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Статті в журналах з теми "Craton margins"
Wang, Xu, Peimin Zhu, Timothy M. Kusky, Na Zhao, Xiaoyong Li, and Zhensheng Wang. "Dynamic cause of marginal lithospheric thinning and implications for craton destruction: a comparison of the North China, Superior, and Yilgarn cratons." Canadian Journal of Earth Sciences 53, no. 11 (November 2016): 1121–41. http://dx.doi.org/10.1139/cjes-2015-0110.
Повний текст джерелаDalziel, Ian W. D. "Antarctica and supercontinental evolution: clues and puzzles." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 104, no. 1 (March 2013): 3–16. http://dx.doi.org/10.1017/s1755691012000096.
Повний текст джерелаPearson, N. J., S. Y. O'Reilly, and W. L. Griffin. "The crust-mantle boundary beneath cratons and craton margins: a transect across the south-west margin of the Kaapvaal craton." Lithos 36, no. 3-4 (December 1995): 257–87. http://dx.doi.org/10.1016/0024-4937(95)00021-6.
Повний текст джерелаHoffman, Paul F. "The Origin of Laurentia: Rae Craton as the Backstop for Proto-Laurentian Amalgamation by Slab Suction." Geoscience Canada 41, no. 3 (August 29, 2014): 313. http://dx.doi.org/10.12789/geocanj.2014.41.049.
Повний текст джерелаLikhanov, Igor I. "Provenance, Age, and Tectonic Settings of Rock Complexes (Transangarian Yenisey Ridge, East Siberia): Geochemical and Geochronological Evidence." Geosciences 12, no. 11 (October 29, 2022): 402. http://dx.doi.org/10.3390/geosciences12110402.
Повний текст джерелаErnst, Richard, and Wouter Bleeker. "Large igneous provinces (LIPs), giant dyke swarms, and mantle plumes: significance for breakup events within Canada and adjacent regions from 2.5 Ga to the PresentThis article is one of a selection of papers published in this Special Issue on the the theme Lithoprobe—parameters, processes, and the evolution of a continent.Lithoprobe Contribution 1482. Geological Survey of Canada Contribution 20100072." Canadian Journal of Earth Sciences 47, no. 5 (May 2010): 695–739. http://dx.doi.org/10.1139/e10-025.
Повний текст джерелаManighetti, Isabelle, André Michard, and Omar Saddiqi. "The West African Craton and its margins. Foreword." Comptes Rendus Geoscience 350, no. 6 (September 2018): 233–35. http://dx.doi.org/10.1016/j.crte.2018.07.001.
Повний текст джерелаHoffman, Paul F., Samuel A. Bowring, Robert Buchwaldt, and Robert S. Hildebrand. "Birthdate for the Coronation paleocean: age of initial rifting in Wopmay orogen, CanadaThis article is one of a series of papers published in this Special Issue on the theme of Geochronology in honour of Tom Krogh." Canadian Journal of Earth Sciences 48, no. 2 (February 2011): 281–93. http://dx.doi.org/10.1139/e10-038.
Повний текст джерелаCurrie, Claire A., and Jolante van Wijk. "How craton margins are preserved: Insights from geodynamic models." Journal of Geodynamics 100 (October 2016): 144–58. http://dx.doi.org/10.1016/j.jog.2016.03.015.
Повний текст джерелаGorczyk, W., D. R. Mole, and S. J. Barnes. "Plume-lithosphere interaction at craton margins throughout Earth history." Tectonophysics 746 (October 2018): 678–94. http://dx.doi.org/10.1016/j.tecto.2017.04.002.
Повний текст джерелаДисертації з теми "Craton margins"
Nowicki, Thomas Edward. "Mantle xenoliths from the Abrahamskraal kimberlite : a craton-margin geotherm." Thesis, Rhodes University, 1991. http://hdl.handle.net/10962/d1001557.
Повний текст джерелаDowney, Matthew. "The Structural Geology, Kinematics and Timing of Deformation at the Superior craton margin, Gull Rapids, Manitoba." Thesis, University of Waterloo, 2005. http://hdl.handle.net/10012/1258.
