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The importance of subduction-related margin-parallel shear zones along transpressional convergent plate margins

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Basement Tectonics 8

Part of the book series: Proceedings of the International Conferences on Basement Tectonics ((ICBT,volume 2))

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Abstract

Structural and tectonic models of ancient convergent margins commonly assume simple orthogonal convergence and collision; hence, they are easily represented in cross-sectional models. These simplified models, useful for predicting first-order relationships between geologic elements, often do not consider a margin-parallel component of relative motion. A growing body of evidence suggests that during oblique convergence, subduction-related margin-parallel strike-slip shear zones (MPSZs) play an important role in the evolution of many convergent margins.

MPSZs are probably most important along margins of oblique convergence characterized by shallow subduction, an overriding plate comprised of continental crust, and an absence of salients that may inhibit margin-parallel motion. Recognition of evidence for oblique convergence and MPSZs, as preserved in the rock record, is the next step in refining convergent plate margin tectonic models. This is particularly important with respect to our understanding of continental margin kinematics in the past, for which there exist few data to constrain plate motions. The formation and geometry of elements within MPSZs depends on structural level and location (i.e., distance from the trench) within the overriding plate. Detailed structural and kinematic analysis across presumed ancient margins may reveal subduction-related MPSZs. Knowledge of MPSZs active along the plate décollement as well as within the overriding plate may allow limits to be placed on the direction, time, and magnitude of the translation of upper-plate slivers. Documentation of MPSZs and incorporation of relevant motion and age data into multi-dimensional models, those which consider more than a classical cross-orogen section, may greatly advance models of Mesozoic (and older) convergent plate-margin evolution.

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References

  • Avé Lallemant, H. G., and J. S. Oldow, 1988, Early Mesozoic southward migration of Cordilleran transpres-sional terranes: Tectonics, v. 7, p. 1057–1075.

    Article  Google Scholar 

  • Brace, W. F., and D. L. Kohlstedt, 1980, Limits on lithospheric stress imposed by laboratory experiments: Journal of Geophysical Research, v. 85, p. 6248–6252.

    Article  Google Scholar 

  • Beck, M. E., Jr., 1980, Paleomagnetic record of plate margin tectonic processes along the western edge of North America: Journal of Geophysical Research, v. 84, p. 7115–7131.

    Article  Google Scholar 

  • ___, 1983 On mechanism of tectonic transport in zones of oblique subduction: Tectonophysics, v. 93. p. 1–11.

    Article  Google Scholar 

  • ___, 1986, Model for late Mesozoic-early Tertiary tectonics of coastal California and western Mexico, and speculation on the origin of the San Andreas fault: Tectonics, v. 5, p. 49–64.

    Article  Google Scholar 

  • Berthé, D., P. Choukroune, and D. Gapais, 1979a, Orientations preferentielles du quartz et orthogneissi-fication progressive en regime cisaillant: I’example du cisaillement sud-Amoricain: Bulletin de Mineralogie, v. 102, p. 265–272.

    Google Scholar 

  • ___, P. Choukroune, and P. Jegouzo, 1979b, Ortho-gneiss, mylonite and noncoaxial deformation of granite: The example of the South American shear zone: Jounal of Structural Geology, v. 1, p. 31–42.

    Article  Google Scholar 

  • Bidwell, M. E., and R. R. Bauer, 1987, Ductile shearingand coeval folding during dextral transpression, central Vermillion district, NE Minesota [abstract]: Geological Society of America Abstracts with Programs v. 19, p. 588.

    Google Scholar 

  • Bohlen, S. R., and J. J. Liotta, 1986, A barometer for garnet amphibolites and garnet granulites: Journal of Petrology, v. 27, p. 1025–1034.

    Article  Google Scholar 

  • Bostick, N. H., 1974, Phytoclasts as indicators of thermal metamorphism, Franciscan assemblage and Great Valley sequence (upper Mesozoic), California; pp. 1–17 in R. R. Dutcher, P. A. Hacquebard, J. M. Schops, and J. A. Simon (eds.), Carbonaceous Materials as Indicators of Metamorphism: Geological Society of America, Special Paper 153, 108 p.

