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Auswahl der wissenschaftlichen Literatur zum Thema „Geology“
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Zeitschriftenartikel zum Thema "Geology"
Gonçalves, Pedro Wagner, Heitor Assis Junior, Marcelo Luis de Brino und Celso Dal Ré Carneiro. „Da Mineralogia à Geologia: quarenta anos que mudaram a ciência no Brasil (1876-1918)“. História da Ciência e Ensino: construindo interfaces 27 (05.01.2024): 124–41. http://dx.doi.org/10.23925/2178-2911.2023v27espp124-141.
Der volle Inhalt der QuelleRoemmele, Christopher. „The Impact of Curriculum and Instructional Choices on Undergraduate Students in Introductory Geology“. International Research in Higher Education 4, Nr. 3 (19.08.2019): 17. http://dx.doi.org/10.5430/irhe.v4n3p17.
Der volle Inhalt der QuelleLi, Yaoguo, Aline Melo, Cericia Martinez und Jiajia Sun. „Geology differentiation: A new frontier in quantitative geophysical interpretation in mineral exploration“. Leading Edge 38, Nr. 1 (Januar 2019): 60–66. http://dx.doi.org/10.1190/tle38010060.1.
Der volle Inhalt der QuelleAdhitya, Bagus, Hari Wiki Utama, Anggi Deliana Siregar, Magdalena Ritonga und Yulia Morsa Said. „Pembuatan maket geologi struktur sebagai bahan ajar di Jurusan Teknik Kebumian Fakultas Sains dan Teknologi Universitas Jambi“. Transformasi: Jurnal Pengabdian Masyarakat 17, Nr. 2 (31.12.2021): 279–86. http://dx.doi.org/10.20414/transformasi.v17i2.4020.
Der volle Inhalt der QuelleSun, Jiajia, Aline Tavares Melo, Jae Deok Kim und Xiaolong Wei. „Unveiling the 3D undercover structure of a Precambrian intrusive complex by integrating airborne magnetic and gravity gradient data into 3D quasi-geology model building“. Interpretation 8, Nr. 4 (23.07.2020): SS15—SS29. http://dx.doi.org/10.1190/int-2019-0273.1.
Der volle Inhalt der QuelleBathrellos, G. D. „An overview in urban geology and urban geomorphology“. Bulletin of the Geological Society of Greece 40, Nr. 3 (05.06.2018): 1354. http://dx.doi.org/10.12681/bgsg.16888.
Der volle Inhalt der QuelleYoung, Davis A. „The Biblical Flood as a Geological Agent: A Review of Theories“. Paleontological Society Papers 5 (Oktober 1999): 119–34. http://dx.doi.org/10.1017/s1089332600000565.
Der volle Inhalt der QuelleOsipov, V. I. „About fundamental losses in engineering geology“. Геоэкология. Инженерная геология. Гидрогеология. Геокриология, Nr. 5 (20.09.2019): 89–91. http://dx.doi.org/10.31857/s0869-78092019589-91.
Der volle Inhalt der QuelleGanguly, Pekham. „Medical Geology Related to Different Trace Elements Deficiency and Toxicity Diseases“. International Journal for Research in Applied Science and Engineering Technology 11, Nr. 9 (30.09.2023): 113–27. http://dx.doi.org/10.22214/ijraset.2023.55616.
Der volle Inhalt der Quellede Mendonça Figueirôa, Silvia Fernanda. „Brazilian geology for Brazilian students: The general geology textbook published by John Casper Branner in 1906“. Earth Sciences History 35, Nr. 2 (01.01.2016): 375–86. http://dx.doi.org/10.17704/1944-6178-35.2.375.
Der volle Inhalt der QuelleDissertationen zum Thema "Geology"
Lund, Cecilia. „Mineralogical, chemical and textural characterisation of the Malmberget iron ore deposit for a geometallurgical model“. Doctoral thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-16819.
