Relevant bibliographies by topics / Schist belt

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Schist belt'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 July 2025

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Journal articles on the topic "Schist belt"

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Bhat, S. S., A. Bhattacharya, H. C. Dasgupta, and D. Dasgupta. "Petrochemistry of a Gametiferrous Chlorite Schist Horizon from the Sandur Schist Belt, Karnataka." Journal Geological Society of India 45, no. 5 (1995): 539–46. http://dx.doi.org/10.17491/jgsi/1995/450505.

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Abstract Petrology and mineral chemistry of garnetiferrous chlorite schists belonging to Deogiri formation in the Sandur schist belt have been studied. Mineral assemblages and chemical data on muscovite, biotite, chlorite, garnet from the Deogiri chlorite schists indicate low grade regional metamorphism under greenschist facies condition. Mineralogy of the metabasics associated with Deogiri chlorite schists and with the overlying Donimalai formation in this region, except near the peripheral contacts, also suggest greenschist facies metamorphism for the schist belt. Mineralogy and chemistry of
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Banerjee, D. C., N. Ranganath, P. B. Maithani, and K. M. V. Jayaram. "Rare Metal-Bearing Pegmatites in Parts of Southern Karnataka, India." Journal Geological Society of India 30, no. 6 (1987): 507–13. http://dx.doi.org/10.17491/jgsi/1987/300605.

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Abstract Several pegmatites containing commercially viable sources of columbite-tantalite have been located in the Holenarsipur, Kdshnarajapet and Nagamangala schist belts. The pegmatites in Holenarsipur schist belt near Hassan, contain columbite-tantalite, rich in both niobium and tantalum and carry appreciable amounts of beryl. The Nagamangala schist belt is particularly rich in tantalite-bearing (Ta2O5 50-70%) pegmatites. Analysis of feldspars from the three different belts indicates that they are potassic in the Nagamangala belt while they are sodic in the case of two other belts. Trace el
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Pichamuthu, C. S. "Chitradurga Schist Belt." Journal Geological Society of India 26, no. 8 (1985): 509–10. http://dx.doi.org/10.17491/jgsi/1985/260801.

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Abdus-Salam, Maryam. "Geochemistry and mineral chemistry of quartz mica schists within Iseyin-Oyan Schist Belt, Southwestern Nigeria." Indian Journal of Science and Technology 13, no. 41 (2020): 4319–31. http://dx.doi.org/10.17485/ijst/v13i41.1628.

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Background/Objectives: The Iseyin-Oyan schist belt is made up metasedimentary rocks, gneisses, granites and pegmatite intrusions. The study was aimed at identifying the schist within this belt and assess their metamorphism, geochemical characteristics and tectonic origin. Methods: Detailed geologic field mapping was undertaken where rocks were located, studied in-situ and identified. Samples of the schist were prepared for petrographic studies. Mineralogical contents were determined using X-Ray Diffraction technique. Polished sections were studied for mineral chemistry using Scanning Electron
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Maryam, Abdus-Salam, Bolarinwa Anthony, Olatunji Akinade, et al. "Geochemistry and mineral chemistry of quartz mica schists within Iseyin-Oyan Schist Belt, Southwestern Nigeria." Indian Journal of Science and Technology 13, no. 41 (2020): 4319–31. https://doi.org/10.17485/IJST/v13i41.1628.

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Abstract <strong>Background/Objectives:</strong>&nbsp;The Iseyin-Oyan schist belt is made up metasedimentary rocks, gneisses, granites and pegmatite intrusions. The study was aimed at identifying the schist within this belt and assess their metamorphism, geochemical characteristics and tectonic origin.&nbsp;<strong>Methods</strong>: Detailed geologic field mapping was undertaken where rocks were located, studied in-situ and identified. Samples of the schist were prepared for petrographic studies. Mineralogical contents were determined using X-Ray Diffraction technique. Polished sections were s
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Omang, B. O., E. A. Asinya, E. Udinmwen, and O. P. Oyetade. "Structural framework and deformation episodes in the igarra schist belt, southwestern nigeria." Global Journal of Geological Sciences 20, no. 1 (2022): 1–17. http://dx.doi.org/10.4314/gjgs.v20i1.1.

