Dissertations / Theses on the topic 'Orogeny'
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Kerrison, Aidan P. "Spatial-temporal-compositional evolution of syn-orogenic magmatism in the northern New England Orogen: Implications for the Permo-Triassic eastern Gondwanan margin." Thesis, Queensland University of Technology, 2022. https://eprints.qut.edu.au/228970/1/Aidan_Kerrison_Thesis.pdf.
Full textShen, Wenlue. "Post-orogenic extension in the Pearl River Delta region (South China) an integrated morphological, structural, geophysical and thermochronological study /." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/HKUTO/record/B39558587.
Full textBrocka, Christopher G. "Laramide stress conditions and deformation mechanisms during the formation of Derby and Dallas Domes, Weiser Pass Quadrangle, Wind River Mountains, Wyoming." Diss., Columbia, Mo. : University of Missouri-Columbia, 2007. http://hdl.handle.net/10355/4922.
Full textThe entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed on April 15, 2009) Includes bibliographical references.
Reed, Robert Mark. "Emplacement and deformation of late syn-orogenic, Grenville-age granites in the Llano uplift, central Texas /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.
Full textVita. Four folded maps in pocket. Includes bibliographical references (leaves 254-271). Available also in a digital version from Dissertation Abstracts.
Bendall, Betina R. "Metamorphic and geochronological constraints on the Kimban Orogeny, Southern Eyre Peninsula /." Title page, abstract and contents only, 1994. http://web4.library.adelaide.edu.au/theses/09SB/09sbb458.pdf.
Full textRiley, Dean Nolan. "Granites, orogeny, and the deblois pluton complex in Eastern Maine, USA." Connect to this title online, 2004. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1087232113.
Full textTitle from first page of PDF file. Document formatted into pages; contains xliv, 546 p.; also includes graphics. Includes bibliographical references (p. 517-546).
Kashubin, Artem. "Seismic Studies of Paleozoic Orogens in SW Iberia and the Middle Urals." Doctoral thesis, Uppsala universitet, Geofysik, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-9405.
Full textScheiner, Scott W. "Refining Paleoproterozoic Sedimentary Sequence Boundaries in East-Central Minnesota, Carlton County: Implications for Source, Age, Correlations, and Tectonic Histories." Kent State University / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=kent1350923963.
Full textSpencer, Christopher J. "Generation and preservation of continental crust in collisional orogenic systems." Thesis, University of St Andrews, 2013. http://hdl.handle.net/10023/11966.
Full textPʻu-chʻüan, Ting. "Structural and tectonic evolution of the Eastern Arunta Inlier in the Harts Range area of Central Australia /." Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09PH/09phd5839.pdf.
Full textTypescript (Photocopy). Copies of 4 published papers co-authored by author, and 7 maps, in back cover pocket. Includes bibliographical references (leaves 203-218).
Stewart, Martyn. "Kinematic evolution of the Great Glen Fault Zone, Scotland." Thesis, Oxford Brookes University, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.364096.
Full textJiaxin, Zhou. "Geochemistry of the Kilmelford intrusives, West Scotland, in relation to the Caledonian orogeny." Thesis, Imperial College London, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261034.
Full textHales, Tristram Charles. "Role of lithospheric delamination and ice-driven rockfall erosion in the evolution of mountainous landscapes /." view abstract or download file of text, 2006. http://proquest.umi.com/pqdweb?did=1280144241&sid=2&Fmt=2&clientId=11238&RQT=309&VName=PQD.
Full textTypescript. Includes vita and abstract. Includes bibliographical references (leaves 115-137). Also available for download via the World Wide Web; free to University of Oregon users.
Baldim, Maurício Rigoni 1983. "O domo gnáissico Alto Alegre, transição embasamento-greenstone belt do Rio Itapicuru : evolução e significado tectônico." [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/286596.
