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Статті в журналах з теми "Crustal tectonics"
Hawkesworth, Chris J., Peter A. Cawood, and Bruno Dhuime. "Tectonics and crustal evolution." GSA Today 26, no. 09 (August 16, 2016): 4–11. http://dx.doi.org/10.1130/gsatg272a.1.
Повний текст джерелаMueller, D. "Plate tectonics and crustal evolution." Eos, Transactions American Geophysical Union 79, no. 18 (1998): 220. http://dx.doi.org/10.1029/98eo00164.
Повний текст джерелаHorscroft, Timothy J. "Plate tectonics and crustal evolution." Earth-Science Reviews 42, no. 4 (November 1997): 276–77. http://dx.doi.org/10.1016/s0012-8252(97)81863-6.
Повний текст джерелаClemens, J. D. "Plate tectonics and crustal evolution." Journal of Structural Geology 12, no. 3 (January 1990): 400–401. http://dx.doi.org/10.1016/0191-8141(90)90028-w.
Повний текст джерелаFyfe, W. S. "Fluids, tectonics and crustal deformation." Tectonophysics 119, no. 1-4 (October 1985): 29–36. http://dx.doi.org/10.1016/0040-1951(85)90031-9.
Повний текст джерелаSLEMMONS, D. B. "Crustal Extension: Continental Extensional Tectonics." Science 239, no. 4844 (March 4, 1988): 1185. http://dx.doi.org/10.1126/science.239.4844.1185.
Повний текст джерелаYang-shen, Shi, Yang Shu-feng, Guo Ling-zhi, and Dong Huo-gen. "Crustal genesis and plate tectonics." Tectonophysics 187, no. 1-3 (February 1991): 277–84. http://dx.doi.org/10.1016/0040-1951(91)90424-q.
Повний текст джерелаSingh, Vinod K. "Geology, Geomorphology and Tectonics of India: Introduction." Journal of Geoscience, Engineering, Environment, and Technology 4, no. 2-2 (July 25, 2019): 1. http://dx.doi.org/10.25299/jgeet.2019.4.2-2.2447.
Повний текст джерелаSingh, Vinod K., Ram Chandra, Asish R. Basu, Surendra P. Verma, and Tapas K. Biswal. "Precambrian crustal growth and tectonics: introduction." International Geology Review 57, no. 11-12 (May 20, 2015): v—viii. http://dx.doi.org/10.1080/00206814.2015.1029542.
Повний текст джерелаNebel, O., F. A. Capitanio, J. F. Moyen, R. F. Weinberg, F. Clos, Y. J. Nebel-Jacobsen, and P. A. Cawood. "When crust comes of age: on the chemical evolution of Archaean, felsic continental crust by crustal drip tectonics." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 376, no. 2132 (October 2018): 20180103. http://dx.doi.org/10.1098/rsta.2018.0103.
Повний текст джерелаДисертації з теми "Crustal tectonics"
Travan, Gaia. "Interactions between salt tectonics and crustal tectonics in the Mediterranean and in the Barents sea." Electronic Thesis or Diss., Université de Lille (2022-....), 2022. http://www.theses.fr/2022ULILR050.
