Relevant bibliographies by topics / Marble rocks

Contents

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

Academic literature on the topic 'Marble rocks'

Author: Grafiati
Published: 3 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Marble rocks"

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Ploumis, P., and I. Chatzipanagis. "GEOLOGICAL, PETROLOGICAL AND TECTONIC FEATURES CHARACTERIZING THE COMMERCIALITY OF THE MARBLES OF SOUTHERN VERMION MOUNTAIN." Bulletin of the Geological Society of Greece 43, no. 5 (2017): 2702. http://dx.doi.org/10.12681/bgsg.11677.

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The southern Vermion mountain is composed of Pelagonian metamorphic rocks. Two different lithologic units are distinguished in this area. The first one consists of the highly metamorphosed rocks of Paleozoic age (migmatites, gneisses with marble intercalations and anatectic granites). The second unit comprises two series: the lower with schists, gneisses and marbles (200 m thick) and the upper with marbles (more than 2500m thick). The age of the rocks in the second unit is Triassic –Jurassic and these are metamorphosed in greenshist facies. During the last 40 years, the marbles of the second u
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Kisin, A. Yu, D. A. Ozornin, M. E. Pritchin, and V. V. Murzin. "Metamorphism and metasomatism of carbonate rocks in the frame of the Suunduk granite-gneiss massif (Southern Urals)." LITHOSPHERE (Russia) 24, no. 4 (2024): 642–60. http://dx.doi.org/10.24930/2500-302x-2024-24-4-642-660.

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Research subject. Carbonate rocks in the frame of the Suunduk granite-gneiss massif of the East Ural uplift (Southern Urals). Aim. Determination of possible petrological and geochemical zonation in carbonate rocks of the metamorphic frame of the granite-gneiss massif. Identification of structural regularities of distribution and the character of relationships between carbonate rocks of different types. Materials and Methods. Expedition works were carried out using the methods of field structural geology and mineralogy. Samples of carbonate rocks were selected along the profile transverse to th
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M. C. Gupta and Shiv Prakash Gupta. "Measuring Environmental Accounting Reporting Practices By Marble Minces Of Rajasthan." GIS Business 15, no. 1 (2020): 59–65. http://dx.doi.org/10.26643/gis.v15i1.17890.

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Rajasthan is known as mineral majestic State as it produces more than 50 types of mineral and rocks. The State is endowed with vast deposits of natural rocks known as “stones” in local parlance and a few important ones amongst them are Granite, Marble, Sandstone, Limestone, Slate and Quartzite. Perhaps, nowhere in the world social, economic and cultural fabric of the society is found to be so intimately ingrained with stone and stone based products as it is in Rajasthan State of India. The current research uses the data of RK Marbles, Evershine Marble, Mumal Marbles, Chandna Marble and Bapu Ma
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Acquafredda, Pasquale, Francesca Micheletti, and Giovanna Fioretti. "Polychrome Marbles in Christian Churches: Examples from the Antependium of Baroque Altars in Apulia (Southern Italy)." Heritage 7, no. 6 (2024): 3120–34. http://dx.doi.org/10.3390/heritage7060147.

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The antependia, realized in polychrome marbles during the Baroque period in two Christian churches of Apulia (Southern Italy), were on-site petrographically investigated by the naked eye to obtain information regarding the types of used rocks; the precision in the making of the marble tesserae was also assessed. Most of the polychrome marbles recognized were taken from buildings and monuments realized during the Roman imperial period; other marbles quarried during the Baroque period, mainly from Italian geological outcrops, were also identified. The precision in the execution of the tesserae i
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Moecher, David P., Eric D. Anderson, Claudia A. Cook, and Klaus Mezger. "The petrogenesis of metamorphosed carbonatites in the Grenville Province, Ontario." Canadian Journal of Earth Sciences 34, no. 9 (1997): 1185–201. http://dx.doi.org/10.1139/e17-095.