Повний текст джерелаThe Gull Rapids area records a complex tectonic history. The area experienced four generations of Neoarchean ductile and brittle deformation (G1 ? G4) and one of Paleoproterozoic ductile-brittle deformation (G5). G1 deformation produced the main foliation in the map area, as well as local isoclinal folding which may be related to an early shearing event. M1a prograde mid-amphibolite facies metamorphism is contemporaneous with the early stages of G1. Widespread, tight to isoclinal sheath folding during G2 was recorded in the supracrustal assemblage, and is the result of southwest-side-up, dextral shearing during the early shearing event. A ca. 2. 68 Ga widespread phase of granitoid intrusion was emplaced late-G1 to early-G2, and is rich in metamorphic minerals that record conditions of M1b upper-amphibolite facies peak metamorphism. M1b metamorphism, late-G1 to early-G2 deformation, and intrusion of this felsic phase are contemporaneous. M2 retrograde metamorphism to mid-amphibolite facies was recorded sometime after M1b. G1 and G2 structures were re-folded during G3, which was then followed by G4 southwest-side-up, dextral and sinistral shearing, contemporaneous with late pegmatite intrusion at ca. 2. 61 Ga. This was followed by mafic dyke emplacement at ca. 2. 10 Ga, and then by G5 sinistral and dextral shearing and M3 greenschist facies metamorphism or hydrothermal alteration at ca. 1. 80 Ga.
Deformation and metamorphism at Gull Rapids post-dates emplacement and deposition of gneissic and supracrustal rocks, respectively. This deformation and metamorphism, except for G5 and M3, is Neoarchean (ca. 2. 68?2. 61 Ga), and represents a significant movement of crustal blocks: km-scale shearing of the supracrustal assemblage and consequent uplift of the Split Lake Block. Late deformation and metamorphism (G5, M3) may be related to the Paleoproterozoic Trans-Hudson orogeny. The Neoarchean and Paleoproterozoic zircon populations in the geochronological data suggest that the Gull Rapids area largely experienced Neoarchean deformation and metamorphism with a weak Paleoproterozoic overprint. All of the evidence presented above suggests that the Gull Rapids area lies in a part of the Superior Boundary Zone, yet does not lie at the exact margin of the Superior craton, and therefore does not mark the Archean-Proterozoic boundary proper in northeastern Manitoba.
Bagai, Zibisani. "Geodynamic evolution and petrogenesis of the neoarchaean Francistown granite-greenstone complex in NE Botswana, SW margin of the Zimbabwe craton." Doctoral thesis, University of Cape Town, 2009. http://hdl.handle.net/11427/4187.
Повний текст джерелаIncludes bibliographical references.
The Archaean Francistown Granite-Greenstone Complex in NE Botswana is an integral part of the southwestern margin of the Zimbabwe Craton. It includes a suite of geochemically diverse Neoarchaean granitoids and mafic dominated-supracrustal assemblages. All the supracrustal rocks and mafic intrusions have undergone greenschist to lower amphibolite facies metamorphism, but most mafic intrusions have preserved original igneous textures. The Francistown Granite Greenstone Complex likely represents an arc complex that developed along an active continental margin in the Neoarchaean. This thesis presents new geological, geochemical and geochronological data with which to evaluate the crustal evolution of the NE Botswana, and with which to formulate a geodynamic model for better understanding of the Archaean crustal growth flanking the southwestern margin of the Zimbabwe Craton
Esteves, Melina Cristina Borges. "Thermal history and fluid circulation in deformational structures associated with the Bambuí Group at the fold-and-thrust zone, western margin of the São Francisco Craton." Universidade de São Paulo, 2018. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-10092018-135551/.
