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Relevant bibliographies by topics / Mylonite

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Academic literature on the topic 'Mylonite'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 July 2024

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Journal articles on the topic "Mylonite"

1

Hanmer, Simon, Randy Parrish, Michael Williams, and Chris Kopf. "Striding-Athabasca mylonite zone: Complex Archean deep-crustal deformation in the East Athabasca mylonite triangle, northern Saskatchewan." Canadian Journal of Earth Sciences 31, no. 8 (1994): 1287–300. http://dx.doi.org/10.1139/e94-111.

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The geophysically defined Snowbird tectonic zone is manifested in northernmost Saskatchewan as a deep-crustal, multistage mylonitic structure, the East Athabasca mylonite triangle. The triangle, located at the northeastern apex of a stiff, crustal-scale "lozenge," is composed of mid-Archean annealed mylonites and late Archean ribbon mylonites, formed during two granulite facies events (850–1000 °C, 1.0 GPa). The flow pattern in the mylonites is geometrically and kinematically complex, and corresponds to that expected adjacent to the apex of a stiff elliptical volume subjected to subhorizontal

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Pearson, A., F. Heidelbach, and H. R. Wenk. "Texture Analysis of Quartz in a Granite Mylonite by EBSP-Orientation Imaging Microscopy." Textures and Microstructures 29, no. 3-4 (1997): 185–99. http://dx.doi.org/10.1155/tsm.29.185.

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The crystallographic preferred orientation (texture) of the quartz phase in a mylonitic leucogranite from the Santa Rosa mylonite zone was investigated using automated analysis of electron backscattering patterns (EBSP) in the scanning electron microscope (SEM). The separation of the quartz diffraction patterns from patterns of other constituents (feldspar, mica, etc.) in this polymineralic rock was achieved using an image quality parameter. The quartz phase displays a texture typical for high temperature mylonites (c-axis maximum in the intermediate strain direction). The misorientation distr

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V, Thirukumaran, Biswal T.K, Sundaralingam K, Sowmya V, Boopathi S, and Mythili R. "Strain Pattern Analysis of Mylonites From Sitampundi-Kanjamalai Shear Zone, Thiruchengode, South India." International Journal of Civil, Environmental and Agricultural Engineering 1, no. 1 (2019): 25–34. http://dx.doi.org/10.34256/ijceae1914.

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This study aims to investigate the petrography and strain pattern of mylonites from parts of N-S trending Sitampundi-Kanjamalai Shear Zone (SKSZ) around Thiruchengode. The petrographic study indicates the presence of recrystallized quartz, K-feldspar, plagioclase, biotite and some hornblende. The kinematic analysis of Mylonites was done with the help of shear sense indicators such as recrystallized type quartz (quartz ribbon) around the cluster of feldspar, S-C fabric shows dextral shear sense and some sinisterly shear sense in some parts of SASZ which can be considered as a product of partiti

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Owen, J. V. "Geochemical changes accompanying the mylonitization of diverse rock types from the Grenville Front zone, eastern Labrador." Canadian Journal of Earth Sciences 25, no. 9 (1988): 1472–84. http://dx.doi.org/10.1139/e88-140.

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The relationship between mineralogy and bulk composition was examined in mylonites developed in a variety of rock types from the Grenville Front zone of eastern Labrador. Mylonites developed from olivine-, pyroxene-, and (or) amphibole-bearing protoliths are the most altered, typically being enriched in K2O and volatiles and depleted in CaO compared with the protolith. Bulk-compositional modification was accompanied by the formation of almandine-rich garnet and (or) relatively ferruginous hornblende in medium-grade (epidote–amphibolite to lower amphibolite facies) mylonites derived from both m

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MALATESTA, C., L. FEDERICO, L. CRISPINI, and G. CAPPONI. "Fluid-controlled deformation in blueschist-facies conditions: plastic vs brittle behaviour in a brecciated mylonite (Voltri Massif, Western Alps, Italy)." Geological Magazine 155, no. 2 (2017): 335–55. http://dx.doi.org/10.1017/s0016756816001163.