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Veins and dikes of calcite-rich rocks within the Central Metasedimentary Belt boundary zone (CMBbz) in the Grenville Province of Ontario have been interpreted to be true carbonatites or to be pseudocarbonatites derived from interaction of pegmatite melts and regional Grenville marble. The putative carbonatites have been metamorphosed and consist mainly of calcite, biotite, and apatite with lesser amounts of clinopyroxene, magnetite, allanite, zircon, titanite, cerite, celestite, and barite. The rocks have high P and rare earth element (REE) contents, and calcite in carbonatite has elevated Sr,
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Mirza, Tola Ahmed, Stavros P. Kalaitzidis, Sardar S. Fatah, and Sophia Tsiotou. "Petrographic and geochemical features of Gimo marble, Gole area, Kurdistan Region, Iraq: constraints on its protolith's origin and depositional environment." Earth Sciences Research Journal 25, no. 3 (2021): 285–95. http://dx.doi.org/10.15446/esrj.v25n3.88686.

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It is essential to identify marbles' petrographic and geochemical characteristics to determine the palaeo-environmental settings where their carbonate protoliths formed. The petrogenesis of massive Gimo marbles in the Gole area, Kurdistan Region of northeast Iraq, was investigated in this study through a combination of field mapping, petrographic, and geochemical techniques. Petrographic examination of these marbles reveals that mineral compositions are similar in all samples, with both homeoblastic and mosaic textures occurring, in addition to opaque grains that provide evidence of mineraliza
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Le, Tu Ngoc Thi, Ban Xuan To, Anh Van Thi Pham, Vinh Thi Dang, and Sinh Truong Pham. "Initial research results on the possibility of using metacarbonate formations in Tan Lap - Cho Don - Bac Kan province as decorative stone." Journal of Mining and Earth Sciences 64, no. 5 (2023): 49–59. http://dx.doi.org/10.46326/jmes.2023.64(5).06.

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Based on the study of the characteristics of materials, structure, textures and physical properties of metacarbonate rocks at Tan Lap area, Cho Don district, Bac Kan province, it is possible to provide the initial possibility of using these rocks as decoration stones. Methods applied in the study include field investigations and sampling; sample analysis for thin-section microscopes, for the chemistry of sicilate and physical properties. The results indicate that metacarbonate rocks consist mainly of marbles which are allocated within the 3rd unit of the upper part of Mia Le formation (D1ml2).
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Daniel, Becerra Fernández. "Notas sobre los revestimientos marmóreos parietales de la «Villa dei Quintili» (Roma, Italia)." Arqueologia Iberoamericana 52 (August 5, 2023): 29–36. https://doi.org/10.5281/zenodo.8207218.

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Este artículo da a conocer los «marmora» empleados en los revestimientos de carácter parietal que se encuentran en la «Villa dei Quintili» (Roma, Italia). Se presta especial atención a la preparación de las paredes y a la identificación macroscópica de los «marmora», constatando una gran variedad de revestimientos marmóreos parietales y de tipos lapídeos, así como la reutilización de rocas ornamentales en la preparación de las paredes. Los mármoles blancos grisáceos (&
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Gu, Bin, Zhijun Wan, Yuan Zhang, Yangsheng Ma, and Xiaodong Bernard Xu. "Influence of Real-Time Heating on Mechanical Behaviours of Rocks." Advances in Civil Engineering 2020 (August 11, 2020): 1–10. http://dx.doi.org/10.1155/2020/8879922.

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The rock mechanical properties under the effect of high temperature present a great significance on underground rock engineering. In this paper, the mechanical properties of sandstones, marbles, and granites under real-time heating were investigated with a servo-controlled compression apparatus. The results show that mechanical behaviours of all the three types of rocks are influenced by real-time heating to different degrees. Due to thermal cracking, the uniaxial compressive strengths decrease as the heating temperature rises from room temperature to 400°C. Above 400°C, the sandstone exhibits
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F., Khamis, and E. Arafah D. "Thermoluminescence Characteristics of Different Types of Natural Marble and the Effect of Annealing Temperatures." Asian Journal of Physical and Chemical Sciences 2, no. 2 (2017): 1–16. https://doi.org/10.9734/AJOPACS/2017/34624.

