Academic literature on the topic 'Mineralogical and Petrological'

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Journal articles on the topic "Mineralogical and Petrological"

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Kamber, Balz S., and Emma L. Tomlinson. "Petrological, mineralogical and geochemical peculiarities of Archaean cratons." Chemical Geology 511 (April 2019): 123–51. http://dx.doi.org/10.1016/j.chemgeo.2019.02.011.

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Bhukte, Pravin, Gopal Daware, Tejas Bhosale, Bhargavi Kulkarni, and Anupam Agnihotri. "Petrological Characteristics of Lateritic Bauxite Deposits of India and Their Significance in Mineral Processing." Journal of Geosciences Research 9, no. 2 (2024): 73–84. http://dx.doi.org/10.56153/g19088-024-0197-59.

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India is endowed with 3896 million tons of bauxite resources and ranking it fifth globally. The bauxite comprises various minerals such as gibbsite, boehmite, diaspore, hematite, goethite, kaolinite, quartz, anatase and rutile. India possesses abundant lateritic bauxite resources originating from parent rocks like Khondalite, Deccan trap basalt, Granite Gneiss, Sandstone, etc., each exhibiting its specific characteristics. The geotechnological evaluation of India's lateritic bauxite deposits, conducted by Jawaharlal Nehru Aluminium Research Development and Design Centre (JNARDDC), revealed the
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Zussman, J. "Minerals and the electron microscope." Mineralogical Magazine 51, no. 359 (1987): 129–38. http://dx.doi.org/10.1180/minmag.1987.051.359.14.

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AbstractThe transmission electron microscope is now used in a great variety of mineralogical and petrological contexts, The development of such applications over the past thirty years is illustrated by reference mainly to studies on serpentine and amphibole minerals.
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SELİM, HAMİT HALUK, AYKUT GÜÇTEKİN, FERHAN ŞAHİN, et al. "Mineralogical, petrological, and geochemical characteristics of Şenkaya Chrysoprase,Turkey." Turkish Journal of Earth Sciences 31, no. 2 (2022): 193–207. http://dx.doi.org/10.55730/1300-0985.1762.

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W., Minyo,, Alabi, O., Adewuyi, B., and Ola-Omole, O. "Chemical, Mineralogical, and Grindability Studies of Anka-Brabra Copper Ore." Advanced Journal of Science, Technology and Engineering 4, no. 2 (2024): 47–63. http://dx.doi.org/10.52589/ajste-y9ttlivr.

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This study examined the chemical characteristics, mineralogy, and grindability of copper ore from Anka-Brabra, Zamfara State, Nigeria. The ore was crushed, ground, and mixed to achieve a uniform sample. The ore sample was characterised using EDX-XRF, XRD, SEM, and petrological microscope. Grindability and fractional sieve analysis techniques were used to ascertain optimal grinding size through particle size distribution and the liberation size of the mineral. Results showed the main copper mineral was malachite (Cu2(CO3)(OH)2) with traces of other minerals. Analysis indicated a copper content
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Szakmány, György, Kristóf Fehér, Zsolt Kasztovszky, and Tamás Sági. "Archaeometric analyses of adze-blades on Nuku Hiva, Marquesas Islands." Archeometriai Műhely 18, no. 1 (2021): 75–88. http://dx.doi.org/10.55023/issn.1786-271x.2021-005.

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In this paper we present our results based on detailed archaeometric (mineralogical, petrological and geochemical) investigations on two flakes, originated from Nuku Hiva, Vaitehii I and Ha’ahinani sites. The main aim of these researches was to determine and characterise the raw material of the stone tools and determine or at least outline their provenances. Based on the mineralogical composition and texture the flake origined from Vaitehii I are basalt and it is very similar to the local Tekao type tholeiitic basalt. On the contrary the raw materials of the flake origined from Ha’ahinani is p
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Pratesi, Giovanni, and Annarita Franza. "Mineralogical, petrological and planetological heritage. The (Italian) story so far." Rendiconti Lincei. Scienze Fisiche e Naturali 32, no. 1 (2021): 95–116. http://dx.doi.org/10.1007/s12210-020-00970-2.

