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Gotowe bibliografie tematyczne / Amphibole chemistry

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Gotowa bibliografia na temat „Amphibole chemistry”

Autor: Grafiati

Data publikacji: 3 czerwca 2025

Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Amphibole chemistry"

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Ustalić, Samir, Ondrej Nemec, Stanislava Milovská, et al. "Amphibole Group Minerals in the Ozren Massif Ophiolites of Bosnia and Herzegovina as Petrogenetic Indicators." Minerals 14, no. 3 (2024): 239. http://dx.doi.org/10.3390/min14030239.

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The Ozren ophiolite complex (OOC) of the Dinaridic Ophiolite Belt is one of the six ophiolite complexes in Bosnia and Herzegovina. This paper deals with the mineral chemistry of amphiboles determined by electron probe micro-analysis and micro-Raman spectroscopy. The detected amphibole generations and types in mafic, ultramafic, and metamorphic rocks suggest a polystage evolution and are therefore useful petrogenetic indicators of the investigated OOC. Most gabbroic rocks and dolerites contain primary magmatic amphibole1 (magnesio-hornblende to pargasite, occasionally hastingsite) and prismatic

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Zhang, Xiaoli, Jinxian He, Zeqiang Ren, Taotao Zhou, Wenjie Cao, and Ben Xu. "Analysis of the Submicrostructural Deformation of Amphibole in a Ductile Shear Zone Based on the TEM Technique." Journal of Nanoscience and Nanotechnology 21, no. 1 (2021): 765–71. http://dx.doi.org/10.1166/jnn.2021.18466.

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Deformed amphibole in the plagioclase amphibolite mylonite of the Guandi Complex, Xishan, Beijing, is the research object in this study. The amphibole nanodeformation under the middle crust was analyzed using microstructural analysis and high-resolution transmission electron microscopy (TEM). Microscope observations show that the amphibolite deformations in the plagioclase amphibolite mylonite are δ and σ type porphyroclasts, and the porphyroclast tail is composed of new long-columnar crystals. Using transmission electron microscopy (TEM, and this acronyms would be defined only once), the auth

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Singh, Ankita A., D. Prakash, B. P. Singh, C. K. Singh, Manoj K. Yadav, and Rajeev K. Pandey. "Mineral Chemistry and IMA Nomenclature of Amphibole Minerals of Amphibolite Sills from Chhotanagpur Granite Gneiss Complex (CGGC), Southern Sonbhadra, Central India." Journal Of The Geological Society Of India 100, no. 5 (2024): 674–82. http://dx.doi.org/10.17491/jgsi/2024/173890.

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ABSTRACT In southern part of Sonbhadra District, near the Rihand Dam, low to medium grade amphibolites of Paleoproterozoic age are exposed. The outcrops are in the form of sills that occur at places in the Chhotanagpur Granite Gneiss Complex (CGGC). The essential mineralogical constituents of the amphibolite are amphibole-plagioclase-chlorite-biotite-iron oxides. Based on the mineral chemistry and interpretation as per the international mineralogical association (IMA) nomenclature scheme, amphiboles in the analysed amphibolite rock samples have been identified as magnesio-hornblende, magnesio-

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Rao, Rameshwar, and Hakim Rai. "Mineral chemistry of eclogites to investigate the evolutionary metamorphic history of UHP rocks from Tso-Morari region, Ladakh, India." Journal of Nepal Geological Society 40 (December 1, 2010): 13–20. http://dx.doi.org/10.3126/jngs.v40i0.23592.

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Micro textures of metabasics from the Tso-Morari region, Ladakh were studied in order to understand the evolutionary metamorphic history of eclogites. The mineral chemistry, paragenesis of mineral inclusions in garnet, and zoning in omphacite, garnet and amphibole suggest three main metamorphic stages: (i) an eclogite stage with late blueschist facies metamorphism, (ii) a medium-pressure amphibolite facies stage, and (iii) a low-pressure amphibolite to greenschist facies stage. The high Si content in phengite, presence of rutile besides almandine-rich garnet and omphacite in eclogites indicate

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Peretyazhko, Igor S., and Elena A. Savina. "Chemistry and Crystallization Conditions of Minerals in Metasomatized Oceanic Lithosphere and Basaltic Rocks of Govorov Guyot, Magellan Seamounts, Pacific Ocean." Minerals 12, no. 10 (2022): 1305. http://dx.doi.org/10.3390/min12101305.