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The structural framework of the Igarra schist belt consists of brittle (mainly fractures) and ductile (foliation, cleavage, folds, lineations, strain markers) structures. The geometry of these structures reveals two major occurrences of transpressional deformation affected the schist belt. These are an older dominantly ductile deformation with NW–SE λ1 which developed foliations, cleavage, folds, and mineral/stretching lineations deforming only the metasediments and a younger brittle–ductile, E-W tectonic shortening deformation which closed deformations in the Igarra schist belt, deforming bot
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Rama Rao, P., and V. Diyakara Rao. "Origin of Polyphase Gneisses Associated with the Krishnarajpet Greenstone Belt, Dharwar Craton." Journal Geological Society of India 43, no. 5 (1994): 539–47. http://dx.doi.org/10.17491/jgsi/1994/430505.

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Abstract Hornblende, biotite and feldspar rich gneisses (HG, BG and FG respectively), in that order of formation are associated with the Krishnarajpet schist belt in Dharwar craton, a greenstone belt coeval with, and similar to, the Holenarasipur and Nuggihalli schist belts. These gneisses show compositional differences with SiO2, K2O and Rb increasing and TiO2, Al2O3, Fe2O3, CaO, MgO, Sr, Zr and Ni decreasing from HO to SO and FG. The overall REE is more in BG (SREE = 332.90), while it is similar in HG (SREE = 173.36) and FG (SREE = 159.03) with comparable LREE/HREE ratios (BG = 12.71; HG = 1
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Raghunatha Rao, B. N. "Chitradurga Schist Belt - A Summary." Journal Geological Society of India 26, no. 8 (1985): 607–10. http://dx.doi.org/10.17491/jgsi/1985/260808.

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Suresh, R. "Early Life in the Chitradurga Schist Belt." Journal Geological Society of India 26, no. 8 (1985): 611–16. http://dx.doi.org/10.17491/jgsi/1985/260809.

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Abstract The Archean Chitradurga schist belt (&amp;gt;2600 m.y.) is ideal for the investigation of morphological and chemical remnants of early life because of the presence of distinct sedimentary units. Available data so far, has not indicated the presence of undoubted microfossils from the Chitradurga belt. Possible microfossils from the Dodguni area are the only reliable evidences of early life from the Chitradurga schist belt.
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Masquelin, Henri, Hernán Silva Lara, Leda Sánchez Bettucci, et al. "Lithologies, structure and basement-cover relationships in the schist belt of the Dom Feliciano Belt in Uruguay." Brazilian Journal of Geology 47, no. 1 (2017): 21–42. http://dx.doi.org/10.1590/2317-4889201720160119.

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ABSTRACT: This work is the result of a multiyear effort to use field geology to describe lithologies, to establish contact relationships and to create a sketch of the tectonic evolution of the Meso- to Neoproterozoic metasedimentary successions within the Schist Belt of the Dom Feliciano Belt. This low-grade metamorphic cover rests on the high-grade metamorphic basement of the La China and Las Tetas complexes. This basement is Archean-Paleoproterozoic in age. The Schist Belt is overlapped unconformably by the Barriga Negra formation. The Lavalleja complex and the Barriga Negra formation both d
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Dissertations / Theses on the topic "Schist belt"

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Omitogun, Ayotunde Allen. "Métamorphisme et structure de la zone mobile pan-africaine centrale du Nigéria ("Schist belt" d'Igarra)." Toulouse 3, 1991. http://www.theses.fr/1991TOU30275.

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La zone mobile du nigeria comprend dans la partie occidentale, des formations supracristales regroupees en entites bien definies au sein d'un complexe de gneiss et de migmatites: les schist-belts ou ceintures schisteuses. Par l'etude de la ceinture d'igarra s. C. Situee dans la partie centrale de la zone mobile, le metamorphisme pan-africain a ete defini. Dans les formations supracrustales du schist belt c'est un metamorphisme de facies amphibolite caracterise par l'association grenat-andalousite-staurotide dans les metapelites. Les conditions p/t definies par le geothermometre gt-bi et les do
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Diener, Johann F. A. "The tectono-metamorphic evolution of the Theespruit Formation in the Tjakastad Schist Belt and surrounding areas of the Barberton Greenstone Belt, South Africa." Thesis, Stellenbosch : University of Stellenbosch, 2004. http://hdl.handle.net/10019.1/16309.