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AbstractA blueschist-facies mylonite crops out between two high-pressure tectono-metamorphic oceanic units of the Ligurian Western Alps (NW Italy). This mylonitic metabasite is made up of alternating layers with different grain size and proportions of blueschist-facies minerals.The mylonitic foliation formed at metamorphic conditions of T = 220–310 °C and P = 6.5–10 kbar. The mylonite shows various superposed structures: (i) intrafoliar and similar folds; (ii) chocolate-tablet foliation boudinage; (iii) veins; (iv) breccia.The occurrence of comparable mineral assemblages along the foliation, i

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SARKARINEJAD, KHALIL, and SOMAYE DERIKVAND. "Structural and kinematic analyses of the basement window within the hinterland fold-and-thrust belt of the Zagros orogen, Iran." Geological Magazine 154, no. 5 (2016): 983–1000. http://dx.doi.org/10.1017/s0016756816000558.

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AbstractThe Zagros hinterland fold-and-thrust belt is located in the central portion of the Zagros Thrust System and consists of the exhumed basement windows associated with NW-striking and NE-dipping flexural duplex structures that contain in-sequence thrusting and related folds. Mylonitic nappes of the basement were exhumed along deep-seated sole thrusts of the Zagros Thrust System. Lattice preferred orientation (LPO) c-axes of quartz show asymmetric type-1 crossed girdles that demonstrate a non-coaxial deformation under plane strain conditions. Based on the opening angles of quartz c-axis f

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Hanmer, Simon. "Textural map units in quartzo-feldspathic mylonitic rocks." Canadian Journal of Earth Sciences 24, no. 10 (1987): 2065–73. http://dx.doi.org/10.1139/e87-195.

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The classical macrotextural subdivision of quartzo-feldspathic mylonitic rocks yields only three rock types: protomylonite, mylonite, and ultramylonite. This restriction impedes detailed mapping of the internal textural transitions common in wide, deep-seated, crustal-scale shear zones, where such transitions may occur over kilometres and involve several clearly mappable textural types. The introduction of two objectively defined field mapping terms, "homoclastic" and "heteroclastic," describing the macroscopic grain-size distribution within the porphyroclast population provides descriptive fl

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Owen, J. Victor. "Determination of the finite-strain ellipsoid from deformed porphyroblastic mineral aggregates and preferentially oriented feldspars in a mylonitized metamafic dyke." Canadian Journal of Earth Sciences 26, no. 11 (1989): 2333–40. http://dx.doi.org/10.1139/e89-199.

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Strain in a narrow mylonite zone has been estimated from deformed garnetiferous porphyroblastic aggregates and from preferentially oriented plagioclase porphyroclasts with high aspect ratios. In the undeformed metamafic dyke hosting the mylonite, the mineral aggregates have spheroidal to slightly oblate shapes, and plagioclase is nearly randomly oriented. In the mylonite, the mineral aggregates are prolate ellipsoids, and plagioclase in the aggregates and matrix is symmetrically oriented about the mylonitic planar fabric. Comparison with the radii of spheres of equal volume shows that the elli

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Festa, Vincenzo, Annamaria Fornelli, Francesca Micheletti, Richard Spiess, and Fabrizio Tursi. "Ductile Shearing and Focussed Rejuvenation: Records of High-P (eo-)Alpine Metamorphism in the Variscan Lower Crust (Serre Massif, Calabria—Southern Italy)." Geosciences 12, no. 5 (2022): 212. http://dx.doi.org/10.3390/geosciences12050212.

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In the present study, we unveil the real significance of mylonitic reworking of the polymetamorphic crystalline basement in the Serre Massif of Calabria (Southern Italy). We use a multidisciplinary approach to comprehend the structural, microstructural and petrologic changes that occurred along a, so far, not much considered shear zone affecting the Variscan lower crustal rocks. It was never before studied in detail, although some late Cretaceous ages were reported for these mylonites, suggesting that this shear zone is of prime importance. Our observations reveal now that the formation of the

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Farkašovský, Roman, Katarína Bónová, and Marián Košuth. "Microstructural, modal and geochemical changes as a result of granodiorite mylonitisation – a case study from the Rolovská shear zone (Čierna hora Mts, Western Carpathians, Slovakia)." Geologos 22, no. 3 (2016): 171–90. http://dx.doi.org/10.1515/logos-2016-0019.

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Abstract Strong tectonic remobilisation and shear zone development are typical features of the easternmost part of the Veporicum tectonic unit in the Western Carpathians. The granodiorite mylonites in the area of the Rolovská shear zone (Čierna hora Mts) underwent a complex polystage evolution during the Hercynian and Alpine orogenies. Deformation during the latter reached greenschist facies under metamorphic conditions. Mylonites are macroscopically foliated rocks with a stretching lineation and shear bands. Structurally different mylonite types, ranging from protomylonites to ulramylonites w

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Dissertations / Theses on the topic "Mylonite"

1

Bretan, P. G. "Deformation processes within mylonite zones associated with some fundamental faults." Thesis, Imperial College London, 1986. http://hdl.handle.net/10044/1/37954.