Der volle Inhalt der QuelleGodkänd; 2013; 20130422 (luncec); Tillkännagivande disputation 2013-08-13 Nedanstående person kommer att disputera för avläggande av teknologie doktorsexamen. Namn: Cecilia Lund Ämne: Malmgeologi/Ore Geology Avhandling: Mineralogical, Chemical and Textural Characterisation of the Malmberget Iron Ore Deposit for a Geometallurgical Model Opponent: Professor emeritus Terje Malvik, Department of Geology and Mineral resources Engineering, NTNU, Trondheim, Norway Ordförande: Professor Pertti Lamberg, Institutionen för samhällsbyggnad och naturresurser, Luleå tekniska universitet Tid: Fredag den 6 september 2013, kl 10.00 Plats: F531, Luleå tekniska universitet
Edfelt, Åsa. „Geology, alterations and mineral chemistry of the Tjårrojåkka Fe-oxide Cu-Au occurrences, northern Sweden“. Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2003. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26616.
Der volle Inhalt der QuelleGodkänd; 2003; 20070215 (ysko)
Kampmann, Tobias Christoph. „3D structural framework and constraints on the timing of hydrothermal alteration and ore formation at the Falun Zn-Pb-Cu-(Au-Ag) sulphide deposit, Bergslagen, Sweden“. Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26483.
Der volle Inhalt der QuelleThe Falun pyritic Zn-Pb-Cu-(Au-Ag) sulphide deposit, situated in the Palaeoproterozoic (1.9–1.8 Ga) Bergslagen lithotectonic unit in the south-western part of the Fennoscandian Shield, is one of the major base and minor precious metal sulphide deposits in Sweden. Host rocks to the deposit as well as the ores and altered rocks were metamorphosed and affected by heterogeneous ductile strain during the Svecokarelian orogeny (2.0–1.8 Ga). These processes both reworked the mineral assemblages of the original hydrothermal alteration system and reshaped the structural geometry of the deposit, following formation of the ores and the associated hydrothermal alteration.In order to study primary geological and ore-forming processes at Falun, it is necessary firstly to investigate the nature of the strong tectonothermal modification. In this licentiate thesis, a three-dimensional modelling approach is used in order to evaluate geometric relationships between lithologies at the deposit. This study demonstrates the polyphase character (D1 and D2) of the ductile deformation at Falun. The major rock-forming minerals in the silicate alteration rocks are quartz, biotite/phlogopite, cordierite, anthophyllite, chlorite, and minor almandine and andalusite. On the basis of microstructural investigations, it is evident that these minerals grew during distinct periods in the course of the tectonic evolution, with major static grain growth between D1 and D2, and also after D2. Furthermore, the occurrence of F2 sheath folds along steeply south-south-east plunging axes is suggested as a key deformation mechanism, forming cylindrical, rod-shaped ore bodies which pinch out at depth. The sheath folding also accounts for the same stratigraphic level on both the eastern and western sides of the massive sulphide ores. A major, sulphide-bearing high-strain zone defines a tectonic boundary inside the deposit and bounds the massive sulphide ores to the north. A precursor to this zone can have played a central role as a metal-bearing fluid conduit during ore genesis, prior to reactivation of the zone in the ductile regime.The geological evolution in the Falun area involved emplacement of felsic volcanic and sub-volcanic rocks and some carbonate sedimentation, followed by ore formation and hydrothermal alteration as well as the intrusion of dykes and plutons of variable composition. U-Pb zircon geochronology of key lithologies in and around the Falun base metal sulphide deposit indicates a rapid sequence of development of different magmatic phases with individual age determinations overlapping within their uncertainties. The igneous activity is constrained between a zircon U-Pb concordia age of 1899 ± 7 Ma for a sub-volcanic host rock and a zircon 207Pb-206Pb weighted average age of 1891 ± 3 Ma for a felsic dyke, with all other reliable ages, including the quartz-rich plutonic rocks, falling in the interval between them. This interval also included the hydrothermal alteration and ore formation at Falun.It is suggested that the bowl-shaped, sub-seafloor feeder part of a high-sulphidation and Au-bearing volcanogenic massive sulphide ore system, with replacement of carbonates and (sub)-volcanic rocks, served as an initial inhomogeneity in the strata for the later development of strong stretching along steep axes and sheath fold formation during ductile strain. The observation of discordant relationships along the margins of the massive sulphide ores, coupled with the syn-magmatic, pre-tectonic timing of ore formation, corroborate this hypothesis, providing a compromise solution to the previous debate around two opposing models of strictly syn-genetic vs. epigenetic, post-deformational carbonate-replacement processes of ore formation at the Falun base metal sulphide deposit.