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Thesis (MSc)--University of Stellenbosch, 2004.<br>ENGLISH ABSTRACT: The southern portions of the Early- to Mid-Archaean Barberton granitoid-greenstone terrain of South Africa consists of a high-grade metamorphic granitoid-gneiss terrain that is juxtaposed against the low-grade metamorphic supracrustal sequence of the Barberton Greenstone Belt. The boundary of the two different crustal domains corresponds to the Theespruit Formation, an amphibolite-facies, highly tectonized mélange of metabasites, felsic volcanics and rare, aluminous clastic sediments that occurs along the granitoidgreens
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Roberts, Todd M. "GEOCHEMICAL AND STRATIGRAPHIC ANALYSIS OF META-SEDIMENTARY ROCKS OF THE GNEISS DOME BELT, WESTERN CONNECTICUT AND MASSACHUSETTS." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin990633701.

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Tünker, Maren Edda. "Mesozoic fold structure of the Otago and alpine schist belt and its implications on the tectonic evolution of South Island, New Zealand." [S.l. : s.n.], 2002. http://deposit.ddb.de/cgi-bin/dokserv?idn=96993856X.

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Korkalo, T. (Tuomo). "Gold and copper deposits in Central Lapland, Northern Finland, with special reference to their exploration and exploitation." Doctoral thesis, University of Oulu, 2006. http://urn.fi/urn:isbn:951428108X.

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Abstract At least 30 gold deposits verified by means of one or more notable diamond drill hole results have been discovered in Central Lapland in the last 20 years, and these can be divided spatially into groups, between which the metal composition varies. The deposits contain varying amounts of sulphides and sulpharsenides as well as gold. Pyrite is the most common sulphide mineral in the gold deposits associated with volcanic rocks, and usually pyrrhotite in those associated with sedimentary rocks. The principal sulphide minerals in those connected with banded iron formations are pyrite and
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Niebling, Ulf. "Untersuchungen zum Wachstum dünner Schichten organischer Metalle aus (BEDT-TTF) 2 I 3." [S.l. : s.n.], 2001. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB9918598.

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Longino, Brando. "Entanglement: dai postulati della meccanica quantistica al teorema di Bell." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2017. http://amslaurea.unibo.it/14595/.

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In questo lavoro di tesi vengono presentati inizialmente i postulati della meccanica quantistica, passando poi alla descrizione di stati tramite vettori in uno spazio di Hilbert e, successivamente, alla descrizione tramite l’operatore densità associato al sistema. Introducendo quindi i concetti di qubit e di decomposizione di Schmidt, si mostra il fenomeno chiamato Entanglement, illustrando alcuni esempi. Nel quinto capitolo viene trattata l’Entropia di Von Neumann come stumento per quantificare l’Entanglement di un sistema, mentre nel sesto si discute il problema del paradosso EPR, acco
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Courtot, Hervé. "Les terrains volcaniques paléozoïques et les minéralisations associées dans la série métamorphique de la Brévenne. District de Sain-Bel/Chessy (Rhône)." Paris 6, 1987. http://www.theses.fr/1987PA066321.

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Kumar, Satish G. "Hydrogeology around Holenarasipur schist belt, Karnataka, India." Thesis, 2003. http://hdl.handle.net/2009/3088.

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LIN, MEI-LING, and 林楳嶺. "Petrotectonic study on the Yuli belt of Tananao schist in the Chinshuichi Area, Yuli, Hualien, Taiwan." Thesis, 1986. http://ndltd.ncl.edu.tw/handle/45459536172037368950.

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Books on the topic "Schist belt"

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R, Vearncombe J., and South Africa. Dept. of Mineral and Energy Affairs., eds. Geology, geophysics, and mineralisation of the Murchison schist belt, Rooiwater Complex, and surrounding granitoids. Dept. of Mineral and Energy Affairs, Geological Survey, Republic of South Africa, 1992.

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Rasilainen, Kalevi. Alteration geochemistry of gold occurrences in the late Archean Hattu schist belt, Ilomantsi, eastern Finland: Synopsis. Geological Survey of Finland, 1996.

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A, Nurmi Pekka, and Sorjonen-Ward Peter, eds. Geological development, gold mineralization and exploration methods in the late Archean Hattu schist belt, Ilomantsi, eastern Finland. Geologian tutkimuskeskus, 1993.

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Michniewicz, Marek. Mineralizacja cynowa w środkowej części pasma łupkowego Starej Kamienicy (Sudety zachodnie): Tin mineralization in the middle part of the Stara Kamienica schist belt (western Sudetes). Państwowy Instytut Geologiczny, 2006.