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AbstractThe goal of this work is to further increase the use, by all the stakeholders, of well-established and official cataloguing methods for the preservation, valorisation and study of naturalistic heritage. The work describes the standards of the Central Institute for Cataloguing and Documentation (ICCD) for cataloguing the Italian mineralogical, petrological and planetological heritage to the community of scientists, curators and museum practitioners. This work then provides an overview of the geoscientific heritage already catalogued through these standards and freely available for study
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Dogan-Kulahci, Gullu Deniz, Abidin Temel, and Alain Gourgaud. "Mineralogical and petrological features of the Cemilköy ignimbrite, Cappadocia, Turkey." Geochemistry 78, no. 1 (2018): 103–15. http://dx.doi.org/10.1016/j.chemer.2017.11.002.

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Tomeoka, Kazushige. "Aqueous Alteration in Hydrated Interplanetary Dust Particles." International Astronomical Union Colloquium 126 (1991): 71–78. http://dx.doi.org/10.1017/s0252921100066501.

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AbstractInterplanetary dust particles (IDPs) characterized by chondritic composition can be divided into two principal groups, anhydrous and hydrated. This paper summarizes recent results of mineralogical and petrological studies dealing with the IDPs of hydrated type. Studies on mineralogical characteristics, infrared absorption spectra, and isotopic properties of the hydrated particles have suggested that they are primitive and may contain surviving interstellar material. The hydrated IDPs consist in major part of layer silicates and resemble CI and CM carbonaceous chondrites. Mineralogical
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ZINCHUK, Nikolay. "The role of petrological, mineralogical and geochemical studies in assessing the potential diamond grade of kimberlite." Domestic geology, no. 1 (March 21, 2022): 59–70. http://dx.doi.org/10.47765/0869-7175-2022-10004.

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The focus of this study is the determination of petrological and mineralogical characteristics of kimberlite pipes with various productivity. Here we provided some examples of the appraisal of the initial substrate evolution and reconstructions of mantle sections that allowed us to suggest a possible zonation of lithosphere mantle of a kimberlite province and its diamondiferous territories.
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Dissertations / Theses on the topic "Mineralogical and Petrological"

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Bloomfield, Matthew J. "Applications of microRaman spectroscopy to the study of petrological, mineralogical and natural structural materials." Thesis, University of Leicester, 2002. http://hdl.handle.net/2381/30446.

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MicroRaman spectroscopy represents a powerful tool for the study of crystal structure and identification of materials. Despite being widely used in other areas of scientific research it has yet to become a routine analytical technique within the Earth Sciences. Case studies are used to describe the application of this technique. Using the different approaches available a variety of materials of a mineralogical and petrographic nature are used to assess the usefulness and applicability of the technique. Following a brief review of the fundamental theory of Raman scattering, a description of the
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Taylor, Richard Peter. "The development of X-ray Excited Optical Luminescence (XEOL) spectroscopic techniques for mineralogical and petrological applications." Thesis, University of St Andrews, 2013. http://hdl.handle.net/10023/3739.

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This thesis investigates the use of X-ray Excited Optical Luminescence (XEOL) and Time Resolved X-ray Excited Optical Luminescence (TR XEOL) within the Earth sciences. The project contains two primary objectives, the first of which is the design and building of a high-resolution luminescence spectroscopy facility. This includes the installation and commissioning of the facility on the I18 microfocus beamline at Diamond, the UK's national synchrotron facility. In describing the system's design and commissioning, I explore many implications of the technique. The second objective is using this ne
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Markwick, Andrew John Windsor. "Petrological, mineralogical, geochemical and geophysical studies of granulite xenoliths from beneath the European platform and northern Baltic shield." Thesis, Birkbeck (University of London), 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.444571.

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Rickard, Jason H. "Petrological and mineralogical study of Cu-Ni-PGE-bearing ores within the 100 orebody, Copper Cliff North mine, Sudbury, Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0012/MQ52404.pdf.

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Rickard, Jason H. Carleton University Dissertation Earth Sciences. "Petrological and mineralogical study of Cu-Ni-PGE-bearing ores within the 100 orebody, Copper Cliff North mine, Sudbury, Ontario." Ottawa, 2000.

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Machumele, Nkateko Jones. "A geological, petrological and mineralogical study of the UG3 chromitite seam at Modikwa Platinum Mine : significance to exploration and PGE resources." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1013553.