Full textDissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências
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Resumo: Domos gnáissicos são estruturas que podem estar associadas tanto aos orógenos extensionais quanto aos colisionais. Em orógenos colisionais, normalmente balizam os distintos terrenos dispondo-se em corredores estruturais. Na região nordeste do Cráton São Francisco, Bloco Serrinha, localiza-se o Greenstone Belt Paleoproterozoico do Rio Itapicuru, interpretado como arco continental acrecionado a um Complexo de alto grau mesoarqueano. Mapeamento geológico realizado no segmento norte da transiçao, embasamento-greenstone, revelou a ocorrência de um domo gnáissico-migmatítico que limita dois terrenos, um arqueano e outro paleoproterozoico, que destoa litoestruturalmente de outros domos reconhecidos a sul do greenstone (e.g. domos do Ambrósio, Salgadália e Pedra Alta). Além disso, dados estruturais mostram que a evolução tectônica da área ocorreu a partir de tectônica compressiva em D1 com direção E-W, seguido de transcorrência N-S em D2, possivelmente associados a transpressão. O domo, denominado Alto Alegre, possui núcleo granito-diatexítico, sendo delineado por faixas anfibolíticas concêntricas e preserva paragênese de alto grau metamórfico. Análises de elementos maiores e traços revelam que as faixas de anfibolitos do referido domo possuem características geoquímicas semelhantes aos diques máficos que cortam o embasamento, e destoam dos basaltos toleíticos do greenstone belt. Dados geocronológicos e de campo revelam idades de ca. 3080 Ma para o embasamento arqueano e para gnaisses do domo Alto Alegre, e idades de ca. 2080 Ma para o granito que intrude a porção central do domo. Os dados mostram que o domo Alto Alegre representa o embasamento arqueano retrabalhado tectonicamente e influenciado por atividade granítica, durante colisão continente-continente em ca. 2080 Ma
Abstract: Gneiss domes are structures that may be associated with both extensional and collisional orogens. In collisional orogens typically delimit distinct land forming structural corridors. In northeastern of São Francisco craton, Serrinha Block, is located the Paleoproterozoic Rio Itapicuru Greenstone Belt which is interpreted as a continental arc acrecionado to a Mesoarqueano high degree Complex. Geological mapping carried out in the northern segment of the greenstone-basement transition, revealed the occurrence of a gneissic-migmatitic dome that limits two lands, one Archean and another Paleoproterozoic. This dome is different both on litology as structuraly when comparing with other domes recognized in a south of the greenstone (e.g., domes of Ambrose, Salgadália and Pedra Alta). Furthermore, structural data show that the tectonic evolution of the area occurred from compressive tectonics E-W in D1, followed by transcurrent N-S in D2, possibly associated with transpression. The dome, called Alto Alegre, has granite-diatexítico core being outlined by concentric amphibolitic bands that preserves high metamorphic grade paragenesis. Results of major and trace elements analyzes reveal that the amphibolites bands of dome has geochemical characteristics similar to mafic dikes that cut the basement, and differ from Rio Itapicuru greenstone belt basalts. Geochronological and field data reveal ages ca. 3080 Ma for the Archean basement and the dome Alto Alegre gneisses, and ages of ca 2080 Ma for the granite that intrude the central portion of the dome. The data show that the dome Alto Alegre represents the tectonically reworked Archean basement and influenced by granite activity during continent-continent collision at ca 2080 Ma
Mestrado
Geologia e Recursos Naturais
Mestre em Geociências
Tozer, Craig Hampton. "The influence of inherited structures on the Cenozoic orogeny of the Kyrgyz Tien Shan /." view abstract or download file of text, 2004. http://wwwlib.umi.com/cr/uoregon/fullcit?p3147837.
Full textTypescript. Includes vita and abstract. Includes bibliographical references (leaves 171-180). Also available for download via the World Wide Web; free to University of Oregon users.
Price, Alun R. "Multiple sheeting as a mechanism of pluton construction : the main Donegal granite, NW Ireland." Thesis, Durham University, 1997. http://etheses.dur.ac.uk/5074/.
Full textMcKellar, Zoe. "Sedimentology of the Lower Old Red Sandstone of the northern Midland Valley and Grampian outliers, Scotland : implications for post-orogenic basin development." Thesis, University of Aberdeen, 2017. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=236193.
Full textChapman, James Benjamin. "Structural relationships and crustal deformation in the Saint Elias Orogen, Alaska." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2008. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.
Full textChan, Yau-cheong Ian, and 陳有昌. "Characterizing crustal melt episodes in the Himalayan orogen." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/206505.
Full textpublished_or_final_version
Applied Geosciences
Master
Master of Science
Linde, G. M., J. H. Trexler, P. H. Cashman, G. Gehrels, and W. R. Dickinson. "Three-Dimensional Evolution of the Early Paleozoic Western Laurentian Margin: New Insights From Detrital Zircon U-Pb Geochronology and Hf Isotope Geochemistry of the Harmony Formation of Nevada." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/626478.
Full textHinojosa-Prieto, Hector R. "Tectonothermal history of the La Noria-Las Calaveras region, Acatlán Complex, southern Mexico implications for Paleozoic tectonic models /." Ohio : Ohio University, 2006. http://www.ohiolink.edu/etd/view.cgi?ohiou1151434573.
