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Thèses sur le sujet « Geology »

Auteur : Grafiati

Publié le 4 juin 2021

Mis à jour le 25 juillet 2025

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1

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.

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The northern Norrbotten ore province is an intensely mineralised area and has traditionally been a very important mining district. It contains Fe, Cu-Au, Au, and Ag deposits ranging from world-class ore deposits to small and uneconomic ones (Martinsson 2004). The most important are the Kiruna and Malmberget iron ores and the Aitik Cu-Au deposit.The cross-discipline approach called geometallurgy connects two different but closely related areas in the mining industry, namely geology and mineral processing. It involves understanding and measurements of the ore properties significant for its succe

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2

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.

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The Tjårrojåkka area is located about 50 km WSW of Kiruna, northern Sweden, and hosts one of the best examples of spatially related Fe-oxide Cu-Au occurrences (the Tjårrojåkka-Fe and Tjårrojåkka-Cu). The bedrock, depositional environment and tectonic evolution of the area were studied through petrological, geochemical and geophysical-petrophysical investigations. The bedrock is dominated by intermediate and basic extrusive and intrusive rocks. The intermediate andesites and basaltic andesites are cut by diabases which acted as feeder dykes for the overlying basalts. The intrusive rocks range f

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3

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.

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The 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 the total duration of which was 2.0–1.8 Ga. These processes both reworked the mineral assemblages of the original hydrothermal alteration system and reshaped the structural ge

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4

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.

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The Palaeoproterozoic Skellefte mining district in northern Sweden covers an area of 120 by 30 km and is one of the most important mining districts in Europe, producing mainly Zn, Cu, Pb, As and Au from volcanogenic massive sulfide (VMS) and orogenic gold deposits.Detailed mapping of structures and stratigraphy within the sedimentary Vargfors Group combined with a structural analysis revealed a syn-extensional fault pattern of NW-SE-trending normal faults and associated NE-SW-trending transfer faults, creating the segmented sedimentary Vargfors basin. It comprises distinct fault-bound compartm

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5

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.

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The well-known Skellefte Ore District, northern Sweden, hosts a large number of massive sulphide deposits, a few porphyry-type-deposits and a number of gold deposits in different geological settings. Southwest of this district a new ore province, the so called Gold Line, is presently being uncovered. During the past decade a number of gold occurrences have been discovered in this area. Only one deposit is in production, the Svartliden gold deposit (2 Mton at 4.3 ppm Au). However, with regards to tonnage the Fäboliden gold deposit stands out with a known mineral resource of c. 16 Mton with 1.33

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6

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.

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7

Amoorizi, 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.

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Tollefsen, 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.

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9

Moberg, 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.

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Bakgrundshalter för olika metaller i svenska sjöar och vattendrag stämmer inte alltid överens med geologin i lokala områden, som kan ha anrikats många gånger högre än beräknade halter i jordskorpan. Detta är fallet i Barseleområdet, norra Sverige där Agnico Eagle genomför undersökningsarbeten med fokus på guld. Syftet med arbetet är att undersöka vad som anses vara naturliga halter av metaller i området med avseende på lokal geologi och jämföra dessa med bedömda bakgrundshalter. Fokus ligger på metallerna arsenik, antimon, bly och zink där även dess geokemiska beteende undersöks. Vattendata fr

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10

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.

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The 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 reve

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11

Mattsson, Tobias. "En petrologisk studie av lavor och en mantelxenolit från Fogo, Kap Verde." Thesis, Uppsala universitet, Berggrundsgeologi, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-185139.

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Alla Kap Verdes öar är av vulkaniskt ursprung. Fogo är den enda ön i Kap Verdes arkipelag som fortfarande är vulkaniskt aktiv, med 30 registrerade utbrott sedan människor bosatte sig på ön för cirka 500 år sedan. Detta gör Fogo till en av de mest aktiva vulkanerna på jorden. Fogos lavor är viktiga att studera för att få en förståelse för vulkanens magmasystem och förhindra framtida katastrofer. Lavorna är mörka och innehåller mycket fenokryster utav olivin och clinopyroxen, och i enstaka prover hittas apatit (inneslutningar i pyroxener) och amfibol. Den petrografiska undersökningen tyder på at

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12

Oxenstierna, Johan. "Remote Sensing and Statistical Analysis of Fracture Populations Around Lake Thingvallavatn, SW Iceland." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-182201.

