Auswahl der wissenschaftlichen Literatur zum Thema „Deep crustal structures“
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Zeitschriftenartikel zum Thema "Deep crustal structures"
Clark, Elizabeth A., und Frederick A. Cook. „Crustal-scale ramp in a Middle Proterozoic orogen, Northwest Territories, Canada“. Canadian Journal of Earth Sciences 29, Nr. 1 (01.01.1992): 142–57. http://dx.doi.org/10.1139/e92-014.
Der volle Inhalt der QuelleKivior, Irena, David Boyd, David Tucker, Stephen Markham, Francis Vaughan, Fasil Hagos und Leslie Mellon. „Deep crustal structures interpreted from potential field data along deep seismic sounding transects in Australia“. APPEA Journal 55, Nr. 2 (2015): 450. http://dx.doi.org/10.1071/aj14085.
Der volle Inhalt der QuelleSiler, Drew L., und B. Mack Kennedy. „Regional crustal-scale structures as conduits for deep geothermal upflow“. Geothermics 59 (Januar 2016): 27–37. http://dx.doi.org/10.1016/j.geothermics.2015.10.007.
Der volle Inhalt der QuelleLouie, J. N., und J. E. Vidale. „Array analysis of reflector heterogeneity“. GEOPHYSICS 56, Nr. 4 (April 1991): 565–71. http://dx.doi.org/10.1190/1.1443074.
Der volle Inhalt der QuelleBotev, Emil, und Edelvays Spassov. „Deep velocity structure of crust and upper mantle in the central parts of Balkan Region“. Geologica Balcanica 20, Nr. 2 (30.04.1990): 71–79. http://dx.doi.org/10.52321/geolbalc.20.2.71.
Der volle Inhalt der QuelleErkhow, V. A. „Deep structure and metallogeny of the earth's crust“. Exploration Geophysics 20, Nr. 2 (1989): 37. http://dx.doi.org/10.1071/eg989037.
Der volle Inhalt der QuelleBenn, Keith, Warner Miles, Mohammad R. Ghassemi und John Gillett. „Crustal structure and kinematic framework of the northwestern Pontiac Subprovince, Quebec: an integrated structural and geophysical study“. Canadian Journal of Earth Sciences 31, Nr. 2 (01.02.1994): 271–81. http://dx.doi.org/10.1139/e94-026.
Der volle Inhalt der QuelleLouie, John N., und Robert W. Clayton. „The nature of deep crustal structures in the Mojave Desert, California“. Geophysical Journal International 89, Nr. 1 (April 1987): 125–32. http://dx.doi.org/10.1111/j.1365-246x.1987.tb04398.x.
Der volle Inhalt der QuelleSchmidt, J., D. Dyrelius, H. Palm, A. Egorkin, N. Yasulievich, E. Zolotov und J. J. Doody. „The CABLES project: Imaging deep crustal structures in the Scandinavian Caledonides“. GFF 118, sup004 (Oktober 1996): 97. http://dx.doi.org/10.1080/11035899609546415.
Der volle Inhalt der QuelleStadtlander, Ralf, und Larry Brown. „Turning waves and crustal reflection profiling“. GEOPHYSICS 62, Nr. 1 (Januar 1997): 335–41. http://dx.doi.org/10.1190/1.1444135.
Der volle Inhalt der QuelleDissertationen zum Thema "Deep crustal structures"
Shi, Zhiqun. „Automatic interpretation of potential field data applied to the study of overburden thickness and deep crustal structures, South Australia“. Title page, contents and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09PH/09phs5548.pdf.
Der volle Inhalt der QuelleGonçalves, Susana Ferreira D. S. „Geophysical characterization of the Crustal structures from Equatorial to North-East Brazilian margins“. Electronic Thesis or Diss., Brest, 2023. https://theses.hal.science/tel-04619710.
Der volle Inhalt der QuelleAdaptation and application of 3D gravity inversion with seismic constraint method to the study of the deep crustal structures of the Northwest Brazil passive margins. With a layer-stripping approach, the method has the capacity, robustness and coherency to study the geometry of the Moho discontinuity, or any other crustal layer, within the context of the passive margins environment. The obtained results have sufficient accuracy to distinguish transitions between different domains – continental domain, necking zones and oceanic domain. It is also capable to identify differences within the same domain when analyzing two parallel profiles, for example.Imaging of deep crustal structures with Reverse Time Migration method applied to two Wide-Angle Seismic data profiles, acquired by Ocean Bottom Seismometers and Land Seismic Stations. The method has capacity to image these type of structures in the two domains. The analysis of the two results is an important tool to investigate the shape and geometry of the necking zone even in profiles with asymmetric shooting. It is also shown the essential contribution of the refracted wavefield for its success.Merge of three sub-parallel Wide-Angle Seismic profiles in the Northwest area of Brazil into a unique profile of approximately 1800 km in length, providing an unique perspective on the evolution process of the opening of the South Atlantic Ocean. The merged profile showcases the similarities between the Equatorial and Central margins of the South Atlantic Ocean in spite of the different geodynamic processes and time of opening
Empinotti, Luiz Carlos Lucena. „Arcabouço crustal profundo da parte Centro-Norte da margem de Angola: modelo de afinamento e contato de crostas“. Universidade do Estado do Rio de Janeiro, 2011. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=9471.