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The UG3 at Modikwa Platinum Mine occurs as a platiniferous, planar chromitite seam. It is stratigraphically located in the Upper Critical Zone of the Eastern Bushveld Complex. Field work study comprise of underground mapping, sampling, surface mapping, borehole core logging, microprobing and microscopic investigations carried out at the Rhodes University. The UG3 at the Modikwa Platinum Mine is about 22cm thick chromitite seam underlain by a white fine grained anorthosite and overlain by a brown medium grained feldspathic pyroxenite. It is an incomplete cyclic unit consisting of chromite and f
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Zhang, Chao [Verfasser]. "Petrological, mineralogical and geochemical investigations of late Mesozoic magmatism in Eastern China : implications for tectonic evolution and crust-mantle interaction / Chao Zhang." Hannover : Technische Informationsbibliothek und Universitätsbibliothek Hannover (TIB), 2012. http://d-nb.info/1024681157/34.

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Brown, Julian William. "A petrological, mineralogical and geochemical ore characterisation of the crater facies kimberlite bodies of the Fore a la Corne Province, Saskatchewan, Canada." Thesis, University of Exeter, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.311091.

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Malatji, Tsholofelo S. "Petrological, mineralogical and geochemical studies of Zhongchang and Yantiangou ultramafic intrusions from the Panxi region, Sichuan Province, S-W China. Metallogenic and Exploration implications." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1012951.

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The Emeishan Large Igneous Province is one of the largest igneous provinces in the world. It is marked by basaltic extrusives that vary in Ti amount, classified as high Ti and low Ti. Several mafic to ultramafic intrusions occur in the province as well as granitic intrusions. The mafic-ultramafic intrusions are associated with mineralization; large layered utlramafic intrusions bearing Fe-Ti-V mineralization, while small dyke like or sill like intrusions contain Cu-Ni-PGE mineralization. The Zhongchang and Yantiangou mafic- ultramafic intrusions are small such intrusions bearing Ni-Cu-PGE mine
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Matzat, Hans-Werner. "Mineralogical, petrological and geochemical features of the ore formation of Savage River, Tasmania (Australia), including a comparison with the Kiruna-Iron Mtn. type of iron ore deposits /." Heidelberg : [Ruprecht-Karls-Universität], 1986. http://catalogue.bnf.fr/ark:/12148/cb374293233.

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Books on the topic "Mineralogical and Petrological"

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Charley, M. J. A preliminary mineralogical and petrological study of the Al Amar gold prospect. Riofinex Ltd. for the Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources, 1985.

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Pontifex, I. R. A mineralogical and petrological study of specimens selected from gold-bearing drillhole intersections Al Amar prospect. Riofinex Ltd. for the Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources, 1986.

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Matzat, Hans-Werner. Mineralogical, petrological and geochemical features of the ore formation of Savage River, Tasmania (Australia), including a comparison with the Kiruna-Iron Mtn. type of iron ore deposits. Ruprecht-Karls-Universität, 1986.

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W, Houseknecht David, Pittman Edward D, and Clay Minerals Society, eds. Origin, diagenesis, and petrophysics of clay minerals in sandstones. SEPM, 1992.

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Fernández, Andrés Cuesta. Petrología granítica del plutón de Caldas de Reyes (Pontevedra, España): Estructura, mineralogía, geoquímica y petrogénesis. Castro, 1991.

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S, Grew E., and Anovitz Lawrence Michael, eds. Boron: Mineralogy, petrology, and geochemistry. Mineralogical Society of America, 1996.

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Observatory, Smithsonian Astrophysical, ed. Mineralogic and petrologic studies of meteorites and lunar samples: Grant NAGW 3451, final progress report, for the period 01 February 1993 through 30 September 1997. Smithsonian Institution, Astrophysical Observatory, 1998.

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F, Howie, ed. The Care and conservation of geological material: Minerals, rocks, meteorites, and lunar finds. Butterworth-Heinemann, 1992.

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Lindsley, Donald H. Oxide Minerals: Petrologic and Magnetic Significance. de Gruyter GmbH, Walter, 2018.

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Petrologiia i mineralogiia severa Urala i Timana (Trudy Instituta geologii). Komi nauchnyi tsentr UrO Rossiiskoi AN, 1997.

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Book chapters on the topic "Mineralogical and Petrological"

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Schwarz-Schampera, Ulrich, and Peter M. Herzig. "Petrological and Mineralogical Framework." In Indium. Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-05076-7_2.

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Xie, Xiande, Fuya Wang, Zhenya Sun, Pui Leung Lo, Kit Chee Kong, and Nanzhu Xie. "Petrological and Mineralogical Studies of the Sibin Bian-Stone, a Material for Making Acupuncture Tools in Ancient China." 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_93.