Godkänd; 2015; 20150212 (tobkam); Nedanstående person kommer att hålla licentiatseminarium för avläggande av teknologie licentiatexamen. Namn: Tobias Christoph Kampmann Ämne: Malmgeologi/Ore Geology Uppsats: 3D Structural Framework and Constraints on the Timing of Hudrothermal Alteration and Ore Formation at the Falun Zn-Pb-Cu-(Au-Ag) Sulphide Deposit, Bergslagen, Sweden Examinator: Professor Pär Weihed Institutionen för samhällsbyggnad och naturresurser, Avdelning Geovetenskap och miljöteknik, Luleå tekniska universitet Diskutant: Docent, adjungerad professor Pietari Skyttä, University of Turku, Department of Geography and Geology, Turun Yliopisto, Finland Tid: Torsdag 23 april 2015 kl 10.00 Plats: F531, Luleå tekniska universitet
Structural evolution, hydrothermal alteration and tectonic setting of the Falun base metal and gold deposit, Bergslagen region, Sweden
Bauer, Tobias. „Structural and sedimentological reconstruction of the inverted Vargfors basin : a base for 4D-modelling“. Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-17596.
Der volle Inhalt der QuelleGodkänd; 2010; 20101029 (tobbau); LICENTIATSEMINARIUM Ämnesområde: Malmgeologi/Ore Geology Examinator: Professor Pär Weihed, Luleå tekniska universitet Diskutant: Dr Peter Sorjonen-Ward, GTK, Kuopio, Finland Tid: Torsdag den 16 december 2010 kl 10.00 Plats: F531, Luleå tekniska universitet
Bark, Glenn. „Genesis and tectonic setting of the hypozonal Fäboliden orogenic gold deposit, northern Sweden“. Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-17200.
Der volle Inhalt der QuelleGodkänd; 2005; 20061214 (haneit)
Martinsson, Olof. „Bispbergs järnmalmsfält : En geologisk och geokemisk studie“. Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 1987. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26303.
Der volle Inhalt der QuelleAmoorizi, Varnamkhasti Kianoosh. „Competitive Business framework design toward the circular economy“. Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-86977.
Der volle Inhalt der QuelleTollefsen, Elin. „Chemical controls on ikaite formation“. Licentiate thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-156839.
Der volle Inhalt der QuelleMoberg, Jesper. „Naturliga halter av metaller i sjöar och vattendrag med avseende på lokal geologi i Barseleområdet“. Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-353770.
Der volle Inhalt der QuelleThe levels of metals measured in individual Swedish lakes and waterways (local scale) do not always correspond to levels expected from knowledge of the underlying geology (regional scale), and in some cases can be orders of magnitude higher than expected. This is the case in the Barsele area, northern Sweden, where Agnico Eagle are exploring for gold. The purpose of this work is to investigate the natural levels of metals in waters with regard to local geology in the area, and compare these with calculated background levels. The study focuses on the metals arsenic, antimony, lead and zinc, and their geochemical behavior. Water data from ten sites during 2001–2016 have been studied. The analyzes were carried out with V2 analyzing package. Background levels were obtained from SLU and Sweden's environmental institute, which have been compared with water data from the area. The results show that arsenic and antimony have consistently higher levels than calculated background levels, while levels of lead and zinc generally correspond to background levels, depending on the classification of the water. Factors such as pH, hydrological conditions, and solubility and mobility in water have a major influence on whether or not the levels of metals exceed the calculated background levels. Adsorption to iron oxides is an example of a factor that decreases the mobility of metals in water.
