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Artykuły w czasopismach na temat "Crustal fluids"
Li, Jiahao, Xing Ding i Junfeng Liu. "The Role of Fluids in Melting the Continental Crust and Generating Granitoids: An Overview". Geosciences 12, nr 8 (22.07.2022): 285. http://dx.doi.org/10.3390/geosciences12080285.
Pełny tekst źródłaNesbitt, Bruce E. "Electrical resistivities of crustal fluids". Journal of Geophysical Research: Solid Earth 98, B3 (10.03.1993): 4301–10. http://dx.doi.org/10.1029/92jb02576.
Pełny tekst źródłaFyfe, W. S. "Fluids, tectonics and crustal deformation". Tectonophysics 119, nr 1-4 (październik 1985): 29–36. http://dx.doi.org/10.1016/0040-1951(85)90031-9.
Pełny tekst źródłaBeaudoin, Georges, D. F. Sangster i C. I. Godwin. "Isotopic evidence for complex Pb sources in the Ag–Pb–Zn–Au veins of the Kokanee Range, southeastern British Columbia". Canadian Journal of Earth Sciences 29, nr 3 (1.03.1992): 418–31. http://dx.doi.org/10.1139/e92-037.
Pełny tekst źródłaCheng, Yuanzhi, Yanlong Kong, Zhongxing Wang, Yonghui Huang i Xiangyun Hu. "Crustal Electrical Structure of the Ganzi Fault on the Eastern Tibetan Plateau: Implications for the Role of Fluids in Earthquakes". Remote Sensing 14, nr 13 (22.06.2022): 2990. http://dx.doi.org/10.3390/rs14132990.
Pełny tekst źródłaYardley, B. W. D. "The Ligand Chemistry of Crustal Fluids". Mineralogical Magazine 58A, nr 2 (1994): 994–95. http://dx.doi.org/10.1180/minmag.1994.58a.2.252.
Pełny tekst źródłaTagirov, Boris, i Jacques Schott. "Aluminum speciation in crustal fluids revisited". Geochimica et Cosmochimica Acta 65, nr 21 (listopad 2001): 3965–92. http://dx.doi.org/10.1016/s0016-7037(01)00705-0.
Pełny tekst źródłaSaxena, S. K., i Y. Fei. "Fluids at crustal pressures and temperatures". Contributions to Mineralogy and Petrology 95, nr 3 (marzec 1987): 370–75. http://dx.doi.org/10.1007/bf00371850.
Pełny tekst źródłaGudelius, Dominik, Sonja Aulbach, Hans-Michael Seitz i Roberto Braga. "Crustal fluids cause strong Lu-Hf fractionation and Hf-Nd-Li isotopic provinciality in the mantle of continental subduction zones". Geology 50, nr 2 (2.11.2021): 163–68. http://dx.doi.org/10.1130/g49317.1.
Pełny tekst źródłaChen, Chien-Chih, Chow-Son Chen i Chiou-Fen Shieh. "Crustal Electrical Conductors, Crustal Fluids and 1999 Chi-Chi, Taiwan, Earthquake". Terrestrial, Atmospheric and Oceanic Sciences 13, nr 3 (2002): 367. http://dx.doi.org/10.3319/tao.2002.13.3.367(cce).
Pełny tekst źródłaRozprawy doktorskie na temat "Crustal fluids"
Ballentine, Christopher John. "He, Ne, and Ar isotopes as tracers in crustal fluids". Thesis, University of Cambridge, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.387053.
Pełny tekst źródłaWilkinson, Jamie John. "The origin and evolution of Hercynian crustal fluids, South Cornwall, England". Thesis, University of Southampton, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.252719.
Pełny tekst źródłaBlythe, Lara S. "Understanding Crustal Volatiles : Provenance, Processes and Implications". Doctoral thesis, Uppsala universitet, Berggrundsgeologi, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-171486.
Pełny tekst źródłaDantas, Cardoso Carolina. "Isotopic tracing of fluids sources and transfer in the crust". Electronic Thesis or Diss., Université de Lorraine, 2023. http://www.theses.fr/2023LORR0139.