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Molnár, Ferenc, Tibor Zelenka, Ernõ Mátyás, et al. "Epithermal Mineralization of the Tokaj Mountains, Northeast Hungary." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.04.

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Abstract The Tokaj Mountains are situated in northeastern Hungary and host one of the oldest Au-Ag-base metal mining districts of the Tertiary-Quaternary volcanic arc of the Carpathians. The first documentation of mining activity of the Telkibánya area in the northern Tokaj Mtns. (Fig. 1) was a 14th century order from the Hungarian Royal Court, in which the borders of the mining field — coincident with the presently known distribution of mineralization — were defined (Benke, 1988). During the Medieval Ages Telkibánya reached the rank of a ‘Royal Mining Town’ and was a regular member of the Cou
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Koeberl, Christian, Wolf Uwe Reimold, Alfred Kracher, Barbara Träxler, Andreas Vormaier, and Wilfried Körner. "Mineralogical, petrological, and geochemical studies of drill core samples from the Manson impact structure, Iowa." In Special Paper 302 The Manson impact structure Iowa anatomy of an impact crater. Geological Society of America, 1996. http://dx.doi.org/10.1130/0-8137-2302-7.145.

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Mageswari, G., Chinchu Lekshmi, G. Kogila, S. Maniyarasan, and R. R. Krishnamurthy. "PETROLOGICAL AND MINERALOGICAL CHARACTERISTICS OF DIFFERENT ROCKS EXPOSED PART OF THE SOUTHERN GRANULITE TERRAIN, TAMIL NADU, INDIA." In Futuristic Trends in Physical Sciences Volume 3 Book 5. Iterative International Publishers, Selfypage Developers Pvt Ltd, 2024. http://dx.doi.org/10.58532/v3baps5p3ch5.

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The Mafic–Ultramafic Complex (SMUC) in Salem District is significant in the Southern Granulite Terrane (SGT), India. It is located in the northern part of the Cauvery Suture Zone (CSZ), is also known as the Chalk Hills of Salem. This study is an attempt to review the petrographic characteristics of the mafic- ultramafic rocks which covers the SGT, especially northern side of the of peninsular India. The study of the petrographic characterization of present rock types aims to understand the textural and mineralogical variations present through the traverse covering the Madurai block, Palghat-Ca
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S.M. Adam, Mohammed, Francois Hategekimana, YoungJae Kim, and Young-Seog Kim. "Deciphering Magmatic Evolution through Zoned Magmatic Enclaves and Composite Dikes: An Example from the Late Cretaceous Taejongdae Granite in Busan, Korea." In Recent Advances in Mineralogy [Working Title]. IntechOpen, 2023. http://dx.doi.org/10.5772/intechopen.113087.

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Late Cretaceous granitic intrusions are common in the southeastern Korean Peninsula. Most of these intrusions enclose abundant microgranular enclaves (MEs) and dikes of almost identical age to their plutons. The granitic intrusion in the Taejongdae area encloses a distinct type of enclave known as zoned MEs. The zoned MEs in this region are composed of multiple zones originated from different magmas that have the same origin and age. Several petrological, mineralogical, geochemical, SHRIMP U-Ph age dating, and Lu-Hf isotopic studies have been conducted for the Taejongdae granitoid to identify
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"Petrologic and Mineralogical Characteristics of Meteorite Groups." In Meteorite Mineralogy. Cambridge University Press, 2021. http://dx.doi.org/10.1017/9781108613767.009.

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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Mineralogy and Petrology of Serpentine." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0006.

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“Serpentine” is used both as the name of a rock and the name of a mineral. Mineralogists use “serpentine” as a group name for serpentine minerals. Petrologists refer to rocks composed mostly of serpentine minerals and minor amounts of talc, chlorite, magnetite, and brucite as serpentinites. The addition of “-ite” to mineral names is common practice in petrologic nomenclature. For instance, quartzite is a name for a rock made up mostly of quartz. Serpentinites are rocks that form as a result of metamorphism or metasomatism of primary magnesium–iron silicate minerals. This entails the replacemen
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Conference papers on the topic "Mineralogical and Petrological"

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Wang, Bojie. "The genetic analysis and their mineralogical, petrological characteristics of magnetite breccia, Ghana." In Sixth International Conference on Geoscience and Remote Sensing Mapping (GRSM 2024), edited by Zhiliang Qin, Jun Chen, and Huaichun Wu. SPIE, 2025. https://doi.org/10.1117/12.3057550.