Sarlus, Zimer. „Geochemical and geochronological constraints on 1.88 and 1.80 Ga magmatic events in the Gällivare area, northern Sweden“. Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-25689.
Der volle Inhalt der QuelleThe Gällivare area is situated in northern Norrbotten, Sweden, and hosts the Aitik Cu-Au deposit and the Malmberget Fe deposit. In addition, more than 17 mineral prospects and mineralizations are present, among these the currently developed Nautanen Cu-Au deposit. All deposits are hosted within Paleoproterozoic volcanic and volcano-sedimentary successions intruded and surrounded by multiple generations of intrusive suites, including large bodies of ultramafic to mafic layered complexes. Detailed field mapping combined with geochemical and petrological investigations and geochronology have revealed the role of intrusive igneous events and their control on ore formation. Main key igneous rocks include 1) tholeiitic, ultramafic-mafic layered intrusive complexes; 2) calc-alkaline mafic to intermediate plutonic and volcanic units; 3) calc-alkaline, mafic-intermediate dykes and sills; 4) calc-alkaline and shoshonitic granitoids. U-Pb multigrain zircon SIMS analysis combined with litho-geochemical investigations suggest two magmatic episodes at 1.88 and 1.80 Ga, respectively, with coeval mafic-felsic magmatism including the generation of voluminous layered complexes. Based on their MORB-type, tholeiitic character, these layered complexes are suggested to have formed in an extensional setting, preferentially in a back-arc environment. U-Pb multigrain zircon SIMS analysis and field mapping also reveal that granitoids in the area range from 1886 to 1779 Ma with the oldest granitoids containing mafic enclaves. This suggests magma interaction between basic and felsic magma sources. Geochemical data suggest generation of granitoids in a volcanic arc environment in a mainly post-collisional setting. Results suggest the formation of layered complexes and a volcanic arc system in an extensional setting followed by a subsequent compressional phase of arc accretion producing post-collisional granitoids. The 1.88 Ga event that generated the ultramafic-mafic layered complexes is is associated with a back-arc setting generated in response to 1.90 Ga NNE trending subduction. The later event at ~1.80 Ga generating voluminous mafic-felsic units is associated with the TIB event also coupled to the regional IOCG overprint.
Godkänd; 2016; 20160518 (zimsar); Nedanstående person kommer att hålla licentiatseminarium för avläggande av teknologie licentiatexamen. Namn: Zmar Sarlus Ämne: Malmgeologi /Ore Geology Uppsats: Geochemical and Geochronological Constraints on 1.88 and 1.80 Ga Magmatic Events in the Gällivare Area, Northern Sweden Examinator: Biträdande professor Christina Wanhainen, Institutionen för samhällsbyggnad och naturresurser, Avdelning: Geovetenskap och miljöteknik, Luleå tekniska universitet. Diskutant: PhD Paul Evins, WSP Sverige AB, Stockholm. Tid: Fredag 17 juni, 2016 kl 10.00 Plats: F341, Luleå tekniska universitet
Bücher zum Thema "Geology"
Efrén, Pérez Segura, und Jacques-Ayala César 1946-, Hrsg. Studies of Sonoran geology. Boulder, Colo: Geological Society of America, 1991.
Den vollen Inhalt der Quelle findenMcLean, A. C. Geology for civil engineers. 2. Aufl. London: Unwin Hyman, 1985.
Den vollen Inhalt der Quelle finden1906-, Hunt Charles Butler, Hrsg. Geology of the Henry Mountains, Utah, as recorded in the notebooks of G.K. Gilbert, 1875-76. Boulder, Colo: Geological Society of America, 1988.
Den vollen Inhalt der Quelle findenGeological Survey (U.S.), Hrsg. Geologic hazards: Geology and resources. Denver, CO (P.O. Box 25286, Denver 80225): U.S. Dept. of the Interior, U.S. Geological Survey, 1996.