    Google Scholar 

  • Bouchez, J. L., G. Nantes, S. Lister, and A. Nicolas, 1983, Fabric asymmetry and shear sense in movement zones: Geologische Rundschau, v. 72, p. 401–419.

    Article  Google Scholar 

  • Chester, F. M., and J. M. Logan, 1987, Composite planar fabric gouge from the Punchbowl Fault California: Journal of Structural Geology, v. 9, p. 621–634.

    Article  Google Scholar 

  • Choukroune, P., 1971, Contribution à l’étude desmech-anisms de la déformation avec schistositié grace aux cristallisation syncinématiques dans les “zones abritées” (“pressure shadows”): Bulletin de la Sociéte Géologique de France, v. 7, p. 257–271.

    Google Scholar 

  • Cobbold, P. R., and D. Gapais., 1987, Shear criteria inrocks: an introductory review: Journal of Structural Geology, v. 9, p. 521–524.

    Article  Google Scholar 

  • Coney, P.J., D.L. Jones, and J. W. H. Monger, 1980, Cordilleran suspect terranes: Nature, v. 188, p. 329–333.

    Article  Google Scholar 

  • ___, and D. L. Jones, 1985, Accretion tectonicsand crustal structure in Alaska, Tectonophysics, v. 119, p. 265–283.

    Article  Google Scholar 

  • Cowan, D. S., 1982, Geological evidence for post-40 m.y. ?.P. large-scale northwestward displacement of part of southeastern Alaska: Geology, v. 10, p. 309–313.

    Article  Google Scholar 

  • Cross, T. A., and R. H. Pilger, Jr., 1982, Controls on subduction geometry, locations of magmatic arc and back-arc regions: Geological Society of America Bulletin, v. 93, p. 545–562.

    Article  Google Scholar 

  • Dewey, J. F., 1980, Episodicity, sequency and style at convergent plate boundaries; pp. 553–573 in D. W. Strange-way (ed.), The Continental Crust and Its Mineral Deposits: Geological Association of Canada, Special Paper 20, 804 p.

    Google Scholar 

  • Dickinson, W. R., 1972, Evidence for plate-tectonic regimes in the rock record: American Journal of Science, v. 272, p. 551–576.

    Article  Google Scholar 

  • Dunbar, J. A., and D. S. Sawyer, 1988, Continental rifting at pre-existing lithosphere weaknesses: Nature, v. 333 p. 450–452.

    Article  Google Scholar 

  • Durney, D. W., and J. G. Ramsey, 1973, Incremental strains measured by syntectonic crystal growth; pp. 67–96 in K. A. DeJong and R. Scholten (eds.), Gravity and Tectonics:Wiley, New York, New York, USA, 502 p.

    Google Scholar 

  • Etchecopar, A., and J. Malaveille, 1987, Computer models of pressure shadows: A method for strain measurement and shear sense determination: Journal of Structural Geology, v. 9, p. 667–678.

    Article  Google Scholar 

  • Ferry, J. M. (ed.), 1982, Characterization of Metamor-phism through Mineral Equilibria: Mineralogical Society of America, Reviews in Mineralogy 10, 397 p.

    Google Scholar 

  • Fitch, T. J., 1972, Plate convergence, transcurrent faults and internal deformation adjacent to Southeast Asia and the western Pacific: Journal of Geophysical Research, v. 77, p. 4432–4461.

    Article  Google Scholar 

  • Gabrielse, H., 1985, Major dextral transcurrent displacements along the northern Rocky Mountain Trench and related lineaments in north-central British Columbia: Geological Society of America Bulletin, v. 96, p. 1–14.