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Studies have provided first detailed data on the chemistry of rock-forming, minor, and accessory minerals of Govorov Guyot volcanic rocks (basalts, trachybasalts, basaltic trachyandesites, and trachyandesites). Some basalt samples bear pargasitic amphibole and clinopyroxene xenocrysts, mantle vein fragments in xenoliths, as well as wehrlite xenoliths, which are remnants of metasomatized oceanic lithosphere. Amphiboles make up a continuous series from pargasite –Mg-hastingsite in wehrlite xenoliths and xenocrysts to Mg-hastingsite – kaersutite end-members in phenocrysts and microlites of basalt

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Green, Carlin J., Robert R. Seal, Nadine M. Piatak, William F. Cannon, Ryan J. McAleer, and Julia A. Nord. "Metamorphic amphiboles in the Ironwood Iron-Formation, Gogebic Iron Range, Wisconsin: Implications for potential resource development." American Mineralogist 105, no. 8 (2020): 1259–69. http://dx.doi.org/10.2138/am-2020-7211.

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Abstract The Paleoproterozoic Ironwood Iron-Formation, a Superior-type banded iron formation located in the western Gogebic Iron Range in Wisconsin, is one of the largest undeveloped iron ore resources in the United States. Interest in the development of this resource is complicated by potential environmental and health effects related to the presence of amphibole minerals in the Ironwood, a consequence of Mesoproterozoic contact metamorphism. The presence of these amphiboles and their contact metamorphic origin have long been recognized; however, recent interest in this resource has highlight

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Mihailova, Boriana, Giancarlo Della Ventura, Naemi Waeselmann, Simone Bernardini, Wei Xu, and Augusto Marcelli. "Polarons in Rock-Forming Minerals: Physical Implications." Condensed Matter 7, no. 4 (2022): 68. http://dx.doi.org/10.3390/condmat7040068.

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The existence of thermally-activated quasiparticles in amphiboles is an important issue, as amphiboles are among the main hydrous complex silicate minerals in the Earth’s lithosphere. The amphibole structure consists of stripes of 6-membered TO4-rings sandwiching MO6 octahedral slabs. To elucidate the atomistic origin of the anomalous rock conductivity in subduction-wedge regions, we studied several Fe-containing amphiboles with diverse chemistry by using in situ, temperature-dependent, polarised Raman spectroscopy. The occurrence of resonance Raman scattering at high temperatures unambiguousl

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Lyalina, L. M., Ya A. Pakhomovsky, J. A. Mikhailova, and E. A. Selivanova. "Amphibole Supergroup Minerals in the Lovozero Alkaline Massif (Kola Peninsula)." Zapiski RMO (Proceedings of the Russian Mineralogical Society) CLII, no. 6 (2023): 1–44. http://dx.doi.org/10.31857/s0869605523060023.

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On the base of published data and results of original researches, there were revealed 21 mineral species of the amphibole supergroup minerals in the Lovozero alkaline massif (Kola peninsula, Russia). Among them, 11 species belong to sodium amphiboles, 4 species are sodium-calcium amphiboles and 6 species – calcium ones. Sodium amphiboles are widely present in alkaline rocks of all complexes in the Lovozero massif – layered, eudialyte, and poikilitic complexes, in pegmatites and hydrothermal veins, as well as in roof xenoliths of volcanoclastic rocks of the trap formation. Magnesio-arfvedsonite

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Riyaz Ulla, M. S., A. M. Pathan, and P. Maaskant. "The Characterization of Metamorphic Facies of Metabasalts of Hutti Greenstone Belt." Journal Geological Society of India 47, no. 5 (1996): 547–54. http://dx.doi.org/10.17491/jgsi/1996/470504.

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Abstract The Hutti greenstone belt, containing several promising gold deposits is predominantly composed of metavolcanics represented by basalt with minor felsic volcanics and metasediments. Basalt has undergone regional metamorphism as indicated by the presence of characteristic metamorphic mineral assemblage of plagioclase, amphibole and chlorite. Electron microprobe studies are carried out on these minerals to study the chemistry and the mineral reactions in the rock. The analytical data indicate that plagioclase is andesine, amphibole is magnesio-hornblende and chlorite is ripidolite. The

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Drakoulis, A., A. Koroneos, T. Soldatos, and L. Papadopoulou. "Mineralogy and chemistry of amphiboles and thermobarometry of Papikion Mt pluton, Rhodope, Northern Greece." Bulletin of the Geological Society of Greece 47, no. 1 (2013): 373. http://dx.doi.org/10.12681/bgsg.11012.

