGBs in deformed Opx porphyroclasts in mylonite. The Cpx structure is definitely formed between the dissociated partial dislocations and contains considerable amounts of calcium replacing iron. Although more investigation is needed, such a Cpx structure may link the deformation and exsolution in the Opx as the nucleus of the exsolution. High-angle, incoherent SGBs probably contain an amorphous-like material of a few atomic layers enriched in calcium. Probably, this is the evidence for the idea that the incoherent SGBs act as diffusion pathways of calcium and maybe other elements. Accordingly, development of SGBs by deformation also accelerates chemical re-equilibrium of minerals during metamorphic processes. These nanostructures of SGBs will be a key to understand deformation, grain size reduction, and mechanical weakening of rocks in ductile shear zones.
spherical aberration coefficient
electron backscatter diffraction
energy dispersive X-ray spectroscopy
focused ion beam
high-angle annular dark-field
high-resolution transmission electron microscopy
scanning electron microscopy
scanning transmission electron microscopy
transmission electron microscopy.
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This work was supported by Grants-in-Aid for Scientific Research from MEXT of Japan (21107005). A part of this work was conducted in Research Hub for Advanced Nano Characterization, The University of Tokyo and supported by ‘Nanotechnology Platform’ (Project No. 12024046), both sponsored by MEXT, Japan.
The authors declare that they have no competing interests.
TK conducted this study; carried out the SEM, EBSD, and TEM analyses; interpreted the data; and prepared the manuscript. HR collected rock samples, prepared petrographic thin sections, performed SEM-EBSD analyses, and joined the preparation of the manuscript. AK carried out the HAADF imaging and X-ray microanalysis in STEM, and gave the interpretation of the images and analysis. EF prepared TEM/STEM specimens using FIB and suggested the technique used to prepare these specimens. Finally, YI gave several valuable comments for the interpretation of TEM/STEM results from his deep background of grain boundaries. All authors read and approved the final manuscript.
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Kogure, T., Raimbourg, H., Kumamoto, A. et al. Subgrain boundary analyses in deformed orthopyroxene by TEM/STEM with EBSD-FIB sample preparation technique. Earth Planet Sp 66, 84 (2014). https://doi.org/10.1186/1880-5981-66-84
- Subgrain boundary