The oxygen isotope geochemistry of granitoid rocks from the southern and central Yukon

by Georges Roman Dagenais

Publisher: University of Alberta, Dept. of Geology in Edmonton

Written in English
Cover of: The oxygen isotope geochemistry of granitoid rocks from the southern and central Yukon | Georges Roman Dagenais
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About the Edition

Masters thesis. Results of study of oxygen isotope ratios of 80 granitoid samples from the southern and central Yukon along with 39 country rocks.

Edition Notes

References cited:p.143-57.

Statementby Georges Roman Dagenais
The Physical Object
Paginationxiv, 168p.
Number of Pages168
ID Numbers
Open LibraryOL27323401M
OCLC/WorldCa70522828

Paleoclimate Reconstruction Based on Oxygen Isotope Composition of Foraminifera in Southern Mountains Area, Central Java-IndonesiaAkumaluddin, Akihiro KANO and Koichiro WATANABEProceedings of the International Seminar on Geology of the Southern Mountains of Java, Yogyakarta, Volume 1, pp, August, Full Text Geochronology, geochemistry, and Sr–Nd–Pb–Hf isotopes of the Zhunsujihua granitoid intrusions associated with the molybdenum deposit, northern Inner Mongolia, China: implications for petrogenesis and tectonic setting. COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has pulled together information and resources to assist library staff as they consider how to handle coronavirus. Neodymium Isotope Geochemistry An Introduction. cyfol 0 Comment.

  The δ34S values of the pyrite range from ‐‰ to −‰, with an average of −‰, suggesting origin from a mixture of magmatic/mantle sources and the basement rocks. The Pb isotope compositions of the pyrite show a range of to for Pb/Pb, to for Pb/Pb, and to for Pb/Pb. The electronic supplements contain all data used in this study. This includes all compiled data from literature and new zircon LA-ICP-MS U-Pb geochronology, whole-rock and zircon geochemistry and Sm-Nd isotope data for the Sveconorwegian granitoid suites. In “Reviews in Mineralogy and Geochemistry: Geochemistry of Non-Traditional Stable Isotopes”, vol. 55, Beard, B and Johnson, C () Chapter 10A: Fe isotope variations in the modern and ancient Earth and other planetary bodies. † Dusel-Bacon, C., Day, W.C., Aleinikoff, J.N., , Geochemistry, petrography, and zircon U–Pb geochronology of Paleozoic metaigneous rocks in the Mount Veta area of east-central Alaska: implications for the evolution of the westernmost part of the Yukon–Tanana terrane. Canadian Journal of Earth Sciences, v. 50, p.

JODIE A. MILLER, GIULIO VIOLA, NEIL S. MANCKTELOW Oxygen, carbon and strontium isotope constraints on the mechanisms of nappe emplacement and fluid–rock interaction along the subhorizontal Naukluft Thrust, central Namibia, Journal of the Geological Society , no.3 3 (May ): Trace element and Sr, Nd, Pb and O isotope variations in medium-K and high-K volcanic rocks from Merapi volcano, Central Java, Indonesia: Evidence for the involvement of subducted sediments in Sunda arc magma genesis. JOURNAL OF PETROLOGY, vol. 44(3), link> doi>. Henderson GM et al.: Direct Dating of Oxygen-Isotope Substage 5e by Measurement of U and Th Isotopes in Marine Sediments From the Bahamas Antonow M: Geochemistry of Central Greenland Sea Sediments and Isotopic Characterization of Surface Water Masses of the Past ky. Volume 84 complete / / Geochemistry of the hot rocks of the volcanogenic massive sulfide deposit at Que River, Tasmania; Geochemistry and metamorphism of the Prieska Zn-Cu Deposit, South Africa; Geologic setting, depths of emplacement, and regional distribution of fluid inclusions in intrusions of the Central Wasatch Mountains, Utah.

The oxygen isotope geochemistry of granitoid rocks from the southern and central Yukon by Georges Roman Dagenais Download PDF EPUB FB2

ELSEVIER Chemical Geology () CHEMICAL GEOLOGY INrGIMN(: ISOTOPE GEOSCIENCE Oxygen and hydrogen isotope geochemistry of S- and I-type granitoids: the Cape Granite suite, South Africa Chris Harris a, *, Kevin Faure a°', Roger E.