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<strong>Aims</strong>: This paper presents preliminary results on the characteristics of different marbles from Libya and Jordan. Several samples were collected and analyzed using thermoluminesence (TL) technique. <strong>Study Design:</strong> Study the effect of annealing temperature on the nature and the kinetics of TL trapping centers of natural marble was studied. <strong>Place and Duration of Study: </strong>Samples: Department of Physics (Atomic Physics Lab's, The University of Jordan), between June and August 2016. <strong>Methodology:</strong> Samples of high purity marble powder were
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Dissertations / Theses on the topic "Marble rocks"

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Songul, Gunes. "Archaeometrical Study On Marble Forgery." Master's thesis, METU, 2012. http://etd.lib.metu.edu.tr/upload/12614566/index.pdf.

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This thesis focuses on the detection of marble sculpture forgery made of cultured marble. Cultured marble is a mixture of marble dust, polyester and accelerators. Thus chemical analysis of cultured marble would give declined levels of calcium when compared to authentic sculptures. Since sample removal is a problem when dealing with archaeological heritage, the instrument used was portable X-Ray Fluorescence device which provides in situ analysis of the samples. Device has been used to analyze six authentic and four forgery sculptures. Seven of the sculptures were provided by Anatolian Civiliza
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Pieri, Marco. "Shear deformation of calcite rocks : rheology and microfabric evolution of Carrara marble under dynamic recrystallization during torsion experiments /." Zürich : ETH, 1999. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=13220.

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Baser, Onur. "Stabilization Of Expansive Soils Using Waste Marble Dust." Master's thesis, METU, 2009. http://etd.lib.metu.edu.tr/upload/12610339/index.pdf.

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Expansive soils occurring in arid and semi-arid climate regions of the world cause serious problems on civil engineering structures. Such soils swell when given an access to water and shrink when they dry out. Several attempts are being made to control the swell-shrink behavior of these soils. Soil stabilization using chemical admixtures is the oldest and most widespread method of ground improvement. In this study, waste limestone dust and waste dolomitic marble dust, by-products of marble industry, were used for stabilization of expansive soils. The expansive soil is prepared in laboratory as
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Miller, Robert J. "Ecological factors shaping subtidal rock wall communities in the Gulf of Maine." View this thesis online, 2005. http://libraries.maine.edu/gateway/oroauth.asp?file=orono/etheses/37803141.pdf.

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Thesis (Ph.D.)--University of Massachusetts Boston, 2005.<br>Title from PDF title page. Available through UMI ProQuest Digital Dissertations. Includes bibliographical references (p. 82-102). Also issued in print.
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Mead, Angela. "Climate and Bioinvasives drivers of change on South African Rocky shores?" Doctoral thesis, University of Cape Town, 2011. http://hdl.handle.net/11427/11308.

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Includes abstract.<br>Includes bibliographical references.<br>The overall aims of the thesis were to assess spatio-temporal change in macro species assemblages at sites located around the South African coast. Detected changes were considered in parallel with regional patterns of bioinvasion and climate change driven shifts in temperature trends over comparable time scales.
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Holmes, Sebastian Paul. "Interactions between settling organisms and molluscs in the rocky intertidal." Thesis, University of Sunderland, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.285280.

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Maher, Marie A. Bonem Rena Mae. "Comprehensive model for modern lagoonal patch reef systems in Discovery Bay, Jamaica." Waco, Tex. : Baylor University, 2007. http://hdl.handle.net/2104/5029.

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Wright, Joanna L. "Fossil terrestrial trackways : function, taphonomy and palaeoecological significance." Thesis, University of Bristol, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.389379.