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This study aims at a description and statistical analysis of tectonic and magmatic fractures in the Western Volcanic Zone (WVZ) on Iceland. Two fracture populations are studied with respect to their distance to the Hengill volcano: The southern area is between 0-10 kilometers from the volcano and the northern area is between 16-25 kilometers from the volcano. The description and analysis of fractures is carried out separately for the two areas as well as for the two areas together to test different mapping procedures, statistical methods and the influence of the volcano on the properties of th

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13

Andersson, Barbro. "Pressure-Temperature Estimates on the Tjeliken Eclogite from Northern Jämtland, Swedish Caledonides." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-196118.

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Eclogites are important in order to understand orogenic processes, since their presence indicates high-pressure metamorphism. In northern Jämtland, Swedish Caledonides, eclogites have been found at several places in the Seve Nappe Complex (SNC). The mountain Tjeliken in the Lower Seve Nappe is one of them. Dating relates the high-pressure metamorphism to the Late Ordovican subduction of the Baltoscandian margin during the closure of the Iapetus Ocean. In this study new P-T conditions are presented for the Tjeliken eclogite based on petrographical and geochemical studies of an eclogite sampled

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14

Karlsson, Pia. "Sulfidmineral i Salatrakten : med en introduktion i opakmikroskopi." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-196982.

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Sala är beläget i Bergslagen och bergarterna hör därmed till den svekofenniska berggrunden. Berggrunden domineras av 1.9-1.87 Ga sedimentära-, vulkaniska- och metamorfa bergarter. Vad man vet idag har metamorfosen i Bergslagen skett vid temperaturer på 500-650 ºC och på ett djup av 10-15 km. Salas berggrund är till stor del uppbyggd av karbonater, hälleflinta, kvartsdioritporfyrit, granofyr och granit. Karbonatstenen är till största delen magnesiumrik och övervägande dolomitisk till sammansättningen. Ett mer än 300 meter mäktigt dolomitlager innehåller Sala gruvas zink- och silvermalmer. I syd

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15

Magnusson, Johan. "Jordens metallresurser : En kort överblick över våra viktigaste industrimetaller och deras bildningssätt." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-211080.

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Metaller och gruvdrift är ett ständigt aktuellt ämne. Återanvändning av metaller blir allt viktigare då metaller betraktas som en ändlig resurs. Men är de verkligen det, och i sådana fall: ur vilket perspektiv? Arbetet behandlar bildningsprocesser för några av våra viktigaste metaller - guld, järn, nickel och koppar - samt en handfull sällsynta metaller vars användning ökat: indium, gallium och germanium. Arbetet börjar med att kortfattat diskutera begreppen malmer och mineral. Därefter beskrivs de processer som enligt rådande vetenskaplig teori ligger till grund för de viktigaste av dessa mal

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16

Martinsson, Evy. "Lainijaurintrusionens geokemi : En geokemisk studie av sidoberget till Lainijaur Ni-Cu malm." Licentiate thesis, Luleå tekniska universitet, 1987. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-16889.

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17

Andersson, Joel. "Structural evolution of two ore-bearing Palaeoproterozoic metasupracrustal belts in the Kiruna area, Northwestern Fennoscandian Shield." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-72034.

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In this project, two key study areas in the northwestern Fennoscandian Shield are under investigation. The “Western supracrustal belt” and “Central Kiruna area” are both located along lithotectonically comparable Rhyacian-Orosirian metasupracrustal belts and both areas are characterized by iron oxide-apatite (IOA) and iron oxide-copper-gold (IOCG)-style mineralizations and related hydrothermal alterations. The area is in general well studied but the structural evolution remains unresolved. In order to build a structural framework for the Kiruna area, the number of deformation events, kinematic

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18

Sädbom, Stefan. "Metamorfos och malmbildning i Enåsens guldgruva Hälsingland." Thesis, Uppsala universitet, Geologiska institutionen, 1987. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-442799.