Pełny tekst źródłaNoble gases occur in low concentration on Earth and are relatively inert, making them good tracers of fluid interactions. Contrary to most stable isotopes or major elements commonly used as geochemical tracers, noble gases are less susceptible to water/rock interactions modifications. Due to their widely variable ratios among the three main Earth reservoirs (mantle, continental crust, and atmosphere), the He and Ne isotopic systems are of particular interest, providing information on the source of fluids. The main goal of this thesis was to detect the sources of crustal and geothermal fluids in different geological and geotectonic settings with a specific emphasis on precising transport processes in the crust: : (i) isotopic monitoring and survey in North Iceland, (ii) tracing the source of He in a continental basin in Central France, and (iii) tracing the source of He in the Lake Abhe geothermal field (Djibouti). From the results reported in this thesis, helium isotopes show that mantle input is present in different geotectonic contexts, not necessarily linked to active volcanism or extension, such as the case of off-rift zones in Iceland (Chapter 4) and of the Paris Basin (Chapter 5), the latter inserted in a continental crust setting. In the Lake Abhe geothermal system (Chapter 6), the helium isotopic signature is below the one expected for this segment of the East African Rift System (EARS), where an enriched plume-like endmember was anticipated, as observed a few kilometres away, in SW Afar (∼ 55 km) and Tendaho Graben (∼ 110 km NW). Thus, helium isotopes are a powerful tool to trace the mantle influence and transport complexities at different geological settings. This thesis is organized in seven chapters; the first three of them give background information on the different studies and the the next ones deal with the results and conclusions of such studies. Chapter 1 presents the context of the thesis, the helium isotopes systematics, and target areas. I detail the principle of helium and neon isotopes, the different applications of these systems in the study of fluids in the crust, finalizing with the presentation of the objectives of each case study. Chapter 2 lists the main sampling procedures I followed and Chapter 3 describes the different steps of helium isotope analyses, the main methodology I employed in this thesis. Chapter 4 presents the results of the investigation in North Iceland - both the isotopic survey of various systems and the time series of 3He/4He of groundwater samples from a borehole (HA-01). The results show the influence of an enriched and plume-like endmember in this off-rift zone of Iceland, via vertical transport along extinct volcanic fissure swarms. One of the fjords exhibit 3He/4He ratios lower than expected for typical mantle values in such a context, that we attribute to 4He* (radiogenic) release enhanced by seismic activity along the Dalvík lineament. We interpret the small variations we observed in the time series as a result of a local scale lateral mixing of groundwater during periods of unrest (M ≥ 5 earthquakes). Chapter 5 presents the main results of our study of the gas reservoir and its nearby springs in Nièvre, Central France. Our findings, from the various isotopic systems employed, indicate a clear yet limited mantle input (∼ 2.5%) in this segment of the continental crust, along N-S fault systems in Central France, reaching the Paris Basin. Chapter 6 reports results from the isotopic investigation performed at the Lake Abhe geothermal field and nearby regions (SW Afar and Tendaho Graben). From the results of multiple isotopic systems, we infer the Lake Abhe geothermal field source of heat is the Dama Ali volcano (∼ 30km), source of the mantle signal observed in helium and CO2, both transported by a regional aquifer fed by meteoric water. Chapter 7 summarizes the main results and conclusions of this thesis, along with the remaining questions and potential future studies
Eglinger, Aurélien. "Cycle de l'uranium et évolution tectono-métamorphique de la ceinture orogénique Pan-Africaine du Lufilien (Zambie)". Thesis, Université de Lorraine, 2013. http://www.theses.fr/2013LORR0306/document.