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Likhanov, I. I. "PETROLOGICAL INDICATORS OF ACTIVE TECTOGENESIS PALEOSETTINGS." In Annual Meeting of the Russian Mineralogical Society combined with the Fedorov Session 2023. LEMA, 2023. http://dx.doi.org/10.30695/zrmo/2023.020.

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Kallesten, E. I., U. Zimmermann, M. V. Madland, and M. W. Minde. "Petrological, Mineralogical and Geochemical Constraints on Hydrocarbon Bearing North Sea Reservoir Chalk." In IOR 2017 - 19th European Symposium on Improved Oil Recovery. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700300.

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Brosky, Madeline, and Nahid Gani. "INVESTIGATING MINERALOGICAL AND PETROLOGICAL CHARACTERISTICS OF THE FLOOD BASALT ON THE ETHIOPIAN PLATEAU." In Southeastern Section-70th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021se-362058.

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Hermann, Jörg. "MSA DANA MEDAL LECTURE: MINERALOGICAL AND PETROLOGICAL CONSTRAINTS ON THE EARTH'S DEEP WATER CYCLE." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320315.

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Sipiera, Paul P., Richard B. Hoover, and Gregory A. Jerman. "Mineralogical and petrological analyses of two possible achondrite meteorites recovered from the Thiel Mountains, Antarctica." In International Symposium on Optical Science and Technology, edited by Richard B. Hoover, Gilbert V. Levin, Roland R. Paepe, and Alexei Y. Rozanov. SPIE, 2002. http://dx.doi.org/10.1117/12.454767.

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Zinchuk, N. N. "ABOUT FEATURES OF FLUID AND HYDROTHERMAL INCLUSIONS IN MINERALS IN KIMBERLITES." In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. Perm State University, 2023. http://dx.doi.org/10.17072/chirvinsky.2023.45.

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Characteristics of new genetic type of inclusions being formed during boiling up of magma or hydrotherms is given. It is indicated that the form and sizes of inclusions of boiling up fluids have important role in learning the nature of minerals. Examples of analysis by composition and temperature homogenous process of individual mineral groups’ inclusions from definite deposits of the world have been analyzed. Temperature analysis of individual inclusions homogenous process indicates that under certain conditions segregation of homogenous magmatic melt into two parts takes place – silicate and
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Šarić, Kristina. "CLAYS: FROM GEOLOGICAL CONTEXT TO CULTURAL HERITAGE." In XXIX kongres DIMK i X kongres SIGP sa Međunarodnim simpozijumom o istraživanjima i primeni savremenih dostignuća u građevinarstvu u oblasti materijala i konstrukcija. Društvo za ispitivanje i istraživanje materijala i konstrukcija Srbije, 2025. https://doi.org/10.46793/29dimk.030s.

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Clays are a fine-grained natural material that becomes plastic in contact with water, and hardens during drying and baking. In geological terms, clays are both minerals (phyllosilicates, main representatives: kaolinite, montmorillonite, illite) and rocks (clastic pelitic sedimentary rocks). The structure of phyllosilicates consists of TO or TOT layers. The layers are made up of tetrahedral (T) and octahedral (O) sheets. The tetrahedral sheet consists of SiO44-tetrahedron that are polymerized over three common oxygens. The octahedral sheet is connected to the tetrahedral sheet by a fourth oxyge
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Reports on the topic "Mineralogical and Petrological"

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Cogulu, E. H. Mineralogical and Petrological Studies of the Crystal Lake Intrusion, Thunder Bay, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128163.

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Bianco, Lino. Petrological, Mineralogical and Geochemical Characteristics of the Globigerina Limestone Outcropping at Fomm ir-Riħ, Malta. "Prof. Marin Drinov" Publishing House of Bulgarian Academy of Sciences, 2020. http://dx.doi.org/10.7546/crabs.2020.07.12.

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Mowatt, T. C., and J. C. Mowatt. Investigations of some mineralogical, petrological, geochemical, and geological relationships at the Arctic Chief (west) locality, Whitehorse Copper Belt, Yukon Territory, Canada. Alaska Division of Geological & Geophysical Surveys, 2007. http://dx.doi.org/10.14509/19553.

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Ryerson, F. J., and J. Beiriger. Mineralogic and petrologic investigation of post-test core samples from the Spent Fuel Test - Climax. Office of Scientific and Technical Information (OSTI), 1985. http://dx.doi.org/10.2172/59359.

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