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Some parts of the mineralogy and the petrology of the Enåsen gold-deposit, northern Hälsingland, Sweden are described. The gold in Enåsen is extracted from a sillimanite-rich quartzite. The rocks in the stratigraphic foot-wall of the ore are described as a part of a stratigraphic column. It is suggested that the sillimanite-quartzite is a part of an overturned stratigraphic sequence. The temperature and the pressure during the main metamorphose is determined to 620-670º C and 5-6.5 kbar by use of the mineral paragenesis and the graphite geothermometer. It is shown that the ores are of epigenet

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19

Minz, Friederike. "Mineralogical characterisation of the Rockliden antimony-bearing volcanic-hosted massive sulphide deposit, Sweden." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-17621.

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Rockliden is a polymetallic Zn-Cu volcanic-hosted massive sulphide (VHMS) deposit. It is located in north-central Sweden about 150 km south of the Skellefte ore district. Two major challenges to mining and production were identified soon after Rockliden was discovered in the 1980’s. Firstly, the geographic distance to Boliden’s main ore deposits and existing concentrator in the Skellefte district will set additional financial and logistic constrains for the processing of the ore. Secondly, the locally high Sb grade in the ore potentially lowers the quality of the Cu-Pb concentrate sent to the

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20

Patten, Clifford G. C. "Mobility of gold and other metals during alteration of the oceanic crust : Implications for the formation of VMS deposits." Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-132782.

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Tremendous physical and chemical exchanges occur along oceanic ridges between the lithosphere, the hydrosphere and the biosphere. During these exchanges important mobilisation of metals by hydrothermal fluid circulation takes place within the oceanic crust. Volcanogenic massive sulphide (VMS) deposits are hydrothermal ore deposits rich in Cu-Zn-Pb bearing sulphide minerals that form during submarine venting of these hydrothermal fluids near the seafloor. A proportion of the metals enriched in these deposits are mobilised from deeper crustal levels during high-temperature hydrothermal alteratio

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21

Metzger, Nicolai. "Structural controls on the shear zone hosted, IOCG-style Kiskamavaara Cu-Co-Au mineralization." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-74068.

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Sweden is the largest producer of iron ore in the European Union, as well as amongst the top producers for base and precious metals. Much of its mineral wealth derives from northern Norrbotten, type locality of the Kiruna-type-magnetite-apatite ores. Besides the massive iron ore bodies, the region is further recognized as important iron-oxide-copper-gold (IOCG) province, with the world class, Aitik Cu-Au-Ag-(Mo) deposit as its most prominent example (1061 Mt with 0,22% Cu; 0,15ppm Au; 1.3ppm Ag), (Wanhainen et al. 2012, Boliden 2017). The close spatial relation between Aitik, further IOCG styl

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22

Möne, Cecilia. "Glacial lake deposits in Kerlingarfjöll, Central Iceland." Thesis, Uppsala universitet, Institutionen för geovetenskap, 1997. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-393047.

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The extent of glacial lake sediments found north of the Kerlingarfjöll mountains in central Iceland has been determined and their formation in an ice dammed lake is suggested. The damming ice moved from an ice divide in the south-east highlands and was divided into two ice lobes by the Kerlingarfjöll mountains. In an early stage the lake was dammed between the two ice lobes but as they retreated the glacial lake was enlarged in the eastern part where it in the later stage was dammed by topography. The ice dammed lake was almost filled with sediments before it drained to the west when the weste

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23

Swärd, Henrik. "The deglaciation of southern central Sweden reflected in the seismic and sedimentary stratigraphy of southern Lake Vättern." Licentiate thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-113498.

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24

Jonsson, Linus. "Seismic tomography as an instrument for structural evaluation in the Printzsköld and Alliansen ore bodies, Malmberget." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-64918.

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The Malmberget deposit is one of the major apatite iron ores in Europe, located in northern Norrbotten. As the mining in Malmberget proceeds deeper more challenges with the stability have been faced. When the stress distribution of a rock mass exceeds the rock strength energy in form of seismic waves is released. In Malmberget, a monitoring system consisting of 200 geophones is installed which detects all seismic waves in the area. Based on data received from the monitoring system, LKAB has achieved to generate a seismic tomography model over the velocity variations of the seismic waves as the

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McClay, K. R. "Structural geology and tectonics /." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SD/09sdm126.pdf.