Der volle Inhalt der QuelleThe main objectives of this study are to identify features on seismic data that allow (1) the building of a deep crustal framework and of the upper portion of the mantle, in part of the Angolan margin; (2) to compare this framework with the adjacent outcropping basement of the African continent and; (3) to try to fit these results to the published continental breakup models. In order to achieve these objectives, five deep reflection seismic lines (25 km of depth) situated in the in Kwanza and Lower Congo Basins on the passive margin of Angola were interpreted. The features identified on seismic were useful to recognize the tripartite division that caracterize the oceanic crust and in defining the Mohorovicic Discontinuity (that represents the limit between crust and mantle). The seismic interpretation associated with the data obtained from the scientific literature (that provided density values for the packages identified on seismic interpretation) allowed the establishment of a gravity modeling that was compared to the gravity data acquired during the seismic acquisition. The gravity model was useful to validate the seismic interpretation, acting as a quality control of the latter. In case of the gravity anomaly generated by the modeling not being in accordance with the measured anomaly, the seismic interpretation was revised in order to obtain a better adjustment between the modeled and the measured result. This adjustment, however, was always done honoring the reflectors that were clearly positioned on seismic. In addition, the magnetic data acquired on the field was used to help on interpretation. The crustal framework obtained by the methodology described above was compared with the passive margin evolution models found on scientific literature, showing some points in common with the models that postulate the occurrence of exhumed mantle in magma-poor passive margins. The final interpretation of these data showed the existence of a proximal domain characterized by a thick continental crust slightly thinned in contact with a distal domain marked by a hyper-extended continental crust. Oceanwards there is a region where the exhumation of the mantle took place. The passage of the proximal to the distal domain is abrupt, here termed as a Necking Zone. Oceanic crust is identified to the west of exhumed mantle. The comparison of the results obtained in this study with data from the outcropping basement on the African continent suggests a basement control on the vales of continental crust thinning attained under the basins and on the regions of exhumed mantle. Recent works done on the Angolan and Brazilian margins show features similar to the ones identified on this dissertation.
Doody, J. J. „Deep crustal seismic studies of Southwest Britain“. Thesis, Bucks New University, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.356207.
Der volle Inhalt der QuelleBiari, Youssef. „Structure profonde de la marge Nord-Ouest Africaine“. Thesis, Brest, 2015. http://www.theses.fr/2015BRES0080/document.
Der volle Inhalt der QuelleThe NE American margin represents one of the best studied margins in the world, it was the subject of several scientific programs. In comparison, the conjugate NW African margin remains fairly unknown, only two deep seismic cruises were acquired: the SISMAR cruise (2001) offshore the Meseta and the DAKHLA cruise (2002) offshore the Sahara. The deep structure of the Canadian margin is known due to the SMART wide-angle seismic profiles 1, 2 and 3. The first objective of the MIRROR project was to acquire combined wide-angle and deep reflection seismic data offshore a segment conjugate to the SMART-1 profile. The comparison between the homologous segments of these two margins aimed to better understand the opening mechanism of the Central Atlantic Ocean. A comparison between Sismar, Dakhla and Mirror models shows that the continental crust is thicker in the north and thins toward the south. The width of the transition zone is narrower south and Sismar profiles are located on a sedimentary basin placed on a very thinned continental crust. Comparing the Mirror profile with that of the Canadian conjugate margin (Smart 1) shows that the thickness, the structure of the continental crust and the thinning is very similar. However, zones of exhumed and serpentinized mantle were imaged along the Canadian profile that have no conjugate on the African margin. Moreover, the thickness of the oceanic crust is variable with 8 km on the African side and only 3-4 km on the Canadian margin. Several hypotheses have been proposed to explain this difference (a) an age difference between the two types of crust (b) thickening associated with the passage of the Canary hotspot (c) an asymmetric accretion or (d) an accretion at slow to ultra-slow speading centers
Hunter, Richard John. „Deep crustal structure of the central North Sea“. Thesis, Imperial College London, 1991. http://hdl.handle.net/10044/1/46834.