Diamond a, Reyno Scheepers b a Department of Geological Sciences, University of Cape Town, Rondebosch,Cited by:   The composite Yozgat batholith consists of a S-I-A-type granitoid association intruding the supra-subduction zone-type (SSZ-type) central Anatolian ophiolite and medium- to high-grade metasedimentary rocks of the central Anatolian crystalline complex.

These rocks are unconformably covered by Palaeocene to Early Eocene sedimentary rocks. The I-type granitoids are the most common rock Cited by:   Metamorphic rocks have oxygen isotope compositions that are usually similar to those of igneous and sedimentary rocks, with δ 18 O values ranging from +6‰ to +18‰, depending on the geochemical nature of protolith and the degree of water–rock interaction during prograde metamorphism (e.g., Hoefs,Sharp et al., ).Cited by: Abstract Granitic orthogneiss is widespread throughout the metamorphic core of the Brooks Range in both the ductilely deformed blueschist/greenschist facies Schist Belt and the lower grade Central.

The Lyhamyar deposit is a large Sb deposit in the Southern Shan Plateau, Eastern Myanmar. The deposit is located in the Early Silurian Linwe Formation, occurring as syntectonic quartz-stibnite veins.

The ore body forms an irregular staircase shape, probably related to steep faulting. Based on the mineral assemblages and cross-cutting relationships, the deposit shows two mineralization stages Author: Aung Min Oo, Lv Xinbiao, Khin Zaw, Than Htay, Sun Binke, Munir Mohammed Abdalla Adam.

White Geochemistry Chapter 9: Stable Isotopes The Fractionation Factor The fractionation factor, α, is the ratio of isotope ratios in two phases: α A−B ≡ R A R B The fractionation of isotopes between two phases is also often reported as ∆.

Muehlenbachs's 99 research works with 2, citations and 4, reads, including: Origin of the high-grade Early Jurassic Brucejack epithermal Au-Ag deposits, Sulphurets Mining Camp.

Sun, T.K. Kyser, M. Stauffer, R. Kerrich and J. Lewry, Constraints on the timing of crustal imbrication in the central Trans-Hudson Orogen from single zircon Pb/Pb ages of granitoid rocks from the Pelican thrust zone, an Journal of Earth Sciences, 33,   Plutons of this age are rare in the Yukon composite terrane of south-central Alaska, but a pluton of this age (ca.

– Ma) has been recently documented in along-strike rocks in the Yukon (M. Colpron,personal commun.). Another potential distal source may be plutons of the eastern portion of the Coast Mountains batholith.

Clark M. Johnson's research works w citations reads, including: Life on a Mesoarchean marine shelf – insights from the world’s oldest known granular iron formation.

Clemens and Finger propose that “Fa 90 would be stable at ∼ times the f O 2 of FMQ” and suggest that the relatively reduced condition of the Jiuyishan granite would be satisfied by melting of an ilmenite-series granitoid; therefore, relatively low f O 2 does not unambiguously support a metasedimentary source.

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Major element and oxygen isotope geochemistry of vapour-phase garnet from the Topopah Spring Tuff at Yucca Mountain, Nevada, USA. Twenty vapour-phase garnets were studied in two samples of the Topopah Spring Tuff of the Paintbrush Group from Yucca Mountain, in southern Nevada.

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Fogel, Bianca Fréchette, Roxane Bowden, John T. The geochemistry and geochronology of the Proterozoic granitoid rocks from the Natal Structural and Metamorphic Province, southeastern Africa.

Rev. Brasileira de Geoci., 17, p. The sulfur isotope composition of single sulfide grains has been studied taking into account their paragenetic sequence in the samples collected from three hydrothermal fields (Logatchev, Krasnov, and Rainbow), located in the northern part of the Mid-Atlantic Ridge.