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Myers, Edwin Carl. "Constructing a creationist geology." Portland, Or. : Theological Research Exchange Network (TREN), 2005. http://www.tren.com.

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27

Riccomini, Claudio. "O Rift Continental do Sudeste do Brasil." Universidade de São Paulo, 1990. http://www.teses.usp.br/teses/disponiveis/44/44136/tde-18032013-105507/.

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O Rift continental do Sudeste do Brasil (RCSB), de idade cenozóica, é uma feição alongada e deprimida, desenvolvida entre as cidades de Curitiba (PR) e Niterói (RJ), numa extensão de pelo menos 800 km. Segue grosseiramente a linha de costa atual, da qual dista em média cerca de 70 km, alcançando o Atlântico na sua terminação nordeste. O segmento mais contínuo desse rift, entre as cidades de São Paulo (SP) e Volta Redonda (RJ), com cerca de 350 km de comprimento, foi objeto de estudo no presente trabalho, no tocante aos seus aspectos de tectonia e sedimentação. Com base principalmente na anális

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Kiani, Tayebeh. "Modeling for geospatial database : application to structural geology data : application to structural geology data." Paris 6, 2010. http://www.theses.fr/2010PA066057.

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L’objectif de cette étude est de créer un modèle de base de données dans un système d’information géographique afin d’archiver, analyser, présenter et de diffuser des données observées lors des analyses de géologie structurale. Le modèle de données est conçu pour atteindre quatre objectifs: établir un vocabulaire partagé par les spécialistes, modéliser les concepts de géologie structurale, produire des cartes dérivées des cartes géologiques d’Iran et fonctionner avec un logiciel de système d’information géographique. Un ensemble de classes conceptuelles est alors identifié pour représenter les

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Garrick-Bethell, Ian 1980. "Early lunar geology and geophysics." Thesis, Massachusetts Institute of Technology, 2009. http://hdl.handle.net/1721.1/47845.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2009.<br>Includes bibliographical references.<br>Despite a number of human and robotic missions to the Moon, there are still important unanswered questions about its early evolution, and how it came to be the object we observe today. Here we use observational, experimental, and theoretical techniques to examine three important events that took place early in lunar history and have left a lasting signature. The first event is the formation of the largest basin on the Moon, the South Pole

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Lisle, Richard John. "Techniques of quantitative structural geology." Thesis, University of Birmingham, 2007. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.446367.

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Woodworth-Lynas, Christopher M. T. "The geology of ice scour." Thesis, Bangor University, 1992. https://research.bangor.ac.uk/portal/en/theses/the-geology-of-ice-scour(eaa92a2c-71af-4304-b8dd-cfe595160468).html.

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Ice scour is the phenomenon that occurs when the keel of a floating mass of ice (iceberg, sea ice or freshwater ice) touches, penetrates and continues to move forward through unlithified seabed or lakebed sediments. The typically curvilinear excavation made by the scouring keel is called a scour mark. Scouring ice keels present logistical problems to the safe installation and operation of, for example, oil and gas production pipelines and power and telecommunication cables in several cold ocean regions. The typical surface morphologies of modern iceberg scour marks on the Labrador continental

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FERRARETTI, Denis. "Data Mining for Petroleum Geology." Doctoral thesis, Università degli studi di Ferrara, 2012. http://hdl.handle.net/11392/2389427.

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In petroleum geology, exploration and production wells are often analysed using image logs, because they provide a visual representation of the borehole surface and they are fundamental to retrieve information on bedding and rocks characteristics. Aim of this Ph.D. work was to define and implement a suite of automatic and semi-automatic tools for interpretation of image logs and large datasets of subsurface data coming from geological exploration. This led to the development of I2AM (Intelligent Image Analysis and Mapping), a semi-automatic system that exploits image processing algori

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Tollefsen, Elin. "Thermal and chemical variations in metamorphic rocks in Nautanen, Gällivare, Sweden." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-149643.