Повний текст джерелаP-T conditions existing at the tectonic event that acted at the fold-and-thrust zone of the western margin of the São Francisco Craton were estimated on the basis of structural, microstructural, petrographic and fluid inclusion study of syntectonic veins. The presence of veins of different generations in the fold-and-thrust zone is evidenced by fluids operating at different scenarios of paleostress throughout the deformation history. The area are composed of weakly deformed rocks of the Bambuí Group recording a metamorphism with conditions ranging from diagenetic to sub-greenschist facies. Two tectonic events were identified by vein geometric arrangement and folded surface, a major early NE-SW compression (D1 - \'sigma\'1 subhorizontal SW-trending and \'sigma\'3 subvertical), related with subhorizontal NW-trending syntectonic veins formed at conditions that have reached at least 140°C and pressures around 200-363 MPa; and later NW-SE compression (D2 - \'sigma\'1 subhorizontal NW-trending and \'sigma\'3 subhorizontal NE-trending), related with subvertical syntectonic cleavage-parallel veins formed at the same range of temperature and pressures between 181-295 MPa. Indication of fluctuations in pressure during these events played a crucial role as fluids significantly influence the mechanical processes, deformation mechanisms and chemical reactions that operate in fold-thrust belts. Fluids show H2O-NaCl-CaCl2 composition where mixing process of different fluids sources (metamorphic and meteoric) are evidenced by evolutive trending of homogenization temperatures and salinities resulting in some variation in salinity (12 against 4 wt.% NaCl eq. for subhorizontal and cleavage-parallel veins respectively). This research confirms that combine the reconstruction of the paleostress states and fluid inclusion studies can provide fundamental information of relationship between fluid flow and tectonic of orogenic terrains contributing to the scientific knowledge about the deformational/metamorphic evolution of the Bambuí Group and the fold-and-thrust zone of the western margin of the São Francisco Craton.
Nethenzheni, Sedzani Shane. "The geochemistry, geochronology and petrogenetic characteristics of two granitic suites on the eastern margin of the Namaqua Sector, Namaqua-Natal Mobile Belt, South Africa." Thesis, University of the Western Cape, 2016. http://hdl.handle.net/11394/5209.
Повний текст джерелаThe group of granites on the eastern margin of the Mesoproterozoic Namaqua sector of the polydeformed and highly metamorphosed Namaqua-Natal Province of southern Africa is known as the Keimoes Suite. The suite includes mixtures of diverse rock types not belonging to a single intrusive series and so it should be subdivided into more than one intrusive suite. The exact definition, extent, distribution and petrogenesis of these granites have been poorly defined in the past, with various authors defining the suite differently due to the lack of proper geochronology and geochemical data. The exact contact between the Namaqua sector and Kaapvaal Craton together with the role of the suite to the Namaqua tectonic evolution is still unclear. The granites of the Keimoes Suite are thought to mark the contact between the Namaqua sector and the Kaapvaal Craton. This study seeks to address the above mentioned problems by making use of new geochronology, isotope, major and trace element geochemistry together with petrography. The granites of the Keimoes Suite were previously grouped based on their degree of deformation. The geochronology, undertaken as part of this study, has proven that this classification is unfounded. The degree of foliation in these granites appears to be largely controlled by the abundance of platy minerals, such as biotite and muscovite, together with the intrusion mechanism, with deformational processes, such as shearing, playing a secondary role. The geochronology, together with geochemistry has helped to redefine the previously defined Keimoes Suite so that two well defined separate suites are recognized and the third is poorly defined due to lack of more samples of that age group. The new classification or grouping of the granites of the eastern Namaqua sector allows a more detailed examination of the tectonic evolution of this region. A member of the 1225 to 1200 Ma early syn-tectonic granites, the Josling Granite, shows a strongly developed foliation and was derived from a depleted source with a relatively low continental crustal component. This granite intruded during the time of arc accretion, and is associated with, and partly responsible for the D₁ deformation and M₁ metamorphism recognized in most of the rocks of the eastern terranes of the Namaqua sector. In terms of age, the syn-tectonic granites of the Augrabies Suite extend from 1200 to 1120 Ma and were largely derived from