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Himmelberg, Glen R. Petrologic characterization of peletic schists in the western metamorphic belt, coast plutonic-metamorphic complex, near Juneau, southeastern Alaska. U.S. G.P.O., 1994.

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Bruce, Lockerbie D., ed. In peril on the sea: The story of Ethel Bell and her children Mary and Robert. Christian Publications, 1996.

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Shenbao, Dong. Proterozoic Glaucophane-Schist Belt and Some Eclogites of North Yangtze Craton, Central China. Taylor & Francis Group, 1996.

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The Proterozoic glaucophane-schist belt and some eclogites of north Yangtze Craton, central China. Science Press, 1996.

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Prozorov, Sergei. Carl Schmitt. Edinburgh University Press, 2018. http://dx.doi.org/10.3366/edinburgh/9781474423632.003.0008.

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The work of Carl Schmitt has been a key influence on Agamben’s work, particularly his more political writings. Especially in the Anglo-American context, the discovery of Agamben’s work after the publication of the first volume of Homo Sacer coincided with a major revival of interest in Schmitt, both of which were partly motivated by the exceptionalist tendencies in US domestic and foreign policy in the aftermath of the 9/11 attacks. At least in the first wave of reception of Agamben’s writings,1 his reinterpretation of Schmitt’s theory of sovereignty in the Foucauldian biopolitical key was the
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Agamben, Giorgio. A Jurist Confronting Himself. Edited by Jens Meierhenrich and Oliver Simons. Oxford University Press, 2016. http://dx.doi.org/10.1093/oxfordhb/9780199916931.013.36.

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This chapter was originally published as a preface to a collection of Italian translations of texts by and interviews with Carl Schmitt. It shows how each text offers an image of Schmitt that can best be seen in light of what Walter Benjamin called the "now of knowability": in a constellation formed by the decisive political problems of Schmitt’s time. The challenge these texts thus propose is akin to that of finding figures hidden in a landscape painting. The chapter argues that the hidden figures in Schmitt’s works designate those points at which their contemporary relevance is greatest. Onl
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Book chapters on the topic "Schist belt"

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Agasnalli, Chandrashekharappa, M. S. Deepak, Anupkumar G. Ekbote, and T. K. Lakkundi. "Gold Mineralization and Their Lithological Controls at Nagavi Area, Gadag Schist Belt, in Karnataka, India." In Lecture Notes in Civil Engineering. Springer Nature Singapore, 2025. https://doi.org/10.1007/978-981-96-1558-2_8.

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Olajide-Kayode, Jerry, Olugbenga Okunlola, and Akinade Olatunji. "Geochemistry and Mineral Chemistry of Amphibolites in Parts of the Proterozoic Ilesa Schist Belt, Southwestern Nigeria." In Advances in Science, Technology & Innovation. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-72547-1_71.

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Oluyede, Kehinde. "Provenance and Evolution of Alkaline Rocks of the Northern Part of Birnin Gwari Schist Belt, Northwestern Nigeria." In Geology and Natural Resources of Nigeria. CRC Press, 2024. http://dx.doi.org/10.1201/9781003454908-10.

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Sunder Raju, P. V., and R. K. W. Merkle. "Högbomite Associated with Vanadiferous–Titaniferous Magnetite Bands at Bhaktarhalli, Nuggihalli Schist Belt, Western Dharwar Craton, Karnataka, India." In Proceedings of the 10th International Congress for Applied Mineralogy (ICAM). Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-27682-8_79.

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Goswami, Sukanta, and P. K. Upadhyay. "Tectonic History of the Granitoids and Kadiri Schist Belt in the SW of Cuddapah Basin, Andhra Pradesh, India." In Tectonics and Structural Geology: Indian Context. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_8.

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Olasunkanmi, Nurudeen, Lukman Sunmonu, Moruffdeen Adabanija, Jimoh Ajadi, and Leke Sunday. "Integrating Aeromagnetic and LandsatTM 8 Data for Geologic Features of Igbeti Schist Belt, Southwestern Nigeria: Implication for Groundwater Exploration." In Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01572-5_54.

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Mitra, Sumit Kr, and Tushar Meshram. "Petrography, Origin and Geochemical Characters of the Granitoids of the Southern Part of the Nellore Schist Belt, Andhra Pradesh, India." In Petrogenesis and Exploration of the Earth’s Interior. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01575-6_14.