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Maurel, Olivier. "L'exhumation de la zone axiale des Pyrénées-Orientales une approche thermo-chronologique multi-méthodes du rôle des failles /." Montpellier : Institut des sciences de la terre, de l'environnement et de l'espace de Montpellier, 2003. http://catalogue.bnf.fr/ark:/12148/cb401527828.

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Point, Raymond. "La lame cratonique et les unités supracrustales de la chaîne calédonienne scandinave méridionale orientale : un exemple d'évolution polycyclique de mylonites précambriennes." Paris 7, 1990. http://www.theses.fr/1990PA077217.

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Dans les caledonides orientales scandinaves, l'etude des roches impliquees dans les deux nappes situees a la base de la grande nappe de seve, permet de definir deux grandes unites formees de mylonites heterogenes et polycycliques: 1) a la base, la lame cratonique, unite formee de lames de socle cristallin mylonitique a lithologie variee parmi lesquelles les orthogneiss de tannas representent une part importante en volume; 2) au-dessus, la nappe de sarv-humelfjell, unite de roches supracrustales formee de lames de tectonites ultramylonitiques et protomylonitiques a facies de pseudo-metaquartzit

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Papa, Simone. "The pseudotachylyte-mylonite association: an insight into the mechanics of deep earthquakes." Doctoral thesis, Università degli studi di Padova, 2019. http://hdl.handle.net/11577/3425421.

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The aim of this thesis is to investigate the association of fault rocks formed by seismic deformation with coeval ductile deformation. The only recognised geological record of these two concurrent deformation mechanisms is represented by the relationship between coeval pseudotachylytes (quenched melts produced during seismic slip) and mylonites (high-‐strain rocks deformed in high-temperature ductile flow). The scientific importance of this association of rocks lies in the fact that their existence in rocks exhumed from below the long-‐term brittle/ductile transition is a compelling evidence

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Stewart, Martyn. "Kinematic evolution of the Great Glen Fault Zone, Scotland." Thesis, Oxford Brookes University, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.364096.

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Parsons, Martha Mary. "Field and Microstructural Constraints on Deformation Conditions and Shear Zone Kinematics in the Burlington Mylonite Zone, Massachusetts:." Thesis, Boston College, 2017. http://hdl.handle.net/2345/bc-ir:107375.

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Thesis advisor: Seth C. Kruckenberg<br>The Burlington Mylonite Zone (BMZ) is a northeast-trending, greenschist- to amphibolite-facies shear zone located entirely within the Boston Avalon terrane in Eastern Massachusetts along the tectonic boundary with the Nashoba terrane (the trailing marginal terrane of Ganderia). The juxtaposition of these terranes, and the development of the BMZ, is hypothesized to represent the amalgamation of Avalon and Laurentia during the late Silurian-early Devonian Acadian orogeny, but the timing of its formation and its structural evolution remain largely unconstrai

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Loehn, Clayton William. "Monazite Geochronology of the Madison Mylonite Zone and Environs, Southwestern Montana: With Implications for Precambrian Thermotectonic Evolution of the Northern Wyoming Province." Thesis, Virginia Tech, 2009. http://hdl.handle.net/10919/31692.

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Neoarchean thermotectonism at in the northern Wyoming province is preserved in metamorphic zircon rims and monazite growth throughout the Snowy shear zone (SSZ) and the Madison mylonite zone (MMZ), South Madison Range, Montana. Comparison of U-Pb and U-Th-Pb ages yielded by monazite grains from both shear zones and zircon rims from SSZ, a new timing for major SE-directed thrusting and formation of the MMZ and SSZ has been identified at ~2550 Ma. The collinearity of these two shears indicates the formation of a much larger single shear zone that extends from the North Snowy block (NE), Bearto

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Mehl, Luc. "Plagioclase preferred orientation in the layered mylonites : evaluation of flow laws for the lower crust." Thesis, Online version of original thesis, 2008. http://hdl.handle.net/1912/2324.

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Jarrett, Corey. "Analysis of an Exposed Portion of the Badwater Turtleback Shear-zone, Death Valley, California, USA." Thesis, University of Oregon, 2018. http://hdl.handle.net/1794/23181.