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Papikion Mt pluton which intrudes Kardamos Dome, consists of biotite (Bi), hornblende (Hbl) and biotite-hornblende (Bi-Hbl) bearing rock types. In this work the relationship among the amphiboles of each Hbl-bearing rock type is studied. Moreover, their minimum crystallization pressure and temperature are estimated. The amphiboles of the Hbl granodiorite (GRD), the Bi-Hbl diorite (DR) and the Hbl diorite (DR) are classified mainly as magnesiohornblende and ferrohornblende and the amphiboles of the Bi-Hbl GRD as ferroedenite and hanstingsite. It is to note that some samples contain amphibole cry

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Rozprawy doktorskie na temat "Amphibole chemistry"

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Haley, Maureen Y. "Mineralogical Perspectives: Using Mineral Chemistry to Unravel the Magmatic Architecture of Granitic Batholiths." Miami University / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=miami1547567947436507.

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Pacella, Alessandro. "Cristallochimie et réactivité de surface d'amphiboles fibreuses d'intérêt environnemental et sanitaire." Phd thesis, Université Pierre et Marie Curie - Paris VI, 2009. http://tel.archives-ouvertes.fr/tel-00814192.

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Ce travail de thèse concerne la caractérisation physico-chimique et structurale de fibres minérales et la compréhension de mécanismes chimiques et moléculaires qui peuvent amorcer des pathologies spécifiques relatives à leur inhalation. En particulier, dans ce travail on s'est concentrés sur la fluoro-édénite, une amphibole naturelle d'origine volcanique découverte récemment à Biancavilla (Sicile), en comparaison avec d'autres fibres minérales, comme les trémolites et le chrysotile. La première partie de cette thèse concerne l'étude minéralogique, chimique et morphologique des fibres naturelle

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PACELLA, Alessandro. "Crystal-chemistry and reactivity of fibrous amphiboles of environmental and health interest." Doctoral thesis, 2008. http://hdl.handle.net/11573/404335.

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La caratterizzazione cristallochimica di fibre minerali, in particolar modo di anfiboli fibrosi, risulta di grande interesse, non solo per l’aspetto mineralogico, ma anche e soprattutto per quello ambientale e sanitario. I minerali fibrosi si presentano nelle rocce ospiti solitamente associati in fasci più o meno compatti, anche se in alcuni casi possono presentarsi sciolti nei materiali geologici, come per es. nel recente rinvenimento dell’anfibolo fluoro-edenite nei prodotti vulcanici di Biancavilla, CT, nei quali il minerale fibroso si presenta disperso nel materiale fine che lo ospita, e

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Chiu, Cong-Siang, and 邱琮翔. "The Contact Relationship between Amphibolite with Glaucophane and Metabasite and their Mineral Chemistry." Thesis, 2009. http://ndltd.ncl.edu.tw/handle/b46zw2.

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碩士<br>國立中央大學<br>地球物理研究所<br>97<br>Yuli belt is a typical geologic province of high pressure minerals. Amphibolites with glaucophane inclusions contacting with metapillow is quite ynusual. In this study, we use petrography and mineral chemistry to construct these rocks and to define their evolutions. According to the petrographic observation, mineral constructions of metabasite are epidote, chlorite, quartz, albite, actinolite, muscovite, calcite, and sphene. Mineral compositions of Garnet-Epidote Amphibolite are garnet, amphibole, epidote, quartz, calcite, chlorite, apatite, and albite. Some am

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Uvarova, Yulia A. "Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks." 2008. http://hdl.handle.net/1993/21323.

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Książki na temat "Amphibole chemistry"

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C, Hawthorne Frank, Mineralogical Society of America, and Accademia nazionale dei Lincei, eds. Amphiboles: Crystal chemistry, occurrence, and health issues. Mineralogical Society of America, 2007.

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Ernst, W. G. Amphiboles: Crystal Chemistry Phase Relations and Occurrence. Springer London, Limited, 2012.

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Ernst, W. G. Amphiboles: Crystal Chemistry Phase Relations and Occurrence. Springer, 2012.

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Mottana, Annibale, Frank C. Hawthorne, Roberta Oberti, and Giancarlo Della Ventura. Amphiboles: Crystal Chemistry, Occurrence, and Health Issues. de Gruyter GmbH, Walter, 2018.