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Sesha Sai, V. V., S. N. Mahapatro, Santanu Bhattacharjee, Tarun C. Khanna, and M. M. Korakoppa. "Petrology and Mineral Chemistry of a Porphyritic Mafic Dyke, Jonnagiri Schist Belt, Eastern Dharwar Craton, India: Implications for Its Magmatic Origin." In Springer Geology. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-1666-1_10.

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Oluyede, Kehinde. "Rocks of the Northern Part of Kushaka Schist Belts, Northwestern Nigeria." In Geology and Natural Resources of Nigeria. CRC Press, 2024. http://dx.doi.org/10.1201/9781003454908-9.

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Murray, Peter. "The Best News Ireland Ever Got? Humanae Vitae’s Reception on the Pope’s Green Island." In The Schism of ’68. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-70811-9_12.

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Conference papers on the topic "Schist belt"

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Bonev, Nikolay. "MINERAL COMPOSITIONS OF SOME ROCK-FORMING MINERALS IN THE LOW-GRADE SEDIMENTARY AND MAFIC ROCKS, EASTERN CIRCUM-RHODOPE BELT, BULGARIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s01.14.

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The eastern Circum-Rhodope belt (CRB) is a major unit that surrounds both the Serbo-Macedonian and the Rhodope zones in the Alpine orogen of the northern Aegean region. This belt contains Triassic-Jurassic metasedimentary successions and Middle Jurassic (176-165 Ma) supra-subduction zone Evros ophiolite. The latter has experienced ocean-floor hydrothermal metamorphism or very-low to low-grade metamorphism. We report on mineral compositions of rock-forming minerals in schist and mafic rocks from the eastern CRB. Our goal is to use the mineral compositions to assess the metamorphic conditions su
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Mehta, Narinder K., Vinod S. Agarwala, Airan Perez, and K. S. Rajan. "Fluorinated Schiff Base Compound as Corrosion Inhibitor for Steel." In CORROSION 1995. NACE International, 1995. https://doi.org/10.5006/c1995-95491.

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A study to evaluate wear and corrosion inhibition, and the mode of molecular bonding of a fluorinated schiff base compound (imine compounds), a condensation reaction product of 4-fluorobenzaldehyde and 4,4'-benzidine, onto AISI 1010 steel surface was undertaken to develop a new lubricant additive for greases. Physical vapor adsorption and chemisorption techniques were used for the deposition of schiff base on the metal surface. The schiff base was found to adhere best with the physical adsorption technique. It involved heating of freshly cleaned specimens suspended over schiff base in an all-g
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Marco, Surracco, and Tilocca Maria Caterina. "FLOTATION AND MAGNETIC SEPARATION PROCESSES FOR A MINERAL OF WOLLASTONITE." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s04.56.

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This paper presents the results of laboratory processing tests conducted to explore the potential for beneficiation of a wollastonite mineral (calcium metasilicate, CaSiO3). The ore studied comes from a mineralized body located in the southern part of Sardinia (Italy), which has been studied in the past with geological surveys and sampling. In the investigated area the mineralization was very irregular. The encasing rocks consist of schist and the mineralized body is composed of wollastonite associated with limestone, garnets and silica. The sample used for treatment tests was taken from this
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Cotta, Romulo, and Robert Cottis. "Methods for the Visualisation of Electrochemical Noise Data." In CORROSION 2007. NACE International, 2007. https://doi.org/10.5006/c2007-07363.

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Abstract The use of electrochemical noise (EN) measurements for the study of corrosion processes is now well established, but it remains somewhat unclear as to the best methods to use the extract useful information from the measured time records. Many of the simpler methods are based on the calculation of statistical parameters, such as the standard deviation of current, σI, or potential, σE, and the electrochemical noise resistance, Rn. A problem with many parameters derived from EN measurements is they are inherently noisy, which can make interpretation difficult. This paper explores an alte
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Abdus-Salam, Maryam, Anthony Bolarinwa, Akinade Olatunji, Ezekiel Chinyio, and Michael Fullen. "Geochemical Investigations of Granitic Rocks within Iseyin-Oyan Schist Belt, Southwestern Nigeria." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.9217.