depleted sources with variable but more substantial amounts of continental crustal components as compared to the early syn-tectonic granite. The granites of this suite intruded during the period of peak D₂ deformation with peak magmatism between 1180 - 1135 Ma, and particularly around 1150 Ma, during the peak of metamorphism (M₂) caused by, and associated with these voluminous intrusions. The Keimoes Suite can now be defined as comprising granites of late- to post-tectonic age relative to the 1.2 - 1.08 Ga Namaquan Orogeny with magmatism occurring on the western side of the Kaapvaal Craton. The 1116 to 1066 Ma Keimoes Suite intruded during the stage of the Namaquan Orogeny in which there was continued indentation of the Kaapvaal Craton into the Namaqua sector with wrenching and shearing causing the development of rifting into which the granites intruded. The Keimoes Suite granites were derived from continental crustal sources and incorporated varying degrees of depleted source components. The intrusives and extrusives of this age occured after the main collisional event between the Namaqua Sector and the Kaapvaal Craton and are associated with the D₃ deformational event, imparting the thermal conditions leading to the M₃ metamorphic event of the rocks within both the Kakamas and Areachap Terranes. The suites mark the suture between the Archean Kaapvaal Craton and the Proterozoic Namaqua sector. The compositions of the granites of the individual suites were mainly controlled by the source with the degree of partial melting exerting a major control. The proportion of entrained peritectic assemblages and accessory minerals played a major role in controlling the compositions of the granites, particularly those of the trace elements. Variations within the compositions of the same suite are due to source heterogeneities. Generally, fractionation processes played a secondary role in influencing the composition of the granites.
Council for Geoscience and National Research Foundation
Loparev, Artiom. "Géométries crustales, évolution paléogéographique et histoire de l'accumulation terrigène des bassins de la marge passive du craton guyanais." Thesis, Toulouse 3, 2020. http://www.theses.fr/2020TOU30170.
Повний текст джерелаThis thesis is a part of "Source to Sink Guyana" project supported by TOTAL and BRGM. Its objective was to establish bases for a Source to Sink study of the Guiana Shield, by studying the geo-dynamic evolution of its passive margin since 200 Ma. These objectives were acquired after seismic data interpretation, crustal cross-sections and paleogeographic maps constructions and terrigeneous accumulation history quantification of the margin. The passive margin of the Guiana Shield is composed of two basins: Guiana/Suriname (GS) and Foz d'Amazonas (FOZ), derived from a Jurassic then Lower Cretaceous diachronous rifting respectively. The study of the subsurface data allowed us to show that the superimposition of the two rifts has shaped the Demerara Shelf into a continental block, thinned twice and surrounded by oceanic crust on three sides. The more oblique rifting of the FOZ basin forms systematically narrower segments and finer syn-rift deposits than in the GS basin. The paleo-geographic evolution of the margin and terrigenous accumulation, over eight intervals of time (from 200 Ma), show a different evolution of the two basins. The lithological distribution of sedimentary systems is homogenized from the Campanian, when both basins reach the late-post-rift stage, during which the distribution is mainly controlled by continental river dynamics. Terrestrial accumulated volumes show however an opposite evolution during Cretaceous in both basins, in connection with the decrease and increase in the drained areas of the major rivers of this region, Paleo-Berbice and Paleo-Tocantins respectively. Siliclastic inputs towards the margin are generally low (between 2 and 11 m/Ma), but alternating with periods of high inputs corresponding to the recreation of the relief on the continent
He, Yanhong. "Ages and geochemistry of the Xiong'er volcanic rocks along the southern margin of the North China Craton implications for the outgrowths of the paleo-mesoproterozoic supercontinent Columbia (Nuna) /." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/B4163424X.
Повний текст джерелаHe, Yanhong, and 何艷紅. "Ages and geochemistry of the Xiong'er volcanic rocks along the southern margin of the North China Craton: implications for the outgrowths of the paleo-mesoproterozoicsupercontinent Columbia (Nuna)." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B4163424X.
Повний текст джерелаDavenport, Kathy. "Continental Tectonics from Dense Array Seismic Imaging: Intraplate Seismicity in Virginia and a Steep Cratonic Margin in Idaho." Diss., Virginia Tech, 2016. http://hdl.handle.net/10919/72976.
Повний текст джерелаPh. D.