Den vollen Inhalt der Quelle findenZvi, Baras, Batzhargal T und Sengee Doobatyn, Hrsg. Mongġol geologi =: Mongolian geology = Mongolʹskai︠a︡ geologi︠a︡. Ulaanbaatar: Ulsyn Khėvlėliĭn Gazar, 1989.
Den vollen Inhalt der Quelle findenDoelling, Hellmut H. The geololgy of Kane County, Utah: Geology, mineral resources, geologic hazards. Salt Lake City, Utah (606 Black Hawk Way, Salt Lake City 84108-1280): Utah Geological and Mineral Survey, Utah Dept. of Natural Resources, 1989.
Den vollen Inhalt der Quelle finden1949-, Sherwood Kirk W., Johnson Peter P und United States. Minerals Management Service. Alaska OCS Region., Hrsg. Geologic report for the Beaufort Sea planning area, Alaska: Regional geology, petroleum geology, environmental geology. Anchorage, Alaska: U.S. Dept. of Interior, Minerals Management Service, Alaska OCS Region, 1986.
Den vollen Inhalt der Quelle findenCraig, James D. Geologic report for the Beaufort Sea planning area, Alaska: Regional geology, petroleum geology, environmental geology. Anchorage, Alaska: U.S. Dept. of Interior, Minerals Management Service, Alaska OCS Region, 1986.
Den vollen Inhalt der Quelle findenCraig, James D. Geologic report for the Beaufort Sea planning area, Alaska: Regional geology, petroleum geology, environmental geology. Anchorage, Alaska: U.S. Dept. of Interior, Minerals Management Service, Alaska OCS Region, 1986.
Den vollen Inhalt der Quelle findenCraig, James D. Geologic report for the Beaufort Sea planning area, Alaska: Regional geology, petroleum geology, environmental geology. Anchorage, Alaska: U.S. Dept. of Interior, Minerals Management Service, Alaska OCS Region, 1986.
Den vollen Inhalt der Quelle findenBuchteile zum Thema "Geology"
Brawer, Moshe. „Geology“. In Atlas of South America, 14–15. London: Palgrave Macmillan UK, 1991. http://dx.doi.org/10.1007/978-1-349-12579-1_5.
Der volle Inhalt der QuelleMarker, Brian R. „Geology“. In Selective Neck Dissection for Oral Cancer, 1–2. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-12127-7_136-1.
Der volle Inhalt der QuelleBrown, Gary, und Bruno A. Mies. „Geology“. In Vegetation Ecology of Socotra, 21–31. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4141-6_3.
Der volle Inhalt der QuelleArnalds, Olafur. „Geology“. In World Soils Book Series, 17–34. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9621-7_3.
Der volle Inhalt der QuelleBondyrev, Igor V., Zurab V. Davitashvili und Vijay P. Singh. „Geology“. In World Regional Geography Book Series, 67–80. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-05413-1_7.
Der volle Inhalt der QuelleOstadhassan, Mehdi, Kouqi Liu, Chunxiao Li und Seyedalireza Khatibi. „Geology“. In SpringerBriefs in Petroleum Geoscience & Engineering, 1–16. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-76087-2_1.
Der volle Inhalt der QuelleNitecki, Matthew H., Harry Mutvei und Doris V. Nitecki. „Geology“. In Receptaculitids, 31–52. Boston, MA: Springer US, 1999. http://dx.doi.org/10.1007/978-1-4615-4691-7_3.
Der volle Inhalt der QuelleElbasiouny, Heba, und Fathy Elbehiry. „Geology“. In World Soils Book Series, 93–109. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-95516-2_6.
Der volle Inhalt der QuelleArnold, Arthur B., Laurence B. James, George A. Kiersch und Alan L. O’Neill. „Geology“. In Advanced Dam Engineering for Design, Construction, and Rehabilitation, 106–52. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4613-0857-7_4.