Full textLock, Jane. "Interpreting how low-temperature thermochronometric data in fold-and-thrust belts : an example from the Western Foothills, Taiwan /." Thesis, Connect to this title online; UW restricted, 2007. http://hdl.handle.net/1773/6698.
Full textClements, James Wesley. "Laramide stress conditions and deformations mechanisms during the formation of Hudson and Dallas Domes, Lander Quadrangle, Wind River Mountains, Lander, Wyoming." Diss., Columbia, Mo. : University of Missouri-Columbia, 2008. http://hdl.handle.net/10355/5640.
Full textThe entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file and four media files (media file 1.pdf, media file 2.pdf, media file 3.pdf, and media file 4.pdf) Title from title screen of research.pdf file (viewed on August 25, 2008) Vita. Includes bibliographical references.
Buscher, Jamie Todd. "The Impact of Long-Term Glacial Erosion on the Active Chugach-St. Elias Mountains, southern Alaska." Thesis, Virginia Tech, 2003. http://hdl.handle.net/10919/9618.
Full textMaster of Science
Cross, David B. "High-frequency tectonic sequences in the Campanian Castlegate Formation during a transition from the Sevier to Laramide orogeny, Utah, U.S.A." ScholarWorks@UNO, 2016. http://scholarworks.uno.edu/td/2133.
Full textBendall, Betina. "Mid-Palaeozoic shear zones in the Strangways Range : a record of intracratonic tectonism in the Arunta Inlier, Central Australia." Title page, contents and introduction only, 2000. http://web4.library.adelaide.edu.au/theses/09PH/09phb458.pdf.
Full textSiqueira, Luzia Helena. "Granito São Domingos : registro de magmatismo pós-tectônico do orógeno intracontinental aguapeí - SW do Cráton Amazônico." Universidade Federal de Mato Grosso, 2015. http://ri.ufmt.br/handle/1/114.
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O Granito São Domingos corresponde a um dos corpos da Suíte Intrusiva Guapé, localizado na Faixa Móvel Aguapeí, relacionado à Orogenia Sunsás, SW do Cráton Amazônico. Trata-se de um corpo com dimensões batolíticas de 150 Km² de área aflorante, levemente alongado segundo direção NE e localizado ao norte do distrito São Domingos, município de Jaurú, estado de Mato Grosso. Constitui-se de rochas holo a leucocráticas, de cor rosa-claro a cinza-rosado, isotrópicas, equi a inequigranulares, por vezes, porfiríticas e pegmatíticas, classificadas como Muscovita biotita monzo a sienogranitos tendo por vezes, granada e monazita como minerais acessórios primários e caracterizadas como granitos do tipo S ou Muscovite bearing Peraluminous Granitoids (MPG). Essas rochas apresentam restritos e elevados teores de sílica, caracterizando-as como muito evoluídas; formadas por magmatismo cálcio alcalino de alto K a shoshonítico, peraluminoso e ferroso. A idade U-Pb (SHRIMP) de 928 ± 5 Ma foi obtida em zircões ígneos, e coincide com idades U-Pb (TIMS) relatadas para este granito. A análise Sm-Nd indica uma idade modelo TDM de 1,58 Ga, e valor ɛND(0,93Ga) negativo (-2,90). Esses resultados indicam que o Granito São Domingos formou-se em um ambiente pós-tectônico, no final da Orogenia Sunsás, cuja origem magmática está associada ao retrabalhamento de crosta continental mesoproterozoica. Três padrões diferentes de ETR foram encontrados para esses litotipos, sugerindo a geração de magmas contemporâneos não cogenéticos, provenientes de fontes crustais distintas.
The São Domingos Granite is an intrusive body of the Guapé Intrusive Suite, located in the Aguapeí mobile belt, corresponding to a branch of the Sunsás Orogeny in SW Amazonian Craton. This body is considered as a batholith slightly elongated in the NE direction, which crops out over an area of ca. 150 km2. It is situated to the north of the São Domingos District, a municipality of the Jauru city, Mato Grosso State. It consists of hololeucocratic to leucocratic rocks ranging from pinky to pinky-gray. They are isotropic, ranging from equigranular to inequigranular grains, sometimes porphyritic and pegmatitic, classified as muscovite-biotite monzo to syenogranites. Sometimes they present garnet and monazite as primary accessory minerals. These features characterize them as S-type granites or Muscovite bearing Peraluminous Granitoides (MPG). The rocks contain high silica content, which characterizes them as very evolved, formed by high-K to shoshonitic, peraluminous, and ferrous calc-alkaline magmatism. A U-Pb age of 928 ± 5 Ma was obtained for one of the analyzed rocks, which agrees with previous U-Pb ages obtained for this granite. Sm-Nd analysis indicates a TDM model age of 1.58 Ga, and negative ND value (-2.90). These results demonstrate that the São Domingos intrusion corresponds to a post tectonic environment, related to the Sunsás orogeny, whose magmatic origin is associated to re-working of the ancient continental crust. Moreover, three different ETR patterns were found for these lithotipes, suggesting the generation of contemporaneous non-cogenetic magmas, involving distinct crustal sources.