Durham, Rachel Lauren. "POTENTIAL FIELD MODELING ACROSS THE NEODYMIUM LINE DEFINING THE PALEOPROTEROZOIC-MESOPROTEROZOIC BOUNDARY OF THE SOUTHEASTERN MARGIN OF LAURENTIA." UKnowledge, 2017. http://uknowledge.uky.edu/ees_etds/53.
Повний текст джерелаКниги з теми "Craton margins"
Brommer, Axel. Strukturelle Entwicklung und Petrogenese des nördlichen Kristallingürtels der Shackleton Range, Antarktis: Proterozoische und Ross-orogene Krustendynamik am Rand des Ostantarktischen Kratons = Structural evolution and petrogenesis of the nothern crystalline belt of the Shackleton Range, Antarctica : Proterozoic and Ross-orogenic crustal dynamics along the margin of the East Antarctic Craton. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1998.
Знайти повний текст джерелаBott, M. H. P. Sedimentary Basins of Continental Margins and Cratons. Elsevier, 2013.
Знайти повний текст джерелаBooth, Adam M., and Anita L. Grunder, eds. From Terranes to Terrains: Geologic Field Guides on the Construction and Destruction of the Pacific Northwest. Geological Society of America, 2021. http://dx.doi.org/10.1130/fld062.
Повний текст джерелаЧастини книг з теми "Craton margins"
Heilbron, Monica, Umberto G. Cordani, and Fernando F. Alkmim. "The São Francisco Craton and Its Margins." In São Francisco Craton, Eastern Brazil, 3–13. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-01715-0_1.
Повний текст джерелаAdams, John, and Peter W. Basham. "Seismicity and Seismotectonics of Canada’s Eastern Margin and Craton." In Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound, 355–70. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2311-9_21.
Повний текст джерелаMüller, Daniel, and David I. Groves. "Direct Associations Between Potassic Igneous Rocks and Copper-Gold Deposits on Craton Margins." In Potassic Igneous Rocks and Associated Gold-Copper Mineralization, 191–201. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-23051-1_7.
Повний текст джерелаMüller, Daniel, and David I. Groves. "Direct Associations Between Potassic Igneous Rocks and Copper–Gold Deposits on Craton Margins." In Potassic Igneous Rocks and Associated Gold-Copper Mineralization, 255–77. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-92979-8_7.
Повний текст джерелаGordon, Andres, Nivaldo Destro, and Monica Heilbron. "The Recôncavo-Tucano-Jatobá Rift and Associated Atlantic Continental Margin Basins." In São Francisco Craton, Eastern Brazil, 171–85. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-01715-0_9.
Повний текст джерелаVeevers, J. J. "Basins of the Australian Craton and Margin." In Dynamics of Plate Interiors, 73–80. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gd001p0073.
Повний текст джерелаJiang, Yuhang, Yan Zhao, and Hecai Niu. "Paleoproterozoic Copper System in the Zhongtiaoshan Region, Southern Margin of the North China Craton: Ore Geology, Fluid Inclusion, and Isotopic Investigation." In Main Tectonic Events and Metallogeny of the North China Craton, 229–50. Singapore: Springer Singapore, 2016. http://dx.doi.org/10.1007/978-981-10-1064-4_9.
Повний текст джерелаBartholomew, Mervin J. "Structural characteristics of the Late Proterozoic (post-Grenville) continental margin of the Laurentian craton." In Proceedings of the International Conferences on Basement Tectonics, 443–67. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-1614-5_30.
Повний текст джерелаZhao, Taiping, and Xiaoqin Deng. "Petrogenesis and Tectonic Significance of the Late Paleoproterozoic to Early Mesoproterozoic (~1.80–1.53 Ga) A-Type Granites in the Southern Margin of the North China Craton." In Main Tectonic Events and Metallogeny of the North China Craton, 423–34. Singapore: Springer Singapore, 2016. http://dx.doi.org/10.1007/978-981-10-1064-4_16.
Повний текст джерелаSuryanarayana Rao, K. V., C. Kumar, A. Kumar, V. Nandish, and R. T. Swamy. "Lamproites from the Eastern Margin of the Bhandara Craton, Orissa, India: An Exploration Case Study." In Proceedings of 10th International Kimberlite Conference, 129–41. New Delhi: Springer India, 2013. http://dx.doi.org/10.1007/978-81-322-1173-0_9.