Der volle Inhalt der QuelleMarshall, A. Saskia. „High-silical peralkaline magmatism of the Greater Olkaria Volcanic Complex, Kenya Rift Valley“. Thesis, Lancaster University, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.310585.
Der volle Inhalt der QuelleDilles, 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.
Der volle Inhalt der QuelleReynisson, Reynir Fjalar. „Deep structure and sub-basalt exploration of the mid-Norwegian margin with emphasis on the Møre margin“. Doctoral thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for petroleumsteknologi og anvendt geofysikk, 2010. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-11136.
Der volle Inhalt der QuelleZhang, Sufang. „Deep structure beneath the Central-South Tibet crustal density modelling and azimuthal anisotropy variation inferred from Quasi-Love wases“. Doctoral thesis, Università degli studi di Trieste, 2010. http://hdl.handle.net/10077/3621.
Der volle Inhalt der QuelleThe area of the present study is the central part of southern Tibet. It consists of two accreted terranes, Lhasa and Himalaya terranes, which today record the deformation history that originated from the processes of collision between the Eurasia and India plates. Our study of the crust/mantle structure in terms of seismic velocity, density, anisotropy and petrologic composition are undoubtedly significant to deepen the understanding of the continent-continent collision and its dynamics. This PhD thesis can be briefly summarized into four parts that are listed in the following. 1) In order to reveal the characteristics of the crust/mantle deformation that has been generated by the Indian/Eurasia collision in the southern Tibet plateau, we study the propagation of Quasi-Love (QL) waves. Our study is based on the results from numerical modeling, which proved that QL is sensitive to lateral variation of seismic anisotropy, rather than heterogeneity and other factors. The results we obtain from processing locally observed seismograms, reveal a West-East variation of crust/mantle deformation in each terrane of the plateau. 2) A 3D density model of central-south Tibet is produced by modeling the Bouguer gravity field using all existing constraints. 3) Integrating seismic velocity and density models of the crust in the Lhasa and Himalaya terranes, we infer crustal composition models in central and southern Tibet. 4) Combining crustal density, velocity and mineralogical composition models, some important issues, such as the Indian slab subduction angle, and the relationship between crustal density and earthquake occurrences are discussed. Some results based on the gravity modeling are summarized as follows: 1) under the constraint of the geometrical structure defined by seismic data, a 3-D density model and Moho interface are proposed for central-south Tibet; 2) the lower crustal density, smaller than 3.2 g/cm3, suggests the absence of eclogite or partial eclogitization due to delamination under the central-south Tibet; 3) seismicity is strong or weak in correspondence of the most negative Bouguer gravity anomaly, so there is not a relationship between them; 4) the composition of the lower crust, determined after the temperature-pressure calibration of seismic P wave velocity, might be one or a mixture of: 1. amphibolite and greenschist facies basalt beneath the Qiangtang terrane; 2. gabbro-norite-troctolite and mafic granulite beneath the Lhasa terrane. When using the data set published by Rudnick & Fountain (1995), the composition of the middle crust turns out to be granulite facies and might be pelitic gneisses. Granulite facies used to be interpreted as residues of partial melting, which coincides with the previous study by Yang et al. (2002) on partial melting in the middle crust. Amphibolite facies are thought to be produced after delamination, when underplating works in the rebound of the lower crust and lithospheric mantle. From the seismology study, I have made the following conclusions: 1) through numerical simulation of surface wave propagation in heterogeneous media, we find that amplitude and polarization of surface wave only change a little when considering heterogeneity and QL waves, generated by surface wave scattering, are caused by lateral variation of anisotropy. 2) QL waves have been identified from the seismograms of selected paths recorded by the Tibetan station CAD, and are utilized to determine the variation of the uppermost mantle anisotropy of the Tibetan plateau. The location of the azimuthal anisotropy gradient is estimated from the group velocities of Rayleigh wave, Love wave and QL wave. We find that a predominant south-north lateral variation of azimuthal anisotropy is located in correspondence of the Tanggula mountain, and a predominant east-west lateral variation of azimuthal anisotropy is found to the north of the Gandese mountain (near 85°E longitude and 30°N latitude) and near the Jinsha river fault (near 85°E longitude and 35°N latitude).
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Bücher zum Thema "Deep crustal structures"
Naidu, G. Dhanunjaya. Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-28442-7.
Der volle Inhalt der QuelleNaidu, G. Dhanunjaya. Deep crustal structure of the Son-Narmada-Tapti Lineament, central India. Berlin: Springer, 2012.