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Mahé, Stéphanie. "Etude de la fracturation et de la déformation d'un massif rocheux aux abords d'une faille d'échelle crustale dans le cadre du tracé du tunnel routier de Saint-Béat." Thesis, Montpellier 2, 2013. http://www.theses.fr/2013MON20254/document.

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Le massif de marbres de Saint-Béat se situe dans la Zone Interne Métamorphique des Pyrénées centrales françaises. Il est formé de sédiments mésozoïques métamorphisés lors de l'événement métamorphique extensif Haute température - Basse pression classiquement décrit dans les Pyrénées. L'objet de cette thèse est de caractériser la déformation ductile et la fracturation qui affectent ce massif, et de déterminer dans quelle mesure les processus responsables de la fracturation peuvent être influencés par l'état de déformation. Les caractéristiques de la déformation des marbres et de ses roches encai
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Fletcher, Helen. "The impact and management of visitor pressure on Rocky Shore communities." Thesis, University of Newcastle Upon Tyne, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.363528.

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Books on the topic "Marble rocks"

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Sales, Fernando Antônio Castelo Branco., Universidade Estadual do Ceará, and Fundação Cearense de Apoio ao Desenvolvimento Cientif́ico e Tecnológico., eds. Rochas ornamentais do Ceará, Brasil =: Dimension stones of Ceará, Brazil. Universidade Estadual do Ceará, 2004.

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Mines, Indian Bureau of, and Indian Bureau of Mines. Mineral Economics Division., eds. Marble, flaggy limestone, and slate: A market survey. Govt. of India, Ministry of Mines, Indian Bureau of Mines, 2005.

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Hong Kong. Geotechnical Control Office., ed. Foundation properties of marble and other rocks in the Yuen Long-Tuen Mun area. Geotechnical Control Office, Civil Engineering Services Dept., 1991.

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(Aurelio), Alvarez Pérez A., ed. Marbles and stones of Hispania: Exhibition catalogue = Marbres i pedres d'Hispania : catàleg de l'exposició = Mármoles y piedras de Hispania : catálogo de la exposición. Institut Català d'Arqueologia Clàssica, 2009.

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Brazil) Simpósio de Rochas Ornamentais do Nordeste (4th 2003 Fortaleza. Anais. Edited by Vidal Francisco Wilson Hollanda, Lima Maria Angélica Batista, CETEM (Center), and Sociedade Brasileira de Geologia. CETEM, 2003.

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Recife, Brazil) Simpósio de Rochas Ornamentais do Nordeste (3rd 2002. Anais. UFPE, 2002.

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Chipponeri, Kelli. SpongeBob rocks! Simon Spotlight/Nickelodeon, 2006.

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Slansky, Maurice. Geology of sedimentary phosphates. North Oxford Academic, 1985.

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Slansky, Maurice. Geology of sedimentary phosphates. North Oxford Academic, 1986.

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Smith, Sian. Rock pool animals. Raintree, 2014.

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Book chapters on the topic "Marble rocks"

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Wenk, H. R., and W. R. Wilde. "Orientation Distribution Diagrams for Three Yule Marble Fabrics." In Flow and Fracture of Rocks. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm016p0083.

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Yang, Sheng-Qi. "Deformation Failure Characteristics of Crystalline Marble Under Triaxial Cyclic Loading." In Mechanical Behavior and Damage Fracture Mechanism of Deep Rocks. Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-7739-7_7.

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Yang, Sheng-Qi. "Triaxial Strength and Deformation Failure Behavior of Coarse Marble Under Six Different Loading Paths." In Mechanical Behavior and Damage Fracture Mechanism of Deep Rocks. Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-7739-7_6.

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Yang, Sheng-Qi. "Strength, Deformability and X-ray Micro CT Observations of Deeply-Buried Marble Under Different Confining Pressures." In Mechanical Behavior and Damage Fracture Mechanism of Deep Rocks. Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-7739-7_8.