    Article  Google Scholar 

  • Gammond, J. F., 1987, Bridge structures as sense of movement on fault surfaces in brittle rocks: Journal of Structural Geology, v. 9, p. 609–620.

    Article  Google Scholar 

  • Hansen, V. L., 1987a, Structural, Metamorphic, and Geochronologic Evolution of the Teslin Suture Zone, Yukon: Evidence for Mesozoic Oblique Convergence Outboard of the Northern Canadian Cordillera:PhD dissertation, University of California, Los Angeles, California, USA, 221 p.

    Google Scholar 

  • ___, 1987b, Tectonic correlation of the Yukon-Tanana (YT) and Slide Mountain (SM) terranes [abstract]: Geological Society of America Abstracts with Programs, v. 19, p. 386.

    Google Scholar 

  • ___, 1988, A model for terrane accretion: Yukon-Tanana and Slide Mountain terranes, northwestrn North America: Tectonics, v. 7, p. 1167–1177.

    Article  Google Scholar 

  • ___, 1989, Structural and kinematic evolution of the Teslin suture zone, Yukon: Record of an ancient transpres-sional margin: Jounal of Structural Geology, v. 11, p. 717–733.

    Article  Google Scholar 

  • Hodges, K. V., and P. D. Crowley, 1985, Error estimation and empirical geothermobarometry for pelitic systems: American Mineralogist, v. 70, p. 702–709.

    Google Scholar 

  • Huddleston, P. J., D. Schulzela, and D. L. Southwick, 1988, Transpression in an Archean greenstone belt, northern Minnesota: Canadian Journal of Earth Sciences, v. 7, p. 1060–1068.

    Google Scholar 

  • Irving, E., 1979, Paleopoles and paleolatitudes of North America and speculation about displaced terranes: Canadian Journal of Earth Sciences, v. 16, p. 669–694.

    Article  Google Scholar 

  • ___, P. J. Woodsworth, P. J. Wynne, and A. Morrison, 1985, Paleomagnetic evidence for displacement from the south of the Coast Plutonic Complex, British Columbia: Canadian Journal of Earth Science, v. 22, p. 584–598.

    Article  Google Scholar 

  • Jarrard, R. D., 1986a, Relations among subduction para-maters: Reviews of Geophysics, v. 24, p. 217–284.

    Article  Google Scholar 

  • ___, 1986b, Terrane motion by strike-slip faulting of forearc slivers: Geology, v. 14, p. 780–783.

    Article  Google Scholar 

  • Johnson, S. Y., 1984, Evidence for a margin-truncating transcurrent fault (pre-late Eocene) in western Washington: Geology, v. 11, p. 538–541.

    Article  Google Scholar 

  • Jones, D. L., D. G. Howell, P. J. Coney, and J. W. H. Monger, 1983, Recognition, character and analysis of tec-tonostratigraphic terranes in western North America; pp. 21–35 in M. Hashimto and S. Uyeda (eds.), Accretion Tectonics in the Circurn-Pacific Regions:Terra Scientific, Tokyo, Japan, 358 p.

    Chapter  Google Scholar 

  • Jones, M. E., and R. M. F. Preston (eds.), 1987, Deformation of Sediments and Sedimentary Rocks: Geological Society of London, Special Publication 9, 350 p.

    Google Scholar 

  • Karig, D. E., D. R. Sarewitz, and G. D. Haeck, 1986, Role of strike-slip faulting in the evolution of alloch-thonous terranes in the Philippines: Geology, v. 14, p. 852–855.

    Article  Google Scholar 

  • ___, and J. Mammerickx, 1972, Tectonic frame-work of the New Hebrides island arc: Marine Geology, v. 12, p. 187–205.

    Article  Google Scholar 

  • Labaume, P., 1987, Syn-diagenetic deformation of a turbidite succession related to submarine gravity nappe emplacement, Autapie Nappe, French Alps; pp. 147–163 in M. E. Jones and R. M. F. Preston (eds.), Deformation of Sediments and Sedimentary Rocks: Geological Society of London, Special Publication 9, 350 p.