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Mohakul, J. P., P. H. Babu, R. Madusudanan, S. A. Khan, and S. Balakrishnan. "Regional and Deposit Scale Controls of Gold Mineralization in Chitradurga Schist Belt, Dharwar Craton, India." In Gold Mining in India: The Way Forward. The Geological Society of India, 2021. http://dx.doi.org/10.17491/cgsi/2021/165462.

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Solankar, S. N., Venkatesh Murthy N., R. B. Ganesh, and Anilkumar B. V. "Current Status of Exploration and Resources of Hutti Gold Mines, Hutti-Maski Schist Belt, Karnataka." In Gold Mining in India: The Way Forward. The Geological Society of India, 2021. http://dx.doi.org/10.17491/cgsi/2021/165467.

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Babu, M. M., A. Kumar, Mangeesh, A. P. Kumar, and M. N. Divya. "Delineation of PGE mineralization occurring with in the ultramafics in Jayachamarajapura schist belt, Tumkur district, Karnataka." In 1st Indian Near Surface Geophysics Conference & Exhibition. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201979026.

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Mohanty, M., C. Parthasarathi, and P. Mahadevappa. "Magmatic Type Platinum Mineralisation in the Mafic-Ultramafic Rocks of Nuggihalli Schist Belt, Hassan District, Karnatak." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63388.

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Фролов, Петр, Вера Ильина, Александр Завёрткин, Екатерина Климовская, and Александр Савицкий. "Karelian talc as a raw material: practical application and potential contribution to Russian mineral raw material reserves." In Mineralogical and technological appraisal of new types of mineral products. Karelian Research Center of RAS, 2019. http://dx.doi.org/10.17076/tm13_6.

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Talc is a unique natural material. Some talc-bearing rocks, e.g. soapstone, are also useful minerals. There are talc deposits on the Fennoscandian Shield. The main potential talc resources and reserves are in the Karelian Craton, which is part of the shield. Talc deposits in the Finnish extension of the craton are being mined in the Kainuu Schist Belt and soapstone deposits in the Suomussalmi-Kuhmo Greenstone Belt. The Karelian portion of the craton seems to be more promising for talc-bearing deposits, because favourable rock complexes of greenstone belts are more common there. The revival of
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Reports on the topic "Schist belt"

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Kuster, K., C. M. Lesher, and M. G. Houlé. Geology and geochemistry of mafic and ultramafic bodies in the Shebandowan mine area, Wawa-Abitibi terrane: implications for Ni-Cu-(PGE) and Cr-(PGE) mineralization, Ontario and Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329394.

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The Shebandowan Ni-Cu-(PGE) deposit occurs in the Shebandowan greenstone belt in the Wawa-Abitibi terrane. This deposit is one of a few economic Ni-Cu-(PGE) deposits in the Superior Province and one of a very few deposits worldwide that contains both Ni-Cu-(PGE) and Cr-(PGE) mineralization. The mafic-ultramafic successions in the area comprise abundant flows and sills of tholeiitic basalt and lesser Al-undepleted komatiite (MgO &amp;amp;gt;18 wt%, Al2O3/TiO2 = 15-25), the latter indicating separation from mantle sources at shallow levels. Siliceous high-Mg basalts (MgO 8-12 wt%, SiO2 &amp;amp;
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Czowalla, Lucas, Andreas Blechschmidt, Dahlia Busch, et al. Handlungsansätze zur verbesserten Verknüpfung von Fahrrad und Öffentlichem Verkehr. Goethe-Universität, Institut für Humangeographie, 2018. http://dx.doi.org/10.21248/gups.40317.

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Die Verknüpfung des Fahrrades mit dem Öffentlichen Verkehr (ÖV) kann den Umweltverbund stärken, den Übergang von einem Verkehrssystem auf das andere erleichtern und eine attraktive Alternative zum motorisierten Individualverkehr schaffen. Die vorliegende Arbeit repräsentiert den zweiten umfassenden Projektbericht innerhalb des Forschungsprojektes „Verbesserte Integration des Fahrrads in den öffentlichen Verkehr – Systematische Erschließung von Handlungsoptionen und Bewertung von Best-Practices“. Im ersten Projektbericht (ebenfalls in dieser Arbeitspapierreihe erschienen – Nr. 15) wurden die En
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Petrologic characterization of pelitic schists in the western metamorphic belt, coast plutonic-metamorphic complex, near Juneau, southeastern Alaska. US Geological Survey, 1994. http://dx.doi.org/10.3133/b2074.

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