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Das, Siddharth, Sangeeta Pandit, Avinash Sahu, and Rajat Kamble. "A Study on Assessment of Tourism Experience on Boat Ride of Narmada River for Sighting Marble Rocks of Bhedaghat, Jabalpur." In Lecture Notes in Mechanical Engineering. Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-1665-8_18.

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Stein, Rüdiger. "Source Rocks, Reservoirs." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6644-0_151-3.

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Stein, Rüdiger. "Source Rocks, Reservoirs." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_151.

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Liu, Ning, Chunsheng Zhang, Weijiang Chu, and Pingzhi Chen. "Time-Dependent Failure of Marble Under Long-Term Loading." In Proceedings of GeoShanghai 2018 International Conference: Rock Mechanics and Rock Engineering. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-0113-1_14.

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Li, Xianglong, Yongbo Wu, Defeng Hou, Jianguo Wang, and Lihua He. "Fractal characteristics of deep marble under impact loading." In Rock Dynamics: Progress and Prospect, Volume 1. CRC Press, 2022. http://dx.doi.org/10.1201/9781003359142-23.

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Iglesia Llanos, María Paula. "Magnetostratigraphy of Jurassic Rocks." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_71-1.

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Conference papers on the topic "Marble rocks"

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Sarkar, S., and R. Kumar. "Behavior of Post-Yielding Parameters of Marble During Plastic Deformation." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0586.

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ABSTRACT: Triaxial compression tests are used for the evaluation of the behavior of marble rock in the plastic region. Marble samples with a diameter of 60 mm are experimented on a servo-controlled universal testing machine (UTM). The marble rocks are tested under various confining stresses of 4 MPa, 8 MPa, 12 MPa, 20 MPa, and 28 MPa. During the testing, the volume change of samples is determined by quantifying the flow of hydraulic fluid into and out of the triaxial chamber. The test results reveal that marble rock is brittle at low confinement and softens with increasing confinement. The dat
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Satheesh, P. V., D. Shirole, and S. Sinha. "Investigation of the Effect of Confinement on Intact Wombeyan Marble Using Continuum Grain-Based Model (CGBM)." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0310.

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ABSTRACT: The progressive failure of brittle rock under compression involves micro-crack initiation, accumulation, and propagation. With advances in numerical modeling, it is now possible to examine complex micro-mechanical processes (e.g., strain heterogeneity, force chains, micro-level damage processes) evolving in the rocks that are difficult to investigate under conventional laboratory settings. While several studies have investigated the micromechanical aspects of brittle rock damage processes under unconfined and confined conditions in discontinuum, understanding them in a continuum medi
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Rakhimov, I. R. "ARSENIC APATITE FROM THE CALCAREOUS SKARNS OF THE KANAKAY FE-DEPOSIT (SOUTHERN URALS)." In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. Perm State University, 2023. http://dx.doi.org/10.17072/chirvinsky.2023.225.

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In the near-ore marble of the Kanakai skarn-magnetite deposit, arsenic apatite was found, which forms small euhedral and subhedral crystals confined to cracks. The As2O3 content in it reaches 0.9 wt %. % (As 0.04 apfu), and stable impurities of SiO2 (0.35–1.33 wt %), SO3 (0.28–0.63 wt %), and Cl (0.09–0.30 wt %) are typical. It could have crystallized into the post-ore stage when the rocks underwent to hydrothermal fluids relatively rich in As, S, and Cl.
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Cai, Guanglei, Hui Yang, and Qi Zhao. "Time-Lapse Measurement of P-Wave Velocities Under the Freeze-Thaw Condition in Various Rocks." In 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0441.