Повний текст джерелаConsidering geological times, the behaviour of the salt can be approximated to a Newtonian fluid (i.e. viscous behaviour) compared to the brittle behaviour of the surrounding rocks, and their interaction can be modelled through scaled analogue models of a viscous material and a brittle one, e.g. silicone and sand. Crustal tectonics, both extensional and contractional, have often a fundamental role in the evolution of the salt structures, and becomes the main cause of deformation in many study areas. The aim of this thesis is to analyze the timing and mechanisms of salt tectonics in three study area characterized by different salt ages and increasing influence of crustal tectonics on the salt tectonics processes: the Western Sardinian and Northern Algerian margin (Western Mediterranean) and the Sørvestsnaget Basin (Southwestern Barents Sea). This has been done through the interpretation of 2D and 3D seismic reflection data from TGS (Norway), OGS (Italy) and UMR Geo-Ocean (France), as well as through the integration with other geophysical data, wells data and the comparison with analogue models. In the W-Mediterranean the salt deposited during the Salinity Crisis (5.6 Ma) so salt tectonics is relatively young, the overburden is thin and the marks of the first stages of deformation are usually imaged. On the W-Sardinian margin the salt structures are mainly consequence of the basinward slope of the salt base, resulting from the differential subsidence after the refilling of the Mediterranean at the end of the crisis. Moving towards the center of the Sardo-Provencal basin, where the sedimentary load of the Rhone Deep Sea Fan forms a thick salt overburden, gravity spreading dominates. While in this area there is no influence of crustal tectonics on salt deformation at a regional scale, we recognized on the SW-Sardinian margin the presence of a flower structure active during Pliocene. We propose it to be part of the North Balearic Fracture Zone, i.e. the dextral strike-slip fault of the Sardo-Provençal basin opening, never recognized in the area.The southern sector of the Western Mediterranean is reactivated in compression since 8 Ma due to the Africa-Europe convergence, and this compression is expressed through thrusts on the Algerian margin. Here salt tectonics is mainly the consequence of crustal tectonics, and in particular of the increased potential energy consequence of the localized uplift. The analogue models produced show that the uplift of the plateau is at the origin of the lateral thickness variations in the salt layer and of the polygonal minibasins formation in the area offshore Algiers. A component of gravity gliding related to the basin subsidence is present.The third study area is the Sørvestsnaget Basin in the SW Barents Sea. Here the Permian salt formed structures that are the result of hundreds of millions years of deformation, mainly through reactive and active salt diapirism consequence of the Mesozoic extensional tectonics due to the Atlantic Ocean opening. This lead to the formation of massive allochthonous salt structures and locally to their deflation. After the end of the crustal extension, the main influence on the salt deformation is attributable to the Quaternary glacial sedimentary wedge and the consequent glacio-isostatically controlled crustal movements, leading to internal redistribution in the allochthonous salt structures. Part of the hypothesis on the salt tectonics mechanisms in the Sørvestsnaget basin were confirmed through analogue modelling.Thanks to the diversity between the three study areas in terms of geological setting, we offer not only a broad picture of different levels of interaction between salt and crustal tectonics, but also of the effect of salt basal slope and differential sedimentary load on the salt structures evolution, as well as different levels of maturity of salt structures, from the younger ones (e.g. salt rollers) to the more mature ones (e.g. salt sheets)
Cragg, Ian Alan. "Numerical modelling of crustal scale fault propagation." Thesis, University of Liverpool, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321166.
Повний текст джерелаRayson, Martin W. "Computer aided design of geodetic networks for monitoring crustal tectonics." Thesis, University of Newcastle Upon Tyne, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.278767.
Повний текст джерелаGordon, Andres Cesar. "Arquitetura crustal da bacia de Almada no contexto das bacias da margem lesste da América do Sul." Universidade do Estado do Rio de Janeiro, 2011. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=2446.
Повний текст джерелаThe Almada Basin, located in the Bahia State, shares similar characteristics with other eastern Brazilian basins when analyzed in terms of major sedimentation process and dominant stress regime. However, a remarkably different composition of the transitional crust is observed when this basin is compared with the other eastern Brazilian basins. A large 3D survey, acquired with cable length of 6 km and 9.2 seconds resulted in good seismic images of the rift deep structure. A detailed gravity survey and 2D forward modeling were integrated with the seismic analysis to corroborate the geological model. The Almada Basin is part of the continental rift system that developed during the Berriasian to Aptian times, heralding the Gondwana break up. Subsequently the basin evolved into a passive divergent margin. The rifting process results in five NNE-SSW striking half-graben sub-basins, from onshore to deep water, producing a complex structural framework. Deep seismic profiles reveal the progressive thinning of the continental crust down to 5 km below the easternmost half-graben with a crustal β factor of 7 before the ocean crust developed. The good-quality seismic images also allowed the recognition of major listric faults systems that cut the upper crust, linking the half-grabens and detaching along the layered lower crust. The basin shows an asymmetrical crustal profile compatible with a simple shear rifting mechanism. Volcanic Margins (VM) and Non Volcanic Margins (NVM) are the end members of the crustal compositional analysis of divergent continental margins. The key architectural elements of the VM, such as large igneous provinces, seaward dipping reflectors and the basinal synrift magmatism, are not recognized in the Almada Basin. Even though the South Atlantic divergent margin is traditionally interpreted as a VM, particularly in the rift segment south of Bahia State, the lack of these key elements, as well as drilling results, indicate a non volcanic character for the Almada segment. Regionally, the South American divergent margin is mostly volcanic, but the amount and the influence of the magmatism during the rift phase is variable from the southernmost Austral Basin in south Argentina up to the Pernambuco Basin in northeast Brazil. Along the whole continental margin different segments of strong, medium and non volcanic character can be recognized. In the classical NVM, the transitional crust is highly stretched and, in some cases, it shows evidence of exhumed sub continental mantle (e.g., Iberian margin). In the Almada Basin, the transitional crust indicates a considerable thinning, but there is no clear evidence of mantle exhumation. The mechanisms responsible for the generation and emplacement of the large amounts of magma recorded in the divergent margins are still subject to discussions. Along the South American segments, both the lithospheric thinning and mantle plume models have been proposed. Alternatively, a combination of these two mechanisms may have played an important role in the margin evolution.