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The exposed shear zone within the footwall of the Badwater turtleback presents an excellent opportunity to explore the brittle-ductile transition. Within this shear zone, a variety of lithologies preserve the last stages of crystal-plastic deformation concurrent with exhumation of the turtleback. The included field study captures a snapshot of each lithologic element during the last stages of ductile deformation. The exposed shear zone's journey through the brittle-ductile transition is analyzed using the deformation mechanisms of calcite and quartz. A history of strain partitioning is constr

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Tatarin, Triffon Joseph, and Triffon Joseph Tatarin. "Interrelationships of cataclasite, mylonite, and leucocratic bodies associated with the Catalina detachment fault, dual wash area, Saguaro National Park east, Rincon Mountains." Thesis, The University of Arizona, 2017. http://hdl.handle.net/10150/626821.

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The Dual Wash area is comprised of two west-northwest-trending washes (Deer Valley and Carillo), which provide excellent cross-section exposures of metamorphic core complex fault rock units. The structural components of metamorphic core complexes consist of upper plate rocks, a detachment fault, cataclasite and chlorite breccia, subdetachment fault, and mylonites. Within the Carillo Wash, the Catalina detachment fault dips ~13° NW, which is consistent with its overall dip in this part of the Rincon Mountains. However, exposed along the Deer Valley Wash, the Catalina detachment fault dips more

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Books on the topic "Mylonite"

1

Hanmer, Simon. Geology of the Striding-Athabasco mylonite zone, northern Saskatchewan and southeastern District of Mackenzie, Northwest Territories. Geological Survey of Canada, 1997.

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Passchier, C. W. (Cees W.), 1954-, Wiersma Dirk J. 1939-, and SpringerLink (Online service), eds. Atlas of Mylonites - and related microstructures. Springer-Verlag Berlin Heidelberg, 2010.

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Fliervoet, Timon F. Deformation mechanisms in fine grained quartzo-feldspathic mylonites: An electron microscopy study. Faculteit Aardwetenschappen, Universiteit Utrecht, 1995.

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Hanmer, Simmon. Geology of the Striding-Athabasca mylonite zone, northern Saskatchewan and southestern District of MacKenzie, Northwest Territories. Geological Survey of Canada, 1997.

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Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8.

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United States. National Aeronautics and Space Administration., ed. P-T conditions of deformation from fluid inclusions in mylonites. Dept. of Geology, University of Maryland, 1990.

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J, Parker A., and Geological Society of Australia. Specialist Group in Tectonics and Structural Geology., eds. Archaean - early proterozoic granitoids, metasediments and mylonites of Southern Eyre Peninsula, South Australia. Geological Society of Australia, 1988.

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Fault-related rocks: A photographic atlas. Princeton University Press, 1998.

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Todd, Victoria R., Arthur W. Snoke, and Jan Tullis. Fault-Related Rocks: A Photographic Atlas. Princeton University Press, 2014.

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Todd, Victoria R., Arthur W. Snoke, and Jan Tullis. Fault-Related Rocks: A Photographic Atlas. Princeton University Press, 2016.

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Book chapters on the topic "Mylonite"

1

Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. "Protomylonite, Mylonite and Ultramylonite." In Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8_7.

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Salda, L. H. Dalla, J. R. Franzese, and V. G. de Posadas. "The 1,800 Ma Mylonite-Anatectic Granitoid Association in Tandilia, Argentina." In Proceedings of the International Conferences on Basement Tectonics. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-017-0833-3_12.

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Knipe, R. J., and R. P. Wintsch. "Heterogeneous Deformation, Foliation Development, and Metamorphic Processes in a Polyphase Mylonite." In Metamorphic Reactions. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_7.

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Takahashi, Yutaka. "Geotectonic evolution of the Nihonkoku Mylonite Zone of north central Japan based on geology, geochemistry, and radiometric ages of the Nihonkoku Mylonites." In Ductile Shear Zones. John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781118844953.ch16.

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Li, Jianhong, and Liang Liang. "Features of mylonite and its relationship to uranium ore-formation in the Xiazhuang uranium ore field." In Mineral Deposit Research: Meeting the Global Challenge. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_74.

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Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. "“False” mylonites." In Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8_11.

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Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. "Low-Grade Mylonites." In Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8_4.

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Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. "Medium-Grade Mylonites." In Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8_5.