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ABSTRACT Global warming issues have led to pronounced cryospheric changes in mountainous areas and cold regions. Freeze-thaw weathering can alter the properties of rock masses and permafrost soils, drastically changing local environmental and geological conditions. So far, although many in-situ and laboratory tests have investigated the variation of mechanical and hydraulic properties of rock under changing temperatures, the effect of temperature variation on the rock seismic properties (e.g., elastic wave velocity, wave amplitude, wave frequency, and wave attenuation) is still insufficiently
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Shen, Q., Y. R. Liu, Y. J. Wang, and R. L. Cao. "The Influences of Drilling Parameters on the Rate of Penetration for Rock Rotary-Percussive Drilling Process." In Innovative Geotechnologies for Energy Transition. Society for Underwater Technology, 2023. http://dx.doi.org/10.3723/ioyt6578.

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The rotary-percussive drilling is commonly-used for geotechnical investigation. The rate of penetration (ROP) is critical to the construction period of geological drilling, and the setting of drilling parameters directly affects ROP. To clarify the influence of drilling parameters on ROP, laboratory full-scale rock drilling tests were conducted for three types of rocks (gneiss, dolomite, and marble). The drilling data were recorded in real time. Through the correlation analysis, the mutual independence of drilling parameters (feeder pressure, hammer pressure, and revolution per minute) was dem
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He, Changdi, and Brijes Mishra. "Methodology for Constructing Three-Dimensional DEM Model of Rock Specimen from CT Scan." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0261.

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ABSTRACT: Developing numerical simulation models that accurately represent actual features of rocks, including the distribution of minerals, voids, and fractures, is crucial. The advancement in non-destructive evaluation methods, especially X-ray computed tomography (CT), allows for detailed analysis of the internal structures of rocks. This study uses the Res-VGG-UNet deep learning model to segment CT images, distinguishing between components that appear similar but are distinct. Integrating the findings from deep learning into PFC3D software enables the creation of rock models that truly mim
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Raimbay, A., T. Babadagli, E. Kuru, and K. Develi. "Quantitative and Visual Analysis of Proppant Transport in Rough Fractures and Aperture Stability." In SPE Hydraulic Fracturing Technology Conference. SPE, 2015. http://dx.doi.org/10.2118/spe-173385-ms.

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AbstractThe consensus reached in the literature is that the roughness of fractures plays a crucial role on proppant transport affecting the aperture sustainability of hydraulic fractures. In this paper, an experimental scheme to visually and quantitatively investigate the hydraulic characteristics of rough fractures in the presence of proppants was presented. Rock samples of different kinds (i.e., granite, marble, and limestone) were fractured under the Brazilian test and molded to manufacture 20x20 cm transparent replicas. Propping agents were injected in a similar fashion and were introduced
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Pec, Matej, Hoagy O’Ghaffari, Ulrich Mok, et al. "Microscopic Defect Dynamics During a Brittle-To-Ductile Transition." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0515.

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ABSTRACT: The strength of the lithosphere is limited by pressure-dependent, "brittle" deformation of the upper crust and temperature- and strain-rate-dependent "ductile" deformation in the lower crust and upper mantle. From a simplified mechanistic point of view, intersection of these two strength envelopes can be used to estimate the depth of a region known as the brittle-to-ductile transition (BDT) where rocks deform by semi-brittle flow. This BDT is key for estimating the integrated strength of tectonic plates, constraining the earthquake cycle, and utilizing deep geothermal resources. The
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Buyuksagis, I. S., A. Cakir, M. Gursoy, and J. Rostami. "Comparison of European (EN) and American (ASTM) Abrasion Resistance Test Standards on Some Igneous and Carbonate Origin Natural Stones Subjected to Foot Traffic." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0506.

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ABSTRACT: This study compared the results of European Union (EN) and American (ASTM) standards, which are used to determine the abrasion resistance of rocks subjected to foot traffic. The amount of abrasion that will occur due to the friction of pedestrians, especially in the floor covering areas of natural stones, is a crucial criterion in estimating the life of natural stones and deciding whether to use them. In this paper, the correlations between the results obtained by applying EN 14157 and ASTM C241 Abrasion Resistance Determination (ARD) standard test methods on some igneous and carbona
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Kašić, Vladan, Ana Radosavljević-Mihajlović, Jovica Stojanović, Ivana Jelić, Slavica Mihajlović, and Nataša Đorđević. "Geological characteristics of the Lisina phosphate deposit near Bosilegrad." In Rudarstvo i geologija danas. Rudarski institut d.o.o. Beograd, 2024. https://doi.org/10.5937/rgd240030k.