The δ34S values of sulfides are + to +6, + to +, and + to + ‰ in the Logatchev, Krasnov, and Rainbow fields. The IUGS- and UNESCO-funded International Geoscience Programme Project # (Neoproterozoic Ice Ages) was conceived to contribute towards a global synthesis of current geological data on the number, duration, extent, causes and consequences of glacial episodes during the Neoproterozoic Era.

IGCP attracted more than scientists from over 30 countries, many of whom provided their regional. A new petrogenetic model for meta-granitic rocks in the central and southern Menderes Massif – W Turkey: Implications for Cadomian crustal evolution within the Pan-African mega-cycle.

Precambrian Research, Vol. Issue., p. Neodymium Isotope Geochemistry An Introduction. Home; Neodymium Isotope Geochemistry An Introduction; Neodymium Isotope Geochemistry An Introduction. pasax; ; 0 Comment. The Banzhusi granite porphyry is located in the Xiong’ershan area, East Qinling orogenic belt (EQOB).

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Aquamarine of distinctly dark blue colour was discovered during the summer of in the Pelly Mountains, southern Yukon Territory, Canada. The beryl is found within quartz veins that fill sigmoidal tension gashes, which cut a Mississippian syenite.

The True Blue showing is differentiated from other beryl occurrences in the northern Cordillera by the colour of the beryl, host rock, mineral. A contribution to the geochronology of the Precambrian basement of central south Norway \/ Fernando Corfu -- The Sesia-Lanza zone, a slice of subducted continental crust \/ G.V.

Dal Piaz, J.C. Hunziker, and W.B. Stern -- Zircons from the mantle \/ Gordon L. Davis -- The origin of anorthosites: geochemical and isotopic constraints \/ D. Geochemistry, geochronology and Sr–Nd–Hf isotopes of two types of Early Cretaceous granite porphyry dykes in the Sulu orogenic belt, eastern China.

Song-Jie Wang, a b Hans-Peter Schertl, c a Yu-Mao Pang a b. a College of Earth Science and Engineering, Shandong University of Science and Technology, QingdaoChina.

The causal mechanisms of global glaciations are poorly understood. The transition to a Neoproterozoic Snowball Earth after more than 1 Gy without glaciation represents the most dramatic episode of climate change in the geological record. Here we present new Re-Os geochronology, which, together with existing U-Pb ages, reveal that the glacial period in northwest Canada lasted ∼55 My.

The Bulage Pb–Zn deposit is a typical hydrothermal vein‐type deposit located in the central part of the EDMB (Figure 1b) and was discovered in by the Inner Mongolia Shandong Gold Geological Minerals Survey, Chifeng, China.

The mineralization is thought to have been controlled by fractures and is spatially closely related to quartz diorite, but the genetic relationship between the.

Isotope Geochemistry: 2: Research Associate: School of Environmental Sciences: Jawaharlal Nehru University, New Delhi: Geochemistry: 3: Post-doctoral fellow: Department of Earth and Space Sciences: State University of New York at Stony Brook, USA: Isotope Geochemistry.

The S and I granitoid rocks from southeastern Australia are readily distinguished by their oxygen isotope ratios and, in addition, a good correlation exists between the â ¢D values and water contents of these rocks (O!Neil anâ ¢ in southern Nevada.

depleted rocks FQrester and Taâ ¢lor of Mull (, ) made detailed studies of the â. Neodymium Isotope Geochemistry An Introduction. Posted on by beli. The applied isotope geochemistry (aig) working group of the international association of geochemistry (iagc) organizes highly successful biennial conferences focused broadly on the emerging field of applied isotope geochemistry and biogeochemistry.

Most recently, aig was held in conjection with wri in tomsk, russia as part of the 1st iagc. Geology of the eastern Lake Laberge area (E), south-central Yukon.

Yukon Geological Survey, Open Filep. Manor, M.J., and Piercey, S.J., Geochemistry of Devono–Mississippian volcanic and intrusive rocks of the Finlayson Lake district, Yukon-Tanana terrane, Yukon.

Neodymium isotope geochemistry of felsic volcanic and intrusive rocks from the Yukon-Tanana terrane in the Finlayson Lake region, Yukon, Canada.

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