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Relevant bibliographies by topics / The Dolomites

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Academic literature on the topic 'The Dolomites'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "The Dolomites"

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Khan, Emad Ullah, Abbas Ali Naseem, Maryam Saleem, et al. "Petrography and Geochemistry of Dolomites of Samanasuk Formation, Dara Adam Khel Section, Kohat Ranges, Pakistan." Sains Malaysiana 50, no. 11 (2021): 3205–17. http://dx.doi.org/10.17576/jsm-2021-5011-05.

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Replacement dolomite occurs in Jurassic Samanasuk Formation in Dara Adam khel area of Kohat ranges, North-Western Himalayas, Pakistan. This study, for the first time, document the process of dolomitization and evolution of strata bound dolomitic bodies. Field investigation, petrography and geochemistry helped in unraveling the formation of several dolomitic bodies. Petrographically dolomites comprises of: (1) medium grain crystalline planer subhedral dolomite (Dol-I); (2) fine grained crystalline anhedral non-planer dolomite rhombs (Dol-II); (3) medium to coarse grained crystalline subhedral-a

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Zhong, Shan, Zhaoqian Liu, Zhenkui Jin, Hongyu Tian, Madaki Agwom Istifanus, and Simon C. George. "The Development of Dolomite Within a Sequence Stratigraphic Framework: Cambrian Series 2 Changping Formation, Xiaweidian, China." Minerals 14, no. 12 (2024): 1189. http://dx.doi.org/10.3390/min14121189.

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The Lower Cambrian Changping Formation in the Western Hills of Beijing hosts tidal flat and lagoonal carbonates comprising dolomites, limestones, and dolomitic limestones, reflecting the processes of dolomite cementation and dolomitization within a sedimentary framework. Based on petrographic textures, two types of dolomites were identified: microcrystalline dolomite and fine-mesocrystalline dolomite. Integrating petrological and geochemical data unveils two diagenetic stages. The initial dolomite formation, attributed to hypersaline fluids, occurred in a supratidal-sabkha setting during the e

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Mohammed, M. A. A., A. Salmiaton, W. A. K. G. Wan Azlina, M. S. Mohamad Amran, and Y. H. Taufiq-Yap. "Preparation and Characterization of Malaysian Dolomites as a Tar Cracking Catalyst in Biomass Gasification Process." Journal of Energy 2013 (2013): 1–8. http://dx.doi.org/10.1155/2013/791582.

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Three types of local Malaysian dolomites were characterized to investigate their suitability for use as tar-cracking catalysts in the biomass gasification process. The dolomites were calcined to examine the effect of the calcination process on dolomite’s catalytic activity and properties. The modifications undergone by dolomites consequent to thermal treatment were investigated using various analytical methods. Thermogravimetric and differential thermal analyses indicated that the dolomites underwent two stages of decomposition during the calcination process. The X-ray diffraction and Fourier-

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Chen, Xiaoquan, Fengcun Xing, Shu Jiang, et al. "Origin and formation model of Eocene dolomite in the upper Niubao Formation of the Lunpola Basin, Tibetan Plateau." Interpretation 9, no. 3 (2021): SF11—SF22. http://dx.doi.org/10.1190/int-2020-0195.1.

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Using fresh core samples, we have determined the origin and formation process of Eocene lacustrine dolomites in the Tibetan Plateau through petrological, mineralogical, and geochemical analyses. Dolomitic rocks were collected from the upper member of the Eocene Niubao Formation in the Lunpola Basin, consisting of dolomitic mudstone, argillaceous dolomite, dolomite-bearing mudstone, and mud-bearing dolomite. These dolomites are dominated by aphanotopic and microcrystalline dolomites, with minor amounts of euhedral or subhedral powder- and fine-crystalline dolomites. Carbon and oxygen stable iso

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Yaghoubi, Marjan, Adel Najafzadeh, Afshin Zohdi, Rahim Mahari, and Fazel Khaleghi. "Petrography and Geochemistry of the Triassic Elika Formation Dolomites in Zal Section, Jolfa, NW Iran." Journal Of The Geological Society Of India 100, no. 11 (2024): 1615–29. http://dx.doi.org/10.17491/jgsi/2024/174020.