Повний текст джерелаТези доповідей конференцій з теми "Craton margins"
Attoh, K., and L. Brown. "Deep structure of the southeastern margin of the West African craton." In 10th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609-pdb.146.5.1.
Повний текст джерелаDing, Jikai, Shihong Zhang, Shihong Zhang, David A. D. Evans, David A. D. Evans, Tianshui Yang, Tianshui Yang, et al. "NORTH CHINA CRATON: THE CONJUGATE MARGIN FOR NORTHWESTERN LAURENTIA IN RODINIA." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359523.
Повний текст джерелаCassola Molina, Eder, Naomi Ussami, and Yára Regina Marangoni. "Digital 5' x5' Gravity Maps of the Săo Francisco Craton, the Marginal Fold/Thrust Belts and Contiguous Continental Margin/Oceanic Basins." In 5th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.299.225.
Повний текст джерелаTakenaka, Lynthener B., William Griffin, Suzanne Yvette O'Reilly, Miguel Basei, Carlos Eduardo Ganade, and Dorrit E. Jacob. "Lithosphere Mapping in the South-Western Margin of the São Francisco Craton." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2535.
Повний текст джерелаKarpenko, Ivan, and Oleksii Karpenko. "Preservation and Destruction of Accumulations in Petroleum Systems of Western Margin of East European Craton." In SPE Eastern Europe Subsurface Conference. SPE, 2021. http://dx.doi.org/10.2118/208542-ms.
Повний текст джерелаHe, Yu, Yuan-Bao Wu, Yujie Zhao, and Guang-Yan Zhou. "Neoproterozoic Amphibolite-Facies Metamorphism of Douling Complex at the Northern Margin of the Yangtze Craton." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1003.
Повний текст джерелаTang, Qing, Shuhai Xiao, Ke Pang, Lei Chen, and Xunlai Yuan. "ROCKS FROM THE EAST: THE TONIAN SYSTEM ON EASTERN MARGIN OF THE NORTH CHINA CRATON." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355201.
Повний текст джерелаShatsky, Vladislav, Alexey Ragozin, Alla Logvinova, Richard Wirth, and Vadim Reutsky. "Evidence of Low Oxygen Fugacity in the Upper Mantle Domains beneath Northeastern Margin of Siberian Craton." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2351.
Повний текст джерелаRenju, M. "Review of Magmatic Systems at Cratonic Margins, Case Study of Homa Hills, Kenya." In EAGE GET 2022. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202221100.
Повний текст джерелаSu, Haiyan, Yican Liu, and Yang Yang. "Petrogenesis and Element Mobility of Neoarchean Alkaline Granitic Gneisses in the Southeastern Margin of the North China Craton." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2477.
Повний текст джерелаЗвіти організацій з теми "Craton margins"
Thomas, M. D. Magnetic and gravity characteristics of the Thelon and Taltson orogens, northern Canada: tectonic implications. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329250.
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 джерелаHarris, L. B., P. Adiban, and E. Gloaguen. The role of enigmatic deep crustal and upper mantle structures on Au and magmatic Ni-Cu-PGE-Cr mineralization in the Superior Province. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328984.
Повний текст джерелаPercival, J. A., A. H. Bailes, and V. McNicoll. Mesoarchean western margin of the Superior Craton in the Lake Winnipeg area, Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212096.
Повний текст джерелаBleeker, W., and D. E. Ames. System scale and deposit scale controls on Ni-Cu-PGE mineralisation in cratonic areas and their margins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299588.
Повний текст джерелаBostock, H. H., and W. D. Loveridge. Geochronology of the Taltson Magmatic Zone and its eastern cratonic margin, District of Mackenzie. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/126603.
Повний текст джерелаThomas, M. D. Magnetic and gravity models, northern half of the Taltson Magmatic Zone, Rae Craton, Northwest Territories: insights into upper crustal structure. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328244.
Повний текст джерела