Pełny tekst źródłaUranium is an incompatible and lithophile element and can be used as a geochemical tracer to discuss the generation and the evolution of continental crust. This thesis, focused on the Pan-African Lufilian belt in Zambia, characterizes the U cycle for this crustal segment. Silici-clastic and evaporitic sediments have been deposited within an intracontinental rift during the dislocation of the Rodinia supercontinent during the early Neoproterozoic. U-Pb ages on detrital zircon grains in these units indicate a dominant Paleoproterozoic provenance. The same zircon grains show subchondritic epsilonHf (between 0 and -15) and yield Hf model ages between ~2.9 and 2.5 Ga. These data suggest that the continental crust was generated before the end of the Archean associated with U extraction from the mantle. This old crust has been reworked by deformation and metamorphism during the Proterozoic. U has been remobilized and re-concentrated during several orogenic cycles until the Pan-African orogeny. During this Pan-African cycle, U-Pb and REY (REE and Yttrium) signatures of uranium oxides indicate a first mineralizing event at ca. 650 Ma during the continental rifting. This event is related to late diagenesis hydrothermal processes at the basement/cover interface with the circulation of basinal brines linked to evaporites of the Roan. The second stage, dated at 530 Ma, is connected to metamorphic highly saline fluid circulations, synchronous to the metamorphic peak of the Lufilian orogeny. These fluids are derived from the Roan evaporite dissolution. Some late uranium remobilizations are described during exhumation of metamorphic rocks and their tectonic accretion in the internal zone of the Lufilian orogenic belt
Hopkinson, Laurence. "The role of aqueous fluids in crustal processes at the inter and intra-crystalline level". Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296147.
Pełny tekst źródłaAy, Erkan. "Origin of crustal reflectivity and influence of fluids and fractures on velocity at the Kola superdeep borehole". Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1453231711&sid=4&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Pełny tekst źródłaRicci, Andrea <1989>. "Geochemistry of C-bearing gas compounds in natural fluids under crustal conditions: insights into deep and shallow processes". Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2019. http://amsdottorato.unibo.it/9007/1/ricci_andrea_tesi.pdf.
Pełny tekst źródłaFichtel, Katja [Verfasser], Heribert [Akademischer Betreuer] Cypionka i Ralf [Akademischer Betreuer] Rabus. "Influence of crustal fluids on growth and activity of marine deep biosphere microbial populations / Katja Fichtel. Betreuer: Heribert Cypionka ; Ralf Rabus". Oldenburg : BIS der Universität Oldenburg, 2014. http://d-nb.info/1066873305/34.
Pełny tekst źródłaMoore, Myles Thomas. "Noble Gas and Hydrocarbon Geochemistry of Coalbed Methane Fields from the Illinois Basin". The Ohio State University, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=osu1462561493.
Pełny tekst źródłaKsiążki na temat "Crustal fluids"
National Research Council (U.S.). Geophysics Study Committee., red. The Role of fluids in crustal processes. Washington, D.C: National Academy Press, 1990.
Znajdź pełny tekst źródłaBos, Bart. Faults, fluids and friction: Effect of pressure solution and phyllosilicates on fault slip behaviour, with implications for crustal rheology. [Utrecht]: Faculteit Aardwetenschappen der Universiteit Utrecht, 2000.
Znajdź pełny tekst źródłaShmulovich, K. I., B. W. D. Yardley i G. G. Gonchar, red. Fluids in the Crust. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1226-0.
Pełny tekst źródłaD, Spudis Paul, Guest John E i United States. National Aeronautics and Space Administration., red. The dynamics of rapidly emplaced terrestrial lava flows and implications for planetary volcanism. [Washington, DC: National Aeronautics and Space Administration, 1995.
Znajdź pełny tekst źródłaAxel, Liebscher, i Heinrich Christoph A. 1953-, red. Fluid-fluid interactions. Chantilly, Va: Mineralogical Society of America, Geochemical Society, 2007.
Znajdź pełny tekst źródłaI, Shmulovich K., Yardley B. W. D i Gonchar G. G, red. Fluids in the crust: Equilibrium and transport properties. London: Chapman & Hall, 1995.
Znajdź pełny tekst źródłaCraven, James A. Electromagnetic imaging of deep fluids in Archean crust. Ottawa: National Library of Canada = Bibliothèque nationale du Canada, 1991.
Znajdź pełny tekst źródłaB, Forster C., Nesbitt Bruce E i Mineralogical Association of Canada, red. Fluids in tectonically active regimes of the continental crust. Nepean, Ont., Canada: Mineralogical Association of Canada, 1990.
Znajdź pełny tekst źródłaLarsen, C. S. Crust and spray. Minneapolis: Millbrook Press, 2010.