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Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. "High-Grade Mylonites." In Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8_6.

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Trouw, Rudolph A. J., Cees W. Passchier, and Dirk J. Wiersma. "Introduction." In Atlas of Mylonites- and related microstructures. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03608-8_1.

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Conference papers on the topic "Mylonite"

1

Mako, Calvin A. "SHEAR HEATING IN THE SANDHILL CORNER MYLONITE ZONE, MAINE." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310944.

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Cubrich, Bart T., Kevin R. Chamberlain, Ernest M. Duebendorfer, Michael L. Williams, and Jeffre W. Hamlin. "THE PALEOPROTEROZOIC MYLONITE OF KINGS CANYON, COLORADO: A CA. 1.6 GA GREENSCHIST FACIES MYLONITE FAR TO THE NORTH OF THE CONCURRENT ACTIVE TECTONIC MARGIN." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314204.

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Hurich, Charles A., Scott B. Smithson, David M. Fountain, and Michael C. Humphreys. "Seismic evidence of mylonite reflectivity in the Kettle dome metamorphic core complex." In 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892624.

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Jarrett, Corey B., Marli B. Miller, and Nancy A. Price. "MYLONITE MÉLANGE IN AN EXTENSIONAL SHEAR-ZONE: A DESCRIPTIVE HISTORY AND STRAIN ANALYSIS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298506.

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Yager, Kristie, Adam Ketchum, Sara E. Bier, Christian Shrader, and Sam Wilson. "KINEMATIC HISTORY OF THE CLARE MYLONITE IN THE NORTHWEST ADIRONDACKS: STRUCTURAL AND PETROGRAPHIC ANALYSIS." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310970.

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Cawood, Tarryn Kim, Scott Paterson, Barbara C. Ratschbacher, et al. "STRAIN (DE)-LOCALIZATION IN THE ~10KM WIDE CUESTA DE RANDOLFO MYLONITE ZONE, FAMATINIAN ARC." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302442.

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St. Denny, John Russell, and Erkan Toraman. "DECIPHERING DEFORMATION CONDITIONS ALONG THE CARTHAGE-COLTON MYLONITE ZONE, NW ADIRONDACKS, BASED ON FELDSPAR MICROSTRUCTURES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300057.

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Jarrett, Corey B., Marli B. Miller, and Nancy A. Price. "MYLONITE MELANGES IN AN EXTENSIONAL SHEAR-ZONE IN THE BADWATER TURTLEBACK OF DEATH VALLEY, CALIFORNIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283136.

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Baldassarre, Genna, Gary Solar, and Paul B. Tomascak. "FABRIC ANALYSIS IN MYLONITE IN THE NORUMBEGA SHEAR ZONE SYSTEM, FREEPORT-HARPSWELL AREA, SOUTHERN MAINE." In Northeastern Section-56th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021ne-361917.

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Tjapkes, Daniel J., Kaitlyn A. Suarez, Michael J. Jercinovic, and Michael L. Williams. "MONAZITE PETROCHRONOLOGY OF ADIRONDACK LOWLANDS MIGMATITES: IMPLICATIONS FOR THE SIGNIFICANCE OF THE CARTHAGE-COLTON MYLONITE ZONE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358741.

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Reports on the topic "Mylonite"

1

Hanmer, S. Geology, East Athabasca Mylonite Triangle, Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194845.

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Tribe, S. Kunghit Island mylonite of the southern Louscoone Inlet fault system, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/184088.

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Hanmer, S. Geology of the Striding-Athabasca mylonite zone, northern Saskatchewan and southeastern District of Mackenzie, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209170.

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Hanmer, S., M. Darrach, and C. Kopf. The east Athabasca Mylonite Zone: an Archean segment of the Snowbird Tectonic Zone in Nortern Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132845.

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Tella, S., J. C. Roddick, and W. Davis. Geochronological constraints on the multiple displacement history of the Amer Mylonite Zone, Churchill structural province, District of Keewatin, Northwest Territories, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209479.

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Hanmer, S. K. Granulite Facies Mylonites: a Brief Structural Reconnaissance North of Stony Rapids, northern Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122557.

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van Breemen, O., S. K. Hanmer, and R. R. Parrish. Archean and proterozoic mylonites along the southeastern margin of the Slave Structural Province, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/129070.

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Murphy, D. C. Direct Evidence For Dextral Strike - Slip Displacement From Mylonites in the southern Rocky Mountain Trench near Valemount, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131373.

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