Bayona, German. "CONTROLS ON MIDDLE TO LATE ORDOVICIAN SYNOROGENIC DEPOSITION IN THE SOUTHEASTERN CORNER OF LAURENTIA." UKnowledge, 2003. http://uknowledge.uky.edu/gradschool_diss/364.
Full textHamlin, Herbert Scott. "Syn-orogenic slope and basin depositional systems, Ozona sandstone, Val Verde Basin, southwest Texas /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.
Full textElswick, Virginia L. "Seismic interpretation and structural evaluation of the Hope Basin, Alaska." Morgantown, W. Va. : [West Virginia University Libraries], 2003. http://etd.wvu.edu/templates/showETD.cfm?recnum=3014.
Full textTitle from document title page. Document formatted into pages; contains vi, 21, [24] p. : ill. (some col.), maps (some col.). Includes abstract. Includes bibliographical references (p. 20-21).
Lagor, Samuel William. "The Relationship Between Magmatism and Deformation During the Acadian Orogeny: A Case Study from Eastern-Central Vermont." ScholarWorks @ UVM, 2016. http://scholarworks.uvm.edu/graddis/566.
Full textGrimes, Stephen Whiteford. "The Grenville orogeny in West Texas : structure, kinematics, metamorphism and depositional environment of the Carrizo Mountain Group /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.
Full textVita. Three folded plates in pocket. Includes bibliographical references (leaves 359-371). Available also in a digital version from Dissertation Abstracts.
Yao, Weihua. "Evolution of the Lower Palaeozoic Nanhua Foreland Basin and nature of the Wuyi-Yunkai Orogeny, South China." Thesis, Curtin University, 2014. http://hdl.handle.net/20.500.11937/2183.
Full textMcNeice, Gary Wayne. "Magnetotelluric investigation of the Appalachians, Newfoundland, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape17/PQDD_0026/MQ36152.pdf.
Full textRose, Shellie. "Timing constraints and significance of Paleoproterozoic metamorphism within the Penokean orogen, northern Wisconsin and Michigan (USA)." Ohio University / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1090940526.
Full textMisiewicz, Julian Edward. "The geology and metallogeny of the Otavi mountain land, Damara orogen, SWA/Namibia, with particular reference to the Berg Aukas Zn-Pb-V deposit a model of ore genesis." Thesis, Rhodes University, 1988. http://hdl.handle.net/10962/d1005571.
Full textLabadie, Julia E. Schermer Elizabeth. "The structural and tectonic history of the Mt. Formidable region, North Cascades, Washington /." Online version, 2010. http://content.wwu.edu/cdm4/item_viewer.php?CISOROOT=/theses&CISOPTR=333&CISOBOX=1&REC=14.
Full textFitz-Gerald, Dudley Braden. "Evidence for an Archean Himalayan-style orogenic event in the northern Teton Range, Wyoming." Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1798480821&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Full textTabaud, Anne-Sophie. "Le magmatisme des Vosges : conséquence des subductions paléozoïques (datation, pétrologie, géochimie, ASM)." Thesis, Strasbourg, 2012. http://www.theses.fr/2012STRAH003/document.
Full textThe Vosges Mountains are characterized by the presence of numerous magmatic intrusions and extrusions of varied affinities. Accordingly, they constitute the best site to investigate, by dating and geochemistry, the evolution of the events affecting this segment of the Variscan orogeny. Two successions of identical magmatic events, shifted in the time, are identified, characterizing both Moldanubian (360 to 320 Ma) and the Saxothuringian (335 to 295 Ma) domains. These successions of magmatic events result of two major process. The progress of subducted and underplated continental crusts at Moho depth under continental blocks permits to shift from calc-alkaline to high potassic calc-alkaline magmatism. The radiogenic heat production from latter underplated continental crusts, in a first time, permits to generate magnesio-potassic magmas at depth. Then, this radiogenic heat permits to generate crustal magmas by intrusion of magnesio-potassic magmas rich in K, U and Th at mid-upper crust boundarie. These successions of magmatic events and particularly, the presence of the magnesio-potassic granites, imply a strong link between the Vosges Mts. and the eastern part of the Variscan orogeny (Black Forest, Bohemian Massif, the Alps and Corsica Batholith)
Moe, Aung. "Structural development of a volcanic sequence of the Lahn area during the variscan orogeny in the Rhenohercynian belt (Germany)." [S.l. : s.n.], 2000. http://deposit.ddb.de/cgi-bin/dokserv?idn=961466162.