    Google Scholar 

  • Laird, J., and A. L. Albee, 1981a, High-pressure meta-morphism in mafic schist from northen Vermont: American Journal of Science, v. 281, p. 97–126.

    Article  Google Scholar 

  • ___, and A. L. Albee, 1981b, Pressure, temperature and time indicators in mafic schist: Their application to reconstructing the polymetamorphic history of Vermont: American Journal of Science, v. 281, p. 127–175.

    Article  Google Scholar 

  • Laville, E., and J. P. Petit, 1984, Role of synsedi-mentary strike-slip faults in the formation of Moroccan Triassic basins: Geology, v. 12, p. 424–427.

    Article  Google Scholar 

  • Lister, G. S., and A. W. Snoke, 1984, S-C mylonites: Journal of Structural Geology, v. 6, p. 617–638.

    Article  Google Scholar 

  • Meisling, K. E., M. C. Gardener, G. W. Cushing, and S. C. Bergman, 1987, A reconstruction of southern Alaska at 75 Ma [abstract]: Geological Society of America Abstracts with Programs, v. 19, p. 769.

    Google Scholar 

  • Owen, G., 1987, Deformation processes in unconsolidated sands; pp. 11–24 in M. E. Jones and R. M. F. Preston (eds.), Deformation of Sediments and Sedimentary Rocks Geological Society of London, Special Publication 9, 350 p.

    Google Scholar 

  • Page, B. M., 1982, Migration of Salinian composite block, California, and disapppearence of fragments: American Journal of Science, v. 282, p. 1694–1734.

    Article  Google Scholar 

  • Panusk, B. C., 1987, The paleomagnetism-geology conflict in southern Alaska tectonics: A review of constraints and conjectures [abstract]: Geological Society of America Abstracts with Programs, v. 19, p. 799.

    Google Scholar 

  • Parrish, R., and J. C. Roddick, 1985, Geochronology and Isotope Geology for the Geologist and Explora-tionist:Geological Association of Canada, Cordilleran Section, Short Course No. 4, 77 p.

    Google Scholar 

  • Passchier, C. W., and C. Simpson, 1986, Porphyroclast systems as kinematic indicators: Journal of Structural Geology, v. 8, p. 831–844.

    Article  Google Scholar 

  • Pavlis, T. L., 1987, Significance of the Border Ranges fault system in the Mesozoic tectonics of the northern Cordillera [abstract]: Geological Society of America Abstracts with Programs, v. 19, p. 801.

    Google Scholar 

  • Petit, J. P., 1987, Criteria for the sense of movement on fault surfaces in brittle rocks: Journal of Structural Geology, v. 9, p. 597–608.

    Article  Google Scholar 

  • ___, and E. LaVille, 1987, Morophology and micro-structures of hydroplastic slickensides in sandstone; pp. 107–121 In M. E. Jones and R. M. F. Preston (eds.), Deformation of Sediments and Sedimentary Rocks: Geological Society of London, Special Publication 29, 350 p.

    Google Scholar 

  • Platt, J. P., 1986, Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks: Geological Society of America Bulletin, v. 97, p. 1037–1053.

    Article  Google Scholar 

  • Price, R. A., and D. M. Carmichael, 1986, Geometric test for Late Cretaceous-Paleogene intracontinental transform faulting in the Canadian Cordillera: Geology, v. 14, p. 468–471.

    Article  Google Scholar 

  • Ramsey, J. G., and M. I. Huber, 1983, The Techniques of Modern Structural Analysis, Volume 1: Strain Analysis: Academic Press, New York, New York, USA, 307 p.

    Google Scholar 

  • Roedder, E., 1984, Fluid Inclusions: Mineralogical Society of America, Reviews in Mineralogy 12, 644 p.