Den vollen Inhalt der Quelle findenNaidu, G. Dhanunjaya. Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012.
Den vollen Inhalt der Quelle findenMint︠s︡, M. V. East European craton: Early Precambrian history and 3D models of deep crustal structure. Boulder, Colorado, USA: The Geological Society of America, 2015.
Den vollen Inhalt der Quelle findenW, Hillhouse John, und International Union of Geodesy and Geophysics. General Assembly, Hrsg. Deep structure and past kinematics of accreted terranes. Washington, DC: International Union of Geodesy and Geophysics, 1989.
Den vollen Inhalt der Quelle findenHilst, Robert Dirk van der, 1961-, McDonough W. F und International Symposium on Deep Structure, Composition, and Evolution of Continents (1997 : Cambridge, Mass.), Hrsg. Composition, deep structure, and evolution of continents. Amsterdam: Elsevier Science, 1999.
Den vollen Inhalt der Quelle findenInternational Symposium on Deep Seismic Sounding Traverses (1985 Bhubaneswar, India). Deep seismic soundings and crustal tectonics: Proceedings of International Symposium on Deep Seismic Sounding Traverses, November 22-24, Bhubaneswar, India. Herausgegeben von Kaila K. L, Tewari H. C und Association of Exploration Geophysicists. Hyderabad, India: Association of Exploration Geophysicists, 1986.
Den vollen Inhalt der Quelle findenInternational Symposium on Deep Seismic Sounding Traverses (1985 Bhubaneswar, India). Deep seismic soundings and crustal tectonics: Proceedings of International Symposium on Deep Seismic Soundings Traverses, Nov. 22-24, Bhubaneswar, India. Herausgegeben von Kaila K. L und Tewari H. C. Hyderabad: Assoaciation of Exploration Geophysicists, 1985.
Den vollen Inhalt der Quelle findenD, Ashwal Lewis, und United States. National Aeronautics and Space Administration., Hrsg. Workshop on the Deep Continental Crust of South India. Houston, Tex: Lunar and Planetary Institute, 1988.
Den vollen Inhalt der Quelle findenD, Ashwal Lewis, und United States. National Aeronautics and Space Administration, Hrsg. Workshop on the Deep Continental Crust of South India. Houston, Tex: Lunar and Planetary Institute, 1988.
Den vollen Inhalt der Quelle findenBuchteile zum Thema "Deep crustal structures"
Basheer, Alhussein Adham. „Deep Crustal and Upper Mantle Structures in North Africa: A Review“. In Regional Geology Reviews, 21–45. Cham: Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-48299-1_2.
Der volle Inhalt der QuelleMyers, John S. „Tectonic evolution of deep crustal structures in the mid-Proterozoic Albany-Fraser Orogen, Western Australia“. In Evolution of Geological Structures in Micro- to Macro-scales, 473–85. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5870-1_26.
Der volle Inhalt der QuelleRuditch, E. M. „On the Relationship of Deep Earthquakes of Eastern Outlying Districts of Asia with Large Crustal Structures“. In Geophysical Monograph Series, 52–59. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm006p0052.
Der volle Inhalt der QuelleWagner, J. J., R. Chessex, S. Sellami und F. Barblan. „Laboratory density and seismic properties of Alpine crustal rocks“. In Deep Structure of the Swiss Alps, 39–44. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_6.
Der volle Inhalt der QuelleWever, Thomas, und Petra Sadowiak. „Crustal suture zones: Seismic signature and structural interpretation“. In Continental Lithosphere: Deep Seismic Reflections, 371–75. Washington, D. C.: American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0371.
Der volle Inhalt der QuelleMarchant, R. H., und G. M. Stampfli. „Crustal and lithospheric structure of the Western Alps: geodynamic significance“. In Deep Structure of the Swiss Alps, 326–37. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_24.
Der volle Inhalt der QuelleWeber, Klaus, und Axel Vollbrecht. „The Crustal Structure at the KTB Drill Site, Oberpfalz“. In Exploration of the Deep Continental Crust, 5–36. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-74588-1_2.
Der volle Inhalt der QuelleLund, C. E., R. G. Roberts, T. Dahl-Jensen und J. Lindgren. „Deep Crustal Structure in the Vicinity of the Siljan Ring“. In Deep Drilling in Crystalline Bedrock, 355–64. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73452-6_29.
Der volle Inhalt der QuelleKahle, H. G., A. Geiger, B. Bürki, E. Gubler, U. Marti, B. Wirth, M. Rothacher et al. „Recent crustal movements, geoid and density distribution: Contribution from integrated satellite and terrestrial measurements“. In Deep Structure of the Swiss Alps, 251–59. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_19.