Gilbert, John Bennett. "Crustal Deformation During Arc-Flare Up Magmatism: Field And Microstructural Analysis Of A Mid-Crustal, Melt Enhanced Shear Zone." ScholarWorks @ UVM, 2017. http://scholarworks.uvm.edu/graddis/699.
Повний текст джерелаChan, Yau-cheong Ian, and 陳有昌. "Characterizing crustal melt episodes in the Himalayan orogen." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/206505.
Повний текст джерелаpublished_or_final_version
Applied Geosciences
Master
Master of Science
Lawson, N. Kate. "Crustal accretion near ridge-transform intersections : Kane fracture zone, mid-Atlantic ridge." Thesis, Durham University, 1996. http://etheses.dur.ac.uk/1157/.
Повний текст джерелаLeftwich, Timothy E. "Geopotential investigations of the crustal structure and evolution of Mars." The Ohio State University, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=osu1147893346.
Повний текст джерелаDilles, Zoe Y. G. "Geochronologic and Petrologic Context for Deep Crustal Metamorphic Core Complex Development, East Humboldt Range, Nevada." Scholarship @ Claremont, 2016. http://scholarship.claremont.edu/scripps_theses/811.
Повний текст джерелаWightman, R. T. "Constraints on crustal development and tectonics in the Archaean rocks of south India." Thesis, Open University, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.374494.
Повний текст джерелаКниги з теми "Crustal tectonics"
Condie, Kent C. Plate tectonics & crustal evolution. 3rd ed. Oxford: Pergamon, 1989.
Знайти повний текст джерелаPlate tectonics & crustal evolution. 3rd ed. Oxford: Pergamon Press, 1989.
Знайти повний текст джерелаCondie, Kent C. Plate tectonics & crustal evolution. 3rd ed. Oxford: Pergamon Press, 1993.
Знайти повний текст джерелаC, Condie Kent, ed. Plate tectonics and crustal evolution. 4th ed. Oxford: Butterworth Heinemann, 1997.
Знайти повний текст джерелаH, Sychanthavong S. P., and Merh S. S, eds. Crustal evolution and orogeny. New Delhi: Oxford & IBH Pub. Co., 1990.
Знайти повний текст джерелаR, Rice J., and United States. National Aeronautics and Space Administration., eds. Crustal deformation in great California eartquake cycles. [Washington, DC: National Aeronautics and Space Administration, 1986.
Знайти повний текст джерелаParsons, Tom. Crustal structure of the Cascadia fore arc of Washington. Reston, Va: U.S. Geological Survey, 2005.
Знайти повний текст джерелаE, Smith David, and Turcotte Donald Lawson, eds. Contributions of space geodesy to geodynamics: Crustal dynamics. Washington, D.C: American Geophysical Union, 1993.
Знайти повний текст джерелаBuiter, Susanne J. H. 1970-, Schreurs Guido, and Geological Society of London, eds. Analogue and numerical modelling of crustal-scale processes. London: Geological Society, 2006.
Знайти повний текст джерелаUnited States. National Aeronautics and Space Administration., ed. Viscoelastic deformation near active plate boundaries. [Washington, DC: National Aeronautics and Space Administration, 1986.