Full textShen, Yunqing. "Gravitational collapse of orogenic belts : a preliminary study /." free to MU campus, to others for purchase, 1997. http://wwwlib.umi.com/cr/mo/fullcit?p9842565.
Full textLillydahl-Schroeder, Hosanna. "New Petrological and In-situ Electron Microprobe Monazite Age Constrainsts on the Timing of the Foxe Orogeny, Melville Penninsula, Nunavut, Canada." Thesis, Boston College, 2013. http://hdl.handle.net/2345/3032.
Full textThe Paleoproterozoic Foxe Fold Belt (FFB) is composed of the Penrhyn Group, a Paleoproterozoic passive margin sequence, and supracrustal Archean basement. These units were interfolded and metamorphosed at amphibolite to lower granulite facies conditions during the 1883-1865 Ma Foxe orogeny, a part of the Trans-Hudson orogeny. The purpose of this study was to constrain the timing of metamorphism and deformation within the Penrhyn Group, in order to determine the role of the Foxe orogeny within the Trans-Hudson orogeny. Petrographic analysis, P-T-X pseudosections, monazite composition, and in-situ electron microprobe U-Th-Pb geochronology from sampled metapelites were used to determine the age and significance of metamorphic and deformation events related to monazite age populations. Population 1 is composed of 1926 ± 8 Ma monazite interpreted as detrital. Population 2 consists of 1892 ± 9 Ma monazite, the youngest detrital ages seen in the Penrhyn Group. Population 3 is composed of 1853 ± 5 Ma high-Y + HREE monazite predating an episode of pervasive garnet growth. Population 4 contains 1839 ± 8 Ma lower-Y + HREE monazite related to pervasive garnet growth. Population 5 is 1819 ± 16 Ma lowest-Y + HREE monazite with high LREE and Th/U, linked to the interpreted peak reaction: Bt + Sil + Pl = Grt + Crd + Kfs + melt. Monazite constraints on deformation fabrics indicate that deformation was ongoing locally as early as 1853 ± 9 Ma and continued until at least 1814 ± 14 Ma, pre- to syn-peak metamorphism. Rare 1794-1776 Ma monazite is interpreted to constrain the age of retrograde metamorphism as the Trans-Hudson orogeny waned. These data support interpreted clockwise P-T-t-D paths consistent with metamorphism initiated by crustal thickening in an orogenic belt
Thesis (MS) — Boston College, 2013
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
Strack, Cody M. "Petrologic Study of the Danburg, Sandy Hill, and Delhi Intrusions: Constraints on Magmatism in the Southern Appalachians." Ohio University / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1439388136.
Full textGraessner, Thorsten. "Thermal evolution of the continental crust of Calabria during the Hercynian orogeny constraints from metamorphic phase equilibria and isotopic dating /." [S.l. : s.n.], 1999. http://e-diss.uni-kiel.de/diss=/d327.pdf.
Full textMacKenzie, Douglas James, and n/a. "Structural controls on orogenic gold mineralisation in the Otago Schist, New Zealand and the Klondike Schist, Canada." University of Otago. Department of Geology, 2008. http://adt.otago.ac.nz./public/adt-NZDU20080704.085108.
Full textAnderson, Eric Douglas. "PETROLOGIC, GEOCHEMICAL, AND GEOCHRONOLOGIC CONSTRAINTS ON THE TECTONIC EVOLUTION OF THE SOUTHERN APPALACHIAN OROGEN, BLUE RIDGE PROVINCE OF WESTERN NORTH CAROLINA." UKnowledge, 2011. http://uknowledge.uky.edu/gradschool_diss/820.
Full text沈文略 and Wenlue Shen. "Post-orogenic extension in the Pearl River Delta region (South China): an integrated morphological, structural,geophysical and thermochronological study." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B39558587.
Full textTsang, Pui-wai Debbie, and 曾珮蔚. "Thermochronology inferring post-orogenic exhumation model around Greater Pearl River Delta region." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2010. http://hub.hku.hk/bib/B45861432.
Full textGrimm, Ryan P. "Insights Into the Stratigraphic Evolution of the Early Pennsylvanian Pocahontas Basin, Virginia." Diss., Virginia Tech, 2010. http://hdl.handle.net/10919/40424.
Full textPh. D.
Hansman, Reuben. "Constraining the Uplift History of the Al Hajar Mountains, Oman." Licentiate thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-133409.
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