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AMPHIBOLES: Crystal Chemistry, Occurrence, and Health Issues, Rimg. Mineralogical Society of Amer, 2007.

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Części książek na temat "Amphibole chemistry"

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Hawthorne, Frank C., and Roberta Oberti. "1. Amphiboles: Crystal Chemistry." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana. De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-002.

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Seal, Robert R., Jeannie M. Kornfeld, Allen L. Meier, and Jane M. Hammarstrom. "Geochemical Settings of Mine Drainage in the Vermont Copper Belt." In Part I. Proterozoic Iron and Zinc Deposits of the Adirondack Mountains of New York and the New Jersey Highlands Part II. Environmental Geochemistry and Mining History of Massive Sulfide Deposits in the Vermont Copper Belt. Society of Economic Geologists, 2001. http://dx.doi.org/10.5382/gb.35.18.

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Abstract Elizabeth and Ely, which exploited Besshi-type massive sulfide deposits, are the two largest abandoned mines in the Vermont copper belt. The ore mineralogy of the deposits and their mine wastes are dominated by pyrrhotite with minor chalcopyrite and sphalerite. Gangue minerals include quartz, muscovite, biotite, amphibole, and minor carbonate. The watersheds of the Vermont copper belt away from the mines are characterized by neutral waters, with significant alkalinity and hardness due to the presence of carbonate rocks in the watersheds. The Elizabeth mine site discharges into the Wes

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Larson, Peter B. "Geochemistry of the Alteration Pipe at the Bruce Cu-Zn Volcanogenic Massive Sulfide Deposit, Arizona." In Proterozoic Ore Deposits of the Southwestern U.S. Society of Economic Geologists, 1987. http://dx.doi.org/10.5382/gb.01.15.

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Abstract The Bruce volcanogenic massive sulfide deposit is a conformable lens which lies at an andesite-rhyolite contact within the 1.7- to 1.0-b.y.-old Yavapai Series exposed south of Bagdad, Arizona. The upper part of a funnel-shaped alteration pipe replaces andesite within the stratigraphic footwall of the deposit. This pipe can be divided into three zones based on characteristic mineralogy: a chlorite zone consisting of chlorite (40–90 wt %%) and quartz completely replaces the andesite in the central part of the pipe. A sericite zone containing subequal amounts of chlorite, sericite, and q

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Baird, Graham B., Fawna J. Korhonen, and Kevin R. Chamberlain. "Pressure-temperature-deformation-time path for the Seve Nappe Complex, Kebnekaise Massif, Arctic Swedish Caledonides." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2554(12).

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ABSTRACT The Seve Nappe Complex in the Scandinavian Caledonides records a range of peak metamorphic conditions and timings. To better understand pressure-temperature-deformation-time differences throughout the complex and possible tectonic scenarios, metamorphosed mafic rocks within the Tarfala Valley of the Kebnekaise Massif (Sweden) were investigated using integrated petrologic and geochronologic techniques. Thermodynamic modeling of two samples using domainal and whole-rock compositions integrated with mineral chemistry, mineral textures, and titanite and zircon U-Pb geochronology constrain

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Streszczenia konferencji na temat "Amphibole chemistry"

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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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Green, Carlin J., Robert R. Seal, William F. Cannon, Nadine M. Piatak, and Ryan J. McAleer. "VARIATIONS IN AMPHIBOLE CHEMISTRY IN THE IRONWOOD IRON-FORMATION, GOGEBIC IRON RANGE, WISCONSIN, USA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303051.

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Green, Carlin J., Robert R. Seal, Nadine M. Piatak, and William F. Cannon. "MORPHOLOGICAL CHARACTERIZATION AND MINERAL CHEMISTRY OF AMPHIBOLES IN THE IRONWOOD IRON-FORMATION, GOGEBIC IRON RANGE, WISCONSIN, USA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283354.

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Raporty organizacyjne na temat "Amphibole chemistry"

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Ames, D. E., and G. Tuba. Epidote-amphibole and accessory phase mineral chemistry as a vector to low-sulphide platinum group element mineralization, Sudbury: laser ablation ICP-MS trace element study of hydrothermal alteration. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296695.

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Ames, D. E., I. M. Kjarsgaard, and J. A. R. Stirling. Mineral chemistry and x-ray diffraction database of greenschist- to amphibolite-facies assemblages in the Hidden and Louis formations, Paleoproterozoic Flin Flon Domain. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289261.

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