Добірка наукової літератури з теми "Sodic metasomatism"
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Статті в журналах з теми "Sodic metasomatism"
Gu, Shangyi, Guojiang Wan, and Jianquan Mao. "Sodic metasomatism in a dacite weathering profile in Pinxiang, Guangxi, China." Chinese Journal of Geochemistry 26, no. 4 (November 2007): 434–38. http://dx.doi.org/10.1007/s11631-007-0434-7.
Повний текст джерелаAlbino, George V. "Sodium metasomatism along the Melones Fault Zone, Sierra Nevada Foothills, California, USA." Mineralogical Magazine 59, no. 396 (September 1995): 383–99. http://dx.doi.org/10.1180/minmag.1995.059.396.02.
Повний текст джерелаHellebrand, Eric, and Jonathan E. Snow. "Deep melting and sodic metasomatism underneath the highly oblique-spreading Lena Trough (Arctic Ocean)." Earth and Planetary Science Letters 216, no. 3 (November 2003): 283–99. http://dx.doi.org/10.1016/s0012-821x(03)00508-9.
Повний текст джерелаCinelu, S., and M. Cuney. "Sodic metasomatism and U–Zr mineralization: A model based on the Kurupung batholith (Guyana)." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A103. http://dx.doi.org/10.1016/j.gca.2006.06.120.
Повний текст джерелаFiannacca, Patrizia, Miguel A. S. Basei, Rosolino Cirrincione, Antonino Pezzino, and Damiano Russo. "Water-assisted production of late-orogenic trondhjemites at magmatic and subsolidus conditions." Geological Society, London, Special Publications 491, no. 1 (February 6, 2019): 147–78. http://dx.doi.org/10.1144/sp491-2018-113.
Повний текст джерелаNardi, Lauro V. S., Jorge Plá-Cid, Maria de Fátima Bitencourt, and Larissa Z. Stabel. "Geochemistry and petrogenesis of post-collisional ultrapotassic syenites and granites from southernmost Brazil: the Piquiri Syenite Massif." Anais da Academia Brasileira de Ciências 80, no. 2 (June 2008): 353–71. http://dx.doi.org/10.1590/s0001-37652008000200014.
Повний текст джерелаKrátký, Ondřej, Vladislav Rapprich, Martin Racek, Jitka Míková, and Tomáš Magna. "On the Chemical Composition and Possible Origin of Na–Cr-Rich Clinopyroxene in Silicocarbonatites from Samalpatti, Tamil Nadu, South India." Minerals 8, no. 8 (August 17, 2018): 355. http://dx.doi.org/10.3390/min8080355.
Повний текст джерелаAlmeida, Delia Del Pilar M. de, Vitor P. Pereira, Adriane Machado, Henrique Zerfass, and Ricardo Freitas. "Late sodic metasomatism evidences in bimodal volcanic rocks of the Acampamento Velho Alloformation, Neoproterozoic III, southern Brazil." Anais da Academia Brasileira de Ciências 79, no. 4 (December 2007): 725–37. http://dx.doi.org/10.1590/s0001-37652007000400012.
Повний текст джерелаMiyazoe, T., M. Enami, T. Nishiyama, and Y. Mori. "Retrograde strontium metasomatism in serpentinite mélange of the Kurosegawa Zone in central Kyushu, Japan." Mineralogical Magazine 76, no. 3 (June 2012): 635–47. http://dx.doi.org/10.1180/minmag.2012.076.3.14.
Повний текст джерелаFedo, C. "Potassic and sodic metasomatism in the Southern Province of the Canadian Shield: Evidence from the Paleoproterozoic Serpent Formation, Huronian Supergroup, Canada." Precambrian Research 84, no. 1-2 (August 1997): 17–36. http://dx.doi.org/10.1016/s0301-9268(96)00058-7.
Повний текст джерелаДисертації з теми "Sodic metasomatism"
Silcock, D. R. "Mineralogy, petrography and stratigraphic analysis of gold-hosting units, Oberon prospect, Tanami Region, N.T." Thesis, 2011. http://hdl.handle.net/2440/97928.
Повний текст джерелаThe newly-discovered Oberon gold deposit, Tanami Goldfields, represents a Paleoproterozoic mesothermal orogenic gold deposit hosted in the Tanami Group. Recent drilling has intersected extensive mineralised zones at various positions within the lower stratigraphy. Studying drillhole TID0065 using a number of different techniques, the project set out to understand the lithostratigraphy of the sequence and its relationship with gold mineralisation, constraints on depositional environments and associated hydrothermal alteration, along with correlations to other deposits in the region. The sequence consists of a dolomitic mudstone, grading up into a phyllite, with a siltstone protolith. This meta-sandstone represents the main host for gold mineralisation and is similar to that seen in the Coyote deposit. Conformably overlying this unit is a rapidly-deposited well-defined turbidite sequence. Gold is also hosted in the overlying Boudin Chert unit, a graphitic, pyrite rich rock that has hosts distinctive diagenetic boudin structures. The Boudin Chert represents a transition into an anoxic sediment-starved environment. Increased clastic input along with a drop in sea level further defines the rest of the sequence, with a siltstone, mudstone and sandstone package and intercalated volcaniclastics and ignimbrites noted in the upper part of the drillhole extending into the Killi Killi Formation. Mineralisation is predominantly stratabound but thrust stacking provides a secondary control to the gold distribution pattern. Gold mineralisation is associated with Na-enrichment and K-depletion; albite is the dominant feldspar in the gold-hosting assemblage. This demonstrates a possible sodic metasomatism of an alkali assemblage. The wide variation in chlorite composition, expressed as varying proportions of chamosite and clinochlore end-members between lithologies, is suggestive of multiple fluid phases and/or alteration events, including possible „seafloor metamorphism‟ prior to hydrothermal activity. Primary alteration in the deposit is represented by an earlier chlorite-sericite assemblage and a later stage calcite-dolomite alteration in certain lithologies at the base of the sequence. Using chlorite thermometry, peak metamorphic temperatures were calculated to be at 366 ± 21 °C (i.e. greenschist facies); conditions reach amphibolite grade less than a kilometre away. Electron probe microanalysis suggests the mineralising fluids were volatile-rich, as demonstrated by the high F content of biotite and apatite. Future exploration potential for deposits of this type should focus on identification of Fe-enriched turbiditic sequences, chlorite-albite-muscovite assemblages and the presence of arsenopyrite. Graphitic oxygen-deprived beds enriched in a range of trace elements with strong pyrite alteration are also good indicators of gold mineralisation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Тези доповідей конференцій з теми "Sodic metasomatism"
Sommer, Holger, Dorrit Jacob, Klaus Regenauer-Lieb, and Laure Martin. "Petrography, petrology and mineralogy of eclogite nodules from the Jwaneng Diamond Mine, Botswana. An approach documented by mantle metasomatism, kimberlite emplacement and finally by super sonic uplift of the diamondiferous host rocks." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7461.
Повний текст джерела