Der volle Inhalt der QuelleWhittaker, Alun. „Geology“. In Theory and Evaluation of Formation Pressures, 11–42. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5355-0_2.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Geology"
Allmendinger, Richard W., und Paul Karabinos. „IMPROVING GEOLOGIC MAPPING WITH COMPUTATIONAL FIELD GEOLOGY“. In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334376.
Der volle Inhalt der QuelleGentile, Richard J., und Robyn L. Daniels. „THE TRAVELING GEOLOGY EXHIBIT - BRINGING GEOLOGY TO THE PEOPLE“. In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-326265.
Der volle Inhalt der QuelleWeisenfluh, Gerald A., Stephen F. Greb und Rebecca Wang. „COAL GEOLOGY INFORMATION: COAL CORE DESCRIPTION AND MINING GEOLOGY“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304493.
Der volle Inhalt der QuelleStephenson, M., F. Bullough, S. Geiger, M. Bridden, P. Ringrose, D. Schofield und R. Davey. „Geology of Decarbonisation“. In 81st EAGE Conference and Exhibition 2019. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201900931.
Der volle Inhalt der QuelleGusev, Vladimir V. „GEOLOGY AND SOCIETY“. In Treshnikov readings – 2021 Modern geographical global picture and technology of geographic education. Ulyanovsk State Pedagogical University named after I. N. Ulyanov, 2021. http://dx.doi.org/10.33065/978-5-907216-08-2-2021-251-252.
Der volle Inhalt der QuelleBubniak, I. M., A. M. Bubniak und O. D. Gavrilenko. „Digital field geology“. In Geoinformatics: Theoretical and Applied Aspects 2020. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.2020geo087.
Der volle Inhalt der QuelleClary, Renee, Athena M. Owen und Eric Shows. „GEOLOGY AROUND ME: LEVERAGING LOCAL ENVIRONMENTS IN ONLINE INTRODUCTORY GEOLOGY COURSES“. In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358064.
Der volle Inhalt der QuelleSellers, Victoria, Stephen M. Moysey, Kelly Best Lazar und Lisa Benson. „CHANGES IN GEOLOGY INTEREST AFTER A VIRTUAL REALITY GEOLOGY FIELD EXPERIENCE“. In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338616.
Der volle Inhalt der QuelleE. Campbell, A., B. C. Scheffers und P. F. M. de Groot. „Geophysics - Desperately seeking geology“. In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201410261.
Der volle Inhalt der QuelleLuh, P. C., F. G. Sherrill und N. L. Carayannopoulos. „Paleodatuming for complex geology“. In 1985 SEG Technical Program Expanded Abstracts. SEG, 1985. http://dx.doi.org/10.1190/1.1892826.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Geology"
Kerr, D. E., A. Plouffe, J. E. Campbell und I. McMartin. Status of surficial geology mapping in the North. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330334.
Der volle Inhalt der QuelleKerr, D. E., A. Plouffe, J E Campbell und I. McMartin. Status of surficial geology mapping in northern Canada. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331420.
Der volle Inhalt der QuelleSanford, B. V., G. B. J. Fader und P. N. Moir. Regional geology and geophysics 8: bedrock geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210609.
Der volle Inhalt der QuelleYorath, C. J., D. K. Norris und F. G. Young. Regional Geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/126948.
Der volle Inhalt der QuelleMayr, U., T. de Freitas und B. Beauchamp. Regional geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209769.
Der volle Inhalt der QuelleEisbacher, G. H. Structural geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209775.
Der volle Inhalt der Quellemayr, U., T. de Freitas und B. Beauchamp. Economic geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209776.
Der volle Inhalt der QuelleDallimore, S. R., und J. S. Vincent. Onshore Geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132218.
Der volle Inhalt der QuelleBlasco, S. M., und J. F. Lewis. Offshore Geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132219.
Der volle Inhalt der QuelleHamblin, A. P. Bedrock geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/298874.
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