Znajdź pełny tekst źródłaJapan-U.S. Seminar on "Magmatic Contributions to Hydrothermal Systems" (1991 Kagoshima-shi, Japan, and Ebino-shi, Japan). Magmatic contributions to hydrothermal systems: Extended abstracts of the Japan-U.S. Seminar on "Magmatic Contributions to Hydrothermal Systems", held at Kagoshima and Ebino, November, 1991 and The behavior of volatiles in magma : abstracts of the 4th Symposium on Deep-crustal Fluids "The behavior of Volatiles in Magma", held at Tsukuba, November, 1991. Tsukuba-shi: Geological Survey of Japan, 1992.
Znajdź pełny tekst źródłaCzęści książek na temat "Crustal fluids"
Bosl, William J., i Amos Nur. "Crustal fluids and earthquakes". W Geocomplexity and the Physics of Earthquakes, 267–84. Washington, D. C.: American Geophysical Union, 2000. http://dx.doi.org/10.1029/gm120p0267.
Pełny tekst źródłaYardley, Bruce W. D., i Kirill I. Shmulovich. "An introduction to crustal fluids". W Fluids in the Crust, 1–12. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1226-0_1.
Pełny tekst źródłaThompson, A. B. "Heat, Fluids, and Melting in the Granulite Facies". W Granulites and Crustal Evolution, 37–57. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2055-2_4.
Pełny tekst źródłaSen, S. K., i A. Bhattacharya. "Granulites of Satnuru and Madras: A Study in Different Behaviour of Fluids". W Granulites and Crustal Evolution, 367–84. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2055-2_18.
Pełny tekst źródłaPirajno, Franco. "Crustal Hydrothermal Fluids and Mesothermal Mineral Deposits". W Hydrothermal Mineral Deposits, 612–91. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-75671-9_16.
Pełny tekst źródłaNewton, Robert C. "Fluids and melting in the Archaean deep crust of southern India". W High-temperature Metamorphism and Crustal Anatexis, 149–79. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-015-3929-6_7.
Pełny tekst źródłaManning, Craig E. "5. Thermodynamic Modeling of Fluid-Rock Interaction at Mid-Crustal to Upper-Mantle Conditions". W Thermodynamics of Geothermal Fluids, redaktorzy Andri Stefánsson, Thomas Driesner i Pascale Bénézeth, 135–64. Berlin, Boston: De Gruyter, 2013. http://dx.doi.org/10.1515/9781501508295-005.
Pełny tekst źródłaSheppard, Simon M. F. "The Isotopic Characterization of Aqueous and Leucogranitic Crustal Fluids". W Fluid Movements — Element Transport and the Composition of the Deep Crust, 245–63. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_22.
Pełny tekst źródłaQuesnel, Benoît, Christophe Scheffer i Georges Beaudoin. "The Light Stable Isotope (Hydrogen, Boron, Carbon, Nitrogen, Oxygen, Silicon, Sulfur) Composition of Orogenic Gold Deposits". W Isotopes in Economic Geology, Metallogenesis and Exploration, 283–328. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-27897-6_10.
Pełny tekst źródłaLühr, Birger G., Ivan Koulakov i Wiwit Suryanto. "Crustal Structure and Ascent of Fluids and Melts Beneath Merapi: Insights From Geophysical Investigations". W Merapi Volcano, 111–35. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-15040-1_5.
Pełny tekst źródłaStreszczenia konferencji na temat "Crustal fluids"
Zhong, Richen, Hao Cui, Yuling Xie, Xueyin Yuan, Joël Brugger, Huan Chen, Weihua Liu i Chang Yu. "Sulfate-Rich Crustal Fluids and REE Tranpsort". W Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.3189.
Pełny tekst źródłaMatthews, Simon, i Dimitri A. Sverjensky. "Modelling Zr Transport in Crustal and Mantle Fluids". W Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1747.
Pełny tekst źródłaTrunilina, Vera. "RARE-EARTH MINERALIZATION IN GRANITES OF THE NORTH-EAST OF THE VERKHOYANSK-KOLYMA OROGEN". W 23rd SGEM International Multidisciplinary Scientific GeoConference 2023. STEF92 Technology, 2023. http://dx.doi.org/10.5593/sgem2023/1.1/s01.17.