Знайти повний текст джерелаЧастини книг з теми "Crustal tectonics"
Muñoz, Josep Anton. "Evolution of a continental collision belt: ECORS-Pyrenees crustal balanced cross-section." In Thrust Tectonics, 235–46. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3066-0_21.
Повний текст джерелаGallagher, John J. "Tectonics of China: Continental Scale Cataclastic Flow." In Mechanical Behavior of Crustal Rocks, 259–73. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm024p0259.
Повний текст джерелаPirajno, Franco. "Crustal Evolution, Global Tectonics and Mineral Deposits." In Hydrothermal Mineral Deposits, 159–96. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-75671-9_6.
Повний текст джерелаBrown, Richard L., Sharon D. Carr, Bradford J. Johnson, Vicki J. Coleman, Frederick A. Cook, and John L. Varsek. "The Monashee decollement of the southern Canadian Cordillera: a crustal-scale shear zone linking the Rocky Mountain Foreland belt to lower crust beneath accreted terranes." In Thrust Tectonics, 357–64. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3066-0_32.
Повний текст джерелаBassi, H. G. L. "El Morro: A Tertiary Volcanic Event Controlled by Pre-Paleozoic Crustal Fracturing, San Luis, Argentina." In Basement Tectonics 10, 323–31. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-017-0831-9_30.
Повний текст джерелаSchwarz, Gerhard, Guillermo Chong Diaz, Detlef Krüger, Eloy Martinez, Winfrid Massow, Volker Rath, and José Viramonte. "Crustal High Conductivity Zones in the Southern Central Andes." In Tectonics of the Southern Central Andes, 49–67. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-77353-2_3.
Повний текст джерелаRooney, Sean T., Donald D. Blankenship, and Charles R. Bentley. "Seismic Refraction Measurements of Crustal Structure in West Antarctica." In Gondwana Six: Structure, Tectonics, and Geophysics, 1–7. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm040p0001.
Повний текст джерелаKahle, Hans-Gert, Max V. Müller, Stephan Mueller, George Veis, Haris Billiris, Demitris Paradissis, Hermann Drewes, et al. "Monitoring West Hellenic Arc tectonics and Calabrian Arc tectonics (“WHAT A CAT”) using the Global Positioning System." In Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 417–29. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0417.
Повний текст джерелаRobaudo, Stefano, and Christopher G. A. Harrison. "Plate tectonics from SLR and VLBI global data." In Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 51–71. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0051.
Повний текст джерелаCook, Frederick A., Dan B. McCullar, Edward R. Decker, and Scott B. Smithson. "Crustal Structure and Evolution of the Southern Rio Grande Rift." In Rio Grande Rift: Tectonics and Magmatism, 195–208. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/sp014p0195.
Повний текст джерелаТези доповідей конференцій з теми "Crustal tectonics"
Zolnai, G. "Understanding Petroleum Systems in the Light of Crustal Tectonics." In 61st EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609.201407797.
Повний текст джерелаLappin, M. "Salt pillows, salt walls and crustal tectonics in the UK Southern Gas Basin." In 55th EAEG Meeting. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609.201411699.
Повний текст джерелаD. Brown, Larry, Andrew Ross, and Camelia Diaconescu. "Seismic Bright Spots, Magmatism, Rheology and Moho Tectonics: New Results from Crustal Seismic Profiling." In 5th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.299.290.
Повний текст джерелаDeLucia, Michael S., Mary Seid, Stephen Marshak, Alison Anders, Gary L. Pavlis, Xiaotao Yang, Hersh Gilbert, Chen Chen, Michael W. Hamburger, and Timothy Larson. "STRUCTURAL AND GEOMORPHOLOGICAL MANIFESTATIONS OF THE CRUSTAL BOUNDARY BETWEEN THE ILLINOIS BASIN AND OZARK DOME: IMPLICATIONS FOR MIDCONTINENT TECTONICS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286885.
Повний текст джерелаZhao, Guochun. "DILEMMAS OF PLATE TECTONICS IN EXPLAINING THE NEOARCHEAN CRUSTAL FORMATION AND EVOLUTION OF THE EASTERN BLOCK, NORTH CHINA CRATON." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338062.