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This study focuses on the geology of the Nautanen area. It is part of the SGU-financed project, Metamorphic Map of Sweden, which aims to compile metamorphic data from Sweden and takes the form of a number of Bachelor and Master projects. The main metamorphic event in the Nautanen area is the Svecokarelian Orogeny (1.96 – 1.75 Ga). The samples are metamorphosed sedimentary and volcanic rocks, which were intruded by intermediate to mafic intrusions and a later granite intrusion. The supracrustal rocks are folded and the Nautanen Deformation Zone (NDZ) traverses the area in a NW to SE direction.

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Turner, Tom. "Petrography, alteration and structure of the Bronäs Zn-Pb-Ag deposits, Bergslagen, Sweden." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-78822.

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This report aims to characterize the alteration styles and mineralization of the Zn-Pb-Ag Bronäs deposit, in the Sala area of the Bergslagen mining district, Sweden. It presents data collected through 237m of lithological logging and subsequent lithogeochemical data, which, coupled with thin section and SEM analysis has led to the first geological descriptions of the rocks in the deposit. The results are presented in the report through logs and a cross-section interpreted from these logs. The Bronäs deposit, mined between 1945 and 1962, is a satellite deposit to the well-known Sala mine, an

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Patch, Nickolas Lee. "Geology of the Dyer Mountain quadrangle, Utah." Thesis, Manhattan, Kan. : Kansas State University, 2009. http://hdl.handle.net/2097/1452.

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Castro, Ana Marina Escobar [UNESP]. "Depósitos marinhos juro-cretácicos em afloramentos de cuba: nanofósseis calcários e microfácies carbonáticas." Universidade Estadual Paulista (UNESP), 2005. http://hdl.handle.net/11449/102979.

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Made available in DSpace on 2014-06-11T19:32:20Z (GMT). No. of bitstreams: 0 Previous issue date: 2005-10-27Bitstream added on 2014-06-13T19:02:54Z : No. of bitstreams: 1 castro_ame_dr_rcla.pdf: 55950380 bytes, checksum: 297aeb38dae64c995595373122b66a6c (MD5)<br>Agência Nacional do Petróleo, Gás Natural e Biocombustíveis (ANP)<br>Rochas do Jurássico Superior e Cretáceo, dominantemente carbonáticas e comumente intercaladas a folhelhos e margas, afloram em Cuba central e ocidental. O estudo de 31 afloramentos é o objeto desta tese, que investiga, centralmente, o seu conteúdo nanofossilífero e

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Copfer, Torrey J. "Geology of the Deseret Peak East 7.5' Quadrangle, Tooele County, Utah, and Impacts for Hydrology of the Region." DigitalCommons@USU, 2003. https://digitalcommons.usu.edu/etd/6723.

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Detailed geologic mapping of the Deseret Peak East 7.5' Quadrangle yields new interpretations regarding the stratigraphy of the Oquirrh Basin, fault and fold geometry, and structural evolution of the region. The Stansbury Range consists of the north-southtrending Deseret anticline. Basal Mississippian units rest unconformably on Cambrian beds in the central part of the range. Paleozoic uplift, Mesozoic contraction, and Cenozoic extension have created a series of broad folds, large thrust faults, and several normal faults. The area is dominated by bedrock springs, with the presence of abundant

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Duber, James R. "Museum of geology for Breezewood, PA: "Studying the role of architecture in the science of geology"." Thesis, Virginia Polytechnic Institute and State University, 1993. http://hdl.handle.net/10919/53347.

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People cannot be trained to marvel at landscapes, nor to love their places and their planet. On the other hand, love of place and of the Earth are scarcely sentimental extras to be indulged only when all technical and material problems have been resolved... The experiences of places, spaces and landscapes in which academic geography originates are a fundamental part of everyone's experience, and geography has no exclusive claim to them. Indeed, one of the first aims of a phenomenology of geography should be to retrieve these experiences from the academic netherworld and to return them to ever

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Stossel, Deborah Louise. "The engineering geology of Frankton Arm." Thesis, University of Canterbury. Geology, 1999. http://hdl.handle.net/10092/6815.

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Seven bedrock landslides situated within quartzofeldspathic schist exist up slope of the residential area along the Frankton Arm of Lake Wakatipu, South Island, New Zealand. Engineering geological and geotechnical failure models for these landslides have been established using engineering geological mapping at scales of 1:5000 and 1:10000, geotechnical testing, and the development of limit-equilibriurn sensitivity models. Geotechnical testing of artificially fractured schist bedrock obtained shear strength values of Φ = 24°-36° and zero cohesion, and point load strength indexes of 0.6-3.83MPa

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Tingley, A. C. "Engineering geology of landfill gas migration." Thesis, University of Surrey, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.290487.