Pełny tekst źródłaBenson, Erin, i Alan Boudreau. "Stable and radiogenic isotopes in the Stillwater Complex, Montana: Evidence for contamination by crustal fluids". W Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12394.
Pełny tekst źródłaSpotkaeff, Cherise, Michael Rappe, Sean Jungbluth, Grieg Steward i Olivia Nigro. "Phylogenomic Analysis of Viral Genomes Assembled from Juan de Fuca Ridge Flank Basalt-Hosted Crustal Fluids". W Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2448.
Pełny tekst źródłaTeboul, Pierre-Alexandre, Neilma Lima, Eric Gaucher i Laury Araujo. "Fluid/rock interaction in extensional setting: a complex contribution from exhumed mantle and crustal fluids – Case study of the Aptian “Pre-salt” carbonates". W Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10164.
Pełny tekst źródłaSanchez-Valle, Carmen, Christina Springklee, Marion Louvel, Christian Pluckthun, Jean-Louis Hazemann i Denis Testemale. "Redox controls on the solubility of SnO2 cassiterite and the speciation of tin in crustal fluids". W Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.8251.
Pełny tekst źródłaErslev, Eric, Kate Miller, Lindsay Lowe Worthington, Megan Anderson i Gary Gray. "LARAMIDE CRUSTAL DETACHMENT IN THE ROCKIES: CORDILLERAN SHORTENING OF FLUID-WEAKENED CRUST". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383674.
Pełny tekst źródłaKuznetsov, O. L., i A. V. Karakin. "Model of crustal waveguides and concept of fluid movement in the upper crust". W Geophysics of the 21st Century - The Leap into the Future. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.38.f152.
Pełny tekst źródłaIyare, U. C., L. P. Frash, J. W. Carey, O. O. Blake i R. Ramsook. "Effect of Water Saturation on Failure Behaviour of Mudstones Under High Pressures". W 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0311.
Pełny tekst źródłaRaporty organizacyjne na temat "Crustal fluids"
Jacques, I. J., A. J. Anderson i S. G. Nielsen. The geochemistry of thallium and its isotopes in rare-element pegmatites. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328983.
Pełny tekst źródłaMatte, S., M. Constantin i R. Stevenson. Mineralogical and geochemical characterisation of the Kipawa syenite complex, Quebec: implications for rare-earth element deposits. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329212.
Pełny tekst źródłaHarris, L. B., P. Adiban i E. Gloaguen. The role of enigmatic deep crustal and upper mantle structures on Au and magmatic Ni-Cu-PGE-Cr mineralization in the Superior Province. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328984.
Pełny tekst źródłaRye, Danny M., i Edward W. Bolton. Reactive Fluid Flow and Applications to Diagenesis, Mineral Deposits, and Crustal Rocks. Office of Scientific and Technical Information (OSTI), listopad 2002. http://dx.doi.org/10.2172/899948.
Pełny tekst źródłaLasaga, A. C., i D. M. Rye. Reactive fluid flow models and applications to diagenesis, mineral deposits and crustal rocks. Office of Scientific and Technical Information (OSTI), styczeń 1992. http://dx.doi.org/10.2172/6973243.
Pełny tekst źródłaLasaga, A. C., i D. M. Rye. Reactive fluid flow models and applications to diagenesis, mineral deposits and crustal rocks. Office of Scientific and Technical Information (OSTI), sierpień 1993. http://dx.doi.org/10.2172/10173566.
Pełny tekst źródłaLasaga, A. C., i D. M. Rye. Reactive fluid flow models and applications to diagenesis, mineral deposits and crustal rocks. Progress report. Office of Scientific and Technical Information (OSTI), październik 1992. http://dx.doi.org/10.2172/10183433.
Pełny tekst źródłaDutrow, Barbara. Thermal-chemical-mechanical feedback during fluid-rock interactions: Implications for chemical transport and scales of equilibria in the crust. Office of Scientific and Technical Information (OSTI), sierpień 2008. http://dx.doi.org/10.2172/935785.
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