Der volle Inhalt der QuelleBlundell, D. J., T. J. Reston und A. M. Stein. „Deep Crustal Structural Controls on Sedimentary Basin Geometry“. In Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources, 57–64. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm048p0057.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Deep crustal structures"
Schmidt, J., D. Dyrelius, H. Palm, A. Egorkin, N. Yasulievich und Y. Zolotov. „The Cables Project - Imaging Deep Crustal Structures in the Central Scandinavian Caledonides“. In 61st EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609.201407737.
Der volle Inhalt der QuelleShiraishi, Kazuya, und Toshiki Watanabe. „Seismic imaging of deep crustal structures via reverse time migration using local earthquakes“. In The 14th SEGJ International Symposium, Online, 18–21 October 2021. Society of Exploration Geophysicists and Society of Exploration Geophysicists of Japan, 2021. http://dx.doi.org/10.1190/segj2021-069.1.
Der volle Inhalt der QuelleOrmeni, R. „Crustal Structures Beneath Seismogenetic Zones and Lateral Velocity Contrasts Across Deep Faults of Albania“. In 5th Congress of Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.126.6243.
Der volle Inhalt der QuelleLouie, John N., und Robert W. Clayton. „The nature of deep crustal structures in the Mojave desert, California, from multioffset reflections“. In SEG Technical Program Expanded Abstracts 1986. Society of Exploration Geophysicists, 1986. http://dx.doi.org/10.1190/1.1893032.
Der volle Inhalt der QuelleAntal Lundin, A., M. Bastani, S. Wang und J. Jönberger. „Imaging Deep Crustal Structures and Mineralised Zones by 3D Modeling of Potential Field and Magnetotelluric Data - Example“. In Near Surface Geoscience 2016 - First Conference on Geophysics for Mineral Exploration and Mining. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201602131.
Der volle Inhalt der Quelle-M. Marthelot, J., M. Diagnieres, A. Hirn, A. Paul, D. Rapping, R. Silioi, B. Damotte et al. „The ecors 2.5D experiment: an attempt to image deep crustal structures with a sparse 3D recording geometry“. In 54th EAEG Meeting. European Association of Geoscientists & Engineers, 1992. http://dx.doi.org/10.3997/2214-4609.201410364.
Der volle Inhalt der QuelleRussell, Michael J. „On Irish bacteriometallogenesis and its wider connotations“. In Irish-type Zn-Pb deposits around the world. Irish Association for Economic Geology, 2023. http://dx.doi.org/10.61153/pbic1076.
Der volle Inhalt der QuelleZhou, Lingli, Yi Zheng, Xlaoxia Duan, Yumlao Meng, Peng-peng Yu, Zhanke Li, Suofei Xiong, Fan Xiao, Yongbin Wang und Jiaxi Zhou. „Carbonate-hosted Pb-Zn deposits in China: a review of the geological characteristics and genesis“. In Irish-type Zn-Pb deposits around the world. Irish Association for Economic Geology, 2023. http://dx.doi.org/10.61153/eyly2924.
Der volle Inhalt der QuelleKeller, G. A., und G. A. McMechan. „Seismic studies of deep crustal structure in Southwestern Oklahoma“. In 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892547.
Der volle Inhalt der QuelleAziz, Fawwaz, Roger Miller und Carlos Giraldo. „Improving deep crustal structure depth interpretation by integrating 2D gravity-magnetic modelling and structural restoration: Offshore Borneo“. In SEG Technical Program Expanded Abstracts 2019. Society of Exploration Geophysicists, 2019. http://dx.doi.org/10.1190/segam2019-3215966.1.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Deep crustal structures"
Harris, L. B., P. Adiban und 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.
Der volle Inhalt der QuelleDafoe, L. T., K. Dickie und G. L. Williams. Stratigraphy of western Baffin Bay: a review of existing knowledge and some new insights. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321846.
Der volle Inhalt der Quellede Kemp, E. A., H. A. J. Russell, B. Brodaric, D. B. Snyder, M. J. Hillier, M. St-Onge, C. Harrison et al. Initiating transformative geoscience practice at the Geological Survey of Canada: Canada in 3D. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331097.
Der volle Inhalt der Quellede Kemp, E. A., H. A. J. Russell, B. Brodaric, D. B. Snyder, M. J. Hillier, M. St-Onge, C. Harrison et al. Initiating transformative geoscience practice at the Geological Survey of Canada: Canada in 3D. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331871.
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