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Moore, Edwin Neville. "Glacial geology and geomorphology of Weardale." Thesis, Durham University, 1994. http://etheses.dur.ac.uk/1625/.

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Teeling, Michael J. "Geology of Galileo Regio quadrangle, Ganymede." Kansas State University, 1987. http://hdl.handle.net/2097/18557.

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Kneller, Benjamin Charles. "The geology of part of Buchan." Thesis, University of Aberdeen, 1988. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU020384.

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The research embodied in this thesis arose from a contract to remap Sheet 87W of the 1:50,000 geological map for the Geological Survey. The rocks investigated include late Precambrian to early Cambrian metasediments of the Dalradian Supergroup, and Caledonian intrusive igneous rocks. The range of sedimentary facies present within the Methlick Formation (Southern Highland Group) is described within the framework of current deep marine clastic facies classifications, and an inner to middle submarine fan facies model erected. Framework petrography, palaeocurrents, geochemistry and facies variatio

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Kerber, Paulo Augusto. "Granitic series and their economic geology." Thesis, Rhodes University, 1993. http://hdl.handle.net/10962/d1005581.

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The granitic rocks are subdivided into four series: tholeiitic, alkaline, calc-alkaline and mobilizates. These series can be formed from melting of mantle material (M-type granites) or from crustal rocks. There are granitic rocks formed from the mixing of these two magmas types. The rocks formed from crustal anatexis are subdivided into those formed from igneous rocks (I-type granites) and those formed from meta-sedimentary rocks (S-type granites). The former has similar characteristics to the mantle-derived granitoids. The mineral deposits related to igneous or mantle derived magma usually ar

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Miller, John Frederick. "Structural geology of the Ohio Shale." Connect to resource, 1996. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1163610177.

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Tiedeken, Staci L. "Magnetism and geology of the moon." Thesis, University of Iowa, 2017. https://ir.uiowa.edu/etd/5660.

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Since different parts of the Moon display varying magnetic field strengths, our goal was to determine whether these differences are due to specific geological characteristics. We found that older materials tend to be more magnetic than younger materials. Additional statistical studies found that the mare regions of the Moon are less magnetic than the plains and terra regions. We did not find a simple relationship between lunar magnetism and crustal thickness, and this is inconsistent with the hypothesis that thicker crust is more magnetic since there is additional material. Thus, it is not jus

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Harris, William B. "The geologic history of Rock Canyon, Utah : a virtual trip /." CLICK HERE for online access, 2002. http://www.geology.byu.edu/faculty/rah/slides/Rock%20Canyon/Home.htm.

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Thesis (M.S.)--Brigham Young University. Dept. of Geology, 2002.<br>Web site works as of 02/10/03. Consult BYU Dept of Geology for URL changes in future. Includes bibliographical references (leaves 8-9). Also available via Internet.

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Key, Heyward M. "Temporal and spatial trends in drilling predation on Crepidula in the U.S. coastal plain /." Electronic version (PDF), 2003. http://dl.uncw.edu/etd/2003/keyh/heywardkey.pdf.

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Lindelöf, Linnea, and Isabelle Åberg. "Landslide survey, Mamuyod, the Philippines." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-228919.

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Kärrström, Timmy. "From Bedrock to Porcelain : A study regarding the history of porcelain, Ytterby mine and the discovery of yttrium in Sweden." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-167721.

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Porcelain is a translucent vitreous material that consists of clay (kaolin), feldspar and quartz which has been mixed and heated together to cause a metamorphic reaction. In Sweden, the Porcelain industry was established in 1726 at Rörstrands castle in Stockholm and is today one of the oldest industries in Europe to produce porcelain. Around the 1790’s Rörstrand got its feldspars and quartz from the Ytterby mine that was located at Resarö in Stockholm’s archipelago making the raw material somewhat easy to access. Rörstrand owned the mine in the 1850’s to 1926. During the time Ytterby mine was

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