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The Lisina phosphate deposit is located in southeastern Serbia, on the territory of Bosilegrad, close to the Serbian-Bulgarian border. Genetically, the Lisina phosphate deposit belongs to metamorphic deposits. A narrower area of the deposit is made up of metamorphic rocks with an intensive presence of granitoid rocks. Phosphorites occur in the contact zone of the metasandstones that make up the basement and the sericitechlorite shale with intercalations of marble and kalkshist in the roof. Raw phosphates can be applied with positive effects as a fertilizer in the territory of the Republic of S
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Reports on the topic "Marble rocks"

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Isard, S. J., J. A. Gilotti, W. C. McClelland, M. B. Petrie, and C. R. van Staal. Geology and U-Pb geochronology of low-grade mafic rocks from the St. Cyr klippe and a marble from the footwall, Canadian Cordillera, Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297474.

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Pisutha-Arnond, Visut, Sirichai Sunmanee, and Sudham Yaemniyom. A report on copper skarn deposit at Phu Lon, Amphoe Sang Khom Changwat Nong Khai. Chulalongkorn University, 1988. https://doi.org/10.58837/chula.res.1988.18.

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Based on the geological and petrographical studies and chemical analysis of drill-core and outcrop samples, the geology and mineralization at the Phu Lon area are revealed. The Phu Lon prospect is a Cu-Fe-Au-Ag skarn deposit of porphyry-related type. The copper- and iron-rich zones are hosted predominantly in the garnet-pyroxene skarn that is developed metasomatically at the contact between the diorite-monzodiorite intrusions and a marble with minor calcsilicate unit. The main stage of iron mineralization probably took place during the prograde garnet-pyroxene skarn formation and was genetical
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Tweet, Justin, Holley Flora, Summer Weeks, Eathan McIntyre, and Vincent Santucci. Grand Canyon-Parashant National Monument: Paleontological resource inventory (public version). National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2289972.

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Grand Canyon-Parashant National Monument (PARA) in northwestern Arizona has significant paleontological resources, which are recognized in the establishing presidential proclamation. Because of the challenges of working in this remote area, there has been little documentation of these resources over the years. PARA also has an unusual management situation which complicates resource management. The majority of PARA is administered by the Bureau of Land Management (BLM; this land is described here as PARA-BLM), while about 20% of the monument is administered by the National Park Service (NPS; th
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Rainbird, R. H., and W. J. Davis. Summary of the Statherian-Calymmian paleogeography of northwestern Laurentia. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332508.

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The ca. 1.75 to 1.27 Ga Hornby Bay intracontinental basin, in northwestern Canada, includes the Big Bear, Mountain Lake, and Dismal Lakes groups. This paper investigates the original depositional environments, paleogeography, and architecture of these groups and how they correlate in time and space. The Big Bear group comprises mainly immature clastic rocks deposited by high-energy rivers, the overlying Mountain Lake group was deposited by westerly flowing rivers over a much broader region, and, following tectonic uplift and erosion, basal clastic rocks of the Dismal Lakes Group were deposited
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Gadd, M. G., J. M. Peter, T A Fraser, and D. Layton-Matthews. Paleoredox and lithogeochemical indicators of the environment of formation and genesis of the Monster River hyper-enriched black shale showing, Yukon. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328004.