Повний текст джерелаBennett, Vickie, and Allen Nutman. "The Case for Eoarchean Plate Tectonics and Limited Early Crustal Volumes from Integrated Geologic and Isotopic Observations in Southwest Greenland." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.168.
Повний текст джерелаHasnan, Zurriya Hayati, Amir Ayub, Mohammad Hishamuddin Ismail, Mariah Harris, Soon Mun Chin, Syarifah Nur Syed Khastudin, Nur Yusra Mansor, Tengku Mohd Tengku Hassan, Noor Farahida Ahmad Sharif, and Xavier Legrand. "The Black Sea, the Latest New Exploration Frontiers in Europe: Preliminary Results of an Escape Tectonics." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21156-ms.
Повний текст джерелаBoavida, J., E. Vagnes, P. Gerónimo, J. M. Peliganga, M. Inkollu, M. de Brito, and M. Symonds. "Crustal structure, rift tectonics and pre-salt stratigraphy beneath the Ultra Deep Water area offshore Angola: Results from reprocessed seismic data." In 7th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.143.16.2.
Повний текст джерелаBethune, Kathryn, Kenneth Ashton, Colin Card, Michael Cloutier, and Jordan Deane. "TECTONICS OF WSW RAE CRATON OF LAURENTIA; EVIDENCE FOR CRUSTAL ASSEMBLY BY COLLISIONAL, ACCRETIONARY PROCESSES FROM THE MID-NEOARCHEAN TO EARLY PALEOPROTEROZOIC." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358460.
Повний текст джерелаvan Rooyen, Deanne, and David Corrigan. "PLATE TECTONICS DURING THE 1.9 – 1.7 GA ASSEMBLY OF NUNA; EXAMPLES OF MODERN CRUSTAL COLLISION AND TRANSPORT PROCESSES FROM THE SOUTHEASTERN CHURCHILL PROVINCE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-353342.
Повний текст джерелаЗвіти організацій з теми "Crustal tectonics"
Sweeney, J. F., R. A. Stephenson, R. G. Currie, and J. M. Delaurier. Crustal Geophysics [Chapter 2: Tectonic Framework]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134077.
Повний текст джерелаMatte, S., M. Constantin, and R. Stevenson. Mineralogical and geochemical characterisation of the Kipawa syenite complex, Quebec: implications for rare-earth element deposits. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329212.
Повний текст джерелаHayward, N., and S. Paradis. Geophysical reassessment of the role of ancient lineaments on the development of the western margin of Laurentia and its sediment-hosted Zn-Pb deposits, Yukon and Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330038.
Повний текст джерелаZagorevski, A., C. R. van Staal, J. H. Bédard, A. Bogatu, D. Canil, M. Coleman, M. Golding, et al. Overview of Cordilleran oceanic terranes and their significance for the tectonic evolution of the northern Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326053.
Повний текст джерелаHeather, K. B., J. A. Percival, D. Moser, and W. Bleeker. Tectonics and metallogeny of Archean crust in the Abitibi-Kapuskasing-Wawa region. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205285.
Повний текст джерелаHayward, N., and J. J. Ryan. Geophysical characteristics of the northern Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326069.
Повний текст джерелаKeen, C. E., K. Dickie, L. T. Dafoe, T. Funck, J. K. Welford, S A Dehler, U. Gregersen, and K J DesRoches. Rifting and evolution of the Labrador-Baffin Seaway. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321854.
Повний текст джерелаSt-Onge, M. R., and S. B. Lucas. New insight on the crustal struture and tectonic history of the Ungava Orogen, Kovik Bay and Cap Wolstenholme, Québec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132846.
Повний текст джерелаKarson, Jeffrey A. Variations in Tectonic Extension Along SLow-Spreading Ridge Axes: Implications for the Internal Structure and Bathymetry of Oceanic Crust. Fort Belvoir, VA: Defense Technical Information Center, January 1992. http://dx.doi.org/10.21236/ada244583.
Повний текст джерелаKuster, K., C. M. Lesher, and M. G. Houlé. Geology and geochemistry of mafic and ultramafic bodies in the Shebandowan mine area, Wawa-Abitibi terrane: implications for Ni-Cu-(PGE) and Cr-(PGE) mineralization, Ontario and Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329394.
Повний текст джерела