    Google Scholar 

  • Saleeby, J., 1977, Fracture zone tectonics, continental margin fragmentation, and emplacement of the Kings-Kaweah ophiolite belt, southwest Sierra Neveda, California; pp. 141–160 in R. Coleman and W. P. Irwin (eds.), North American Ophiolites: Oregon Department of Geology and Mineral Industries, Bulletin 95, 183 p.

    Google Scholar 

  • Sarewitz D. R., and D. E. Karig, 1986, Processes of allochthonous terrane evolution, Mindoro Island, Philippines: Tectonics, v. 5, p. 525–552.

    Article  Google Scholar 

  • Sibson, R. H., 1977, Fault rocks and fault mechanisms: Journal of the Geological Society of London, v. 133, p. 191–213.

    Article  Google Scholar 

  • Simpson C., 1986, Determination of movement sense in mylonities: Journal of Geological Education, v. 34, p. 246–261.

    Google Scholar 

  • ___, and S. M. Schmid, 1984, An evaluation of the sense of movement in sheared rocks: Geological Society of America Bulletin, v. 94, p. 1281–1288.

    Google Scholar 

  • Spear, F., S. J. Selverstone, D. Hickmott, P. Crowley, and K. V. Hodges, 1984, P-T paths from garnet zoning: A new technique for deciphering tectonic processes in crystalline terranes: Geology, v. 12, p. 87–90.

    Article  Google Scholar 

  • Suppe, J., 1970, Offset of late Mesozoic basement terranes by the San Andreas fault system: Geological Society of America Bulletin, v. 81, p. 3253–3258.

    Article  Google Scholar 

  • Turcotte, D. L., 1987, Rheology of the oceanic and continental lithosphere; pp. 61–67 in K. Fuchs and C. Froidevaux (eds.), Composition, Structure and Dynamics of the Lithosphere-Asthenosphere System: American Geophysical Union, Geodynamics Series 16, 327 p.

    Google Scholar 

  • Umhoefer, P. J., 1987, Northward translation of “Baja British Columbia” along the Late Cretaceous to Paleocene margin of western North America: Tectonics, v. 6, p. 377–394.

    Article  Google Scholar 

  • Uyeda, S., and H. Kanamori, 1979, Back-arc opening and the mode of subduction: Journal of Geophysical Research, v. 84, p. 1049–1061.

    Article  Google Scholar 

  • Vink, G. E., W. J. Morgan, and W. L. Zhao, 1984, Preferential rifting of continents: A source of displaced terranes: Journal of Geophysical Research, v. 89, p. 10,072–10,076.

    Article  Google Scholar 

  • Walcott, R. I., 1978, Geodetic strains and large earthquakes in the axial tectonic belt of North Island, New Zealand: Journal of Geophysical Research, v. 83, p. 4419–4429.

    Article  Google Scholar 

  • Wickham, J. S., 1973, An estimate of strain increments in a naturally deformed carbonate rock: American Journal Science, v. 273, p. 23–47.

    Article  Google Scholar 

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Authors and Affiliations

  1. Department of Geological Sciences, Southern Methodist University, Dallas, Texas, 75275, USA

    Vicki L. Hansen

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Editors and Affiliations

  1. Earth Sciences and Resources Institute, University of South Carolina, Columbia, SC, USA

    Mervin J. Bartholomew

  2. Department of Geology, University of Montana, Missoula, MT, USA

    Donald W. Hyndman

  3. Department of Earth Sciences, Montana State University, Bozeman, MT, USA

    David W. Mogk

  4. Department of Geological Sciences, Queen’s University, Kingston, Ontario, Canada

    Robert Mason

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Hansen, V.L. (1992). The importance of subduction-related margin-parallel shear zones along transpressional convergent plate margins. In: Bartholomew, M.J., Hyndman, D.W., Mogk, D.W., Mason, R. (eds) Basement Tectonics 8. Proceedings of the International Conferences on Basement Tectonics, vol 2. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1614-5_5

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  • DOI: https://doi.org/10.1007/978-94-011-1614-5_5

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