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Northern Yukon hosts occurrences of Middle Devonian hyper-enriched black shale (HEBS) Ni-Mo-Zn-platinum-group element-Au-Re mineralization, including the Monster River showing in the Ogilvie Mountains. This mineralization has been documented predominantly in the Paleozoic Richardson trough; however, the Monster River showing is atypical, occurring within the Blackstone trough, more than 200 km to the west on the southern margin of the Yukon block. The ambient paleoredox conditions of the marine water column and sediments may be primary controlling factors in HEBS formation. We use major and tr
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Tweet, Justin, Vincent Santucci, Vincent Santucci, and Justin Tweet. Effigy Mounds National Monument: Paleontological resource inventory (public version). National Park Service, 2025. https://doi.org/10.36967/2307451.

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Effigy Mounds National Monument (EFMO) in northeastern Iowa was proclaimed on October 25, 1949, to protect a significant concentration of Native American burial mounds, many of which were built in the shapes of animals such as bears. Many of these effigy mounds are found atop commanding bluffs flanking the Yellow River at its junction with the Mississippi River. The geology of the monument has not been a central interest in its history, but the rocks contain evidence of millions of years of shallow marine life from the early Paleozoic. Paleozoic fossils were first documented at what is now EFM
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Tweet, Justin, Vincent Santucci, Vincent Santucci, and Justin Tweet. Effigy Mounds National Monument: Paleontological resource inventory (sensitive version). National Park Service, 2024. http://dx.doi.org/10.36967/2306478.

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Effigy Mounds National Monument (EFMO) in northeastern Iowa was proclaimed on October 25, 1949 to protect a significant concentration of Native American burial mounds, many of which were built in the shapes of animals such as bears. Many of these effigy mounds are found atop commanding bluffs flanking the Yellow River at its junction with the Mississippi River. The geology of the monument has not been a central interest in its history, but the rocks contain evidence of millions of years of shallow marine life from the early Paleozoic. Paleozoic fossils were first documented at what is now EFMO
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Dafoe, L. T., K. Dickie, G. L. Williams, and T. McCartney. Stratigraphy of the Labrador margin: a synthesis and new perspectives. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321829.

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The Labrador Sea formed during rifting between North America and Greenland beginning in the Early Cretaceous, with subsequent seafloor spreading from the Maastrichtian (chron C31) to Early Paleocene (chron C27n) that ended by chron C13 (earliest Oligocene). Early Cretaceous rifting resulted in accumulation of Alexis Formation basalt units and Bjarni Formation nonmarine and marginal marine clastic rocks. In the Late Cretaceous, extension focused further offshore as sag basin conditions formed across the shelf, with a basinwide transgression of Markland Formation shale and localized Freydis Memb
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Cox-Ammann, Karah, Mirella Cortez, Eric Dinger, and Alexis Necarsulmer. Rocky intertidal monitoring: 2021–2022 results from Redwood National and State Parks. National Park Service, 2025. https://doi.org/10.36967/2309092.

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This report presents survey results from 2021 and 2022 for the rocky intertidal community at 3 sites at Redwood National and State Parks (RNSP) in Del Norte County, California. These sites are part of MARINe (Multi-Agency Rocky Intertidal Network), a regional intertidal monitoring network sponsored by the Bureau of Ocean Energy Management (BOEM), with additional funding and support from local and state governments, universities, and private organizations (see www.marine.ucsc.edu). Funding for annual monitoring in RNSP is provided by the National Park Service (NPS) Klamath Network (KLMN) throug
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Ammann, Karah, Eric Dinger, and David Lohse. Rocky intertidal monitoring: 2019?2020 results from Redwood National and State Parks. National Park Service, 2023. http://dx.doi.org/10.36967/2301673.

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This report presents the results of the monitoring surveys done in 2019 and 2020 of the rocky intertidal community at three sites within the Redwood National and State Parks (RNSP) in Del Norte County, California. These sites are part of MARINe (Multi-Agency Rocky Intertidal Network), a regional intertidal monitoring network sponsored by the Bureau of Ocean Energy Management (BOEM), with additional funding and support from local and state governments, universities, and private organizations (see www.marine.ucsc.edu). Funding for annual monitoring in RNSP is provided by the National Park Servic
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