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ABSTRACT The Triassic Elika Formation contains nine distinct sedimentary units with calcareous and dolomitic composition and up to 377 m in stratigraphic thickness in NW Iran. The two upper dolomitic units with about 78 m in thickness mainly consist of dolomicrite and have formed in shallow burial environments under reducing conditions, frequently influenced by marine fluids. This formation was deposited in supratidal to intertidal shallow marine settings with low temperature and a high rate of evaporation, resulting in the formation of very fine-grained dolomite. The nearsurface diagenetic en

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Huang, Shuguang, Mingcai Hou, Anqing Chen, et al. "Fluid Properties and Genesis of Dolomites in the Devonian Guanwushan Formation of Upper Yangtze Platform, SW China." Minerals 12, no. 3 (2022): 317. http://dx.doi.org/10.3390/min12030317.

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The Guanwushan Formation (GWSF) of Devonian dolomite are extensively developed in the northwest of Sichuan Basin in the Upper Yangtze region, but the properties of dolomitization fluid and the geneses are still unclear. Three types of dolomites can be divided by petrological characteristics: the fine-microcrystalline dolomites (FMD), the fine crystalline dolomites (FCD) and the medium crystalline dolomites (MCD). The order degree of these three types of dolomites increased in turn, and they all showed dark cathodoluminescence (CL) luminescence. The total amount of Rare Earth Elements (∑REE) of

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Δήμου, Ε., and Κ. Κούκουζας. "MlNERALOGICAL STUDY OF Mg-SKARNS WITH CLINOHUMITE AT THE OMERLI SITE AGGISTRO, SERRES." Bulletin of the Geological Society of Greece 36, no. 1 (2004): 436. http://dx.doi.org/10.12681/bgsg.16732.

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Mg-skam occurrences located in the dolomitic marbles at the Omerli site near Aggistro are studied. The dolomitic marbles are gradually enriched in metasomatic minerals, up to the full replacement and the formation of cohesive lenticular beds of skarns in the marbles. The aplito-pegmatitic veins traversing the surrounding marbles as well as the granodiorite occurring in the broader area of Ahladohoho, are considered responsible for the phenomena of thermal metamorphism and metasomatism in the dolomites. On the basis of mineralogical analytical methods (optical microscopy, X-Ray diffraction, mic

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Manche, Cameron J., and Stephen E. Kaczmarek. "A global study of dolomite stoichiometry and cation ordering through the Phanerozoic." Journal of Sedimentary Research 91, no. 5 (2021): 520–46. http://dx.doi.org/10.2110/jsr.2020.204.

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ABSTRACT Various geochemical proxies are used to constrain the diagenetic origin and evolution of ancient dolomites. Dolomite stoichiometry (mole % MgCO3) and cation ordering, two mineralogical attributes that define dolomite, have also been shown to demonstrate utility in this regard. Observations from laboratory experiments and field studies suggest that these attributes broadly reflect the fluid chemistry and temperature of the dolomitizing environment. The degree to which these parameters reflect global conditions during dolomitization (e.g., seawater chemistry, eustasy, atmospheric pCO2)

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WANG, Jian, Lu ZHOU, Baozhen ZHANG, and Chonglong GAO. "INSIGHTS INTO THE ORIGIN OF SHALLOW MARINE DOLOSTONES, LONGWANGMIAO FORMATION (LOWER CAMBRIAN), NORTHEAST SICHUAN BASIN, CHINA: PETROGRAPHIC AND GEOCHEMICAL CONSTRAINTS." Carpathian Journal of Earth and Environmental Sciences 17, no. 1 (2022): 5–20. http://dx.doi.org/10.26471/cjees/2022/017/196.

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For a better understanding of the origin of Early Cambrian dolomites in the Sichuan Basin, which serve as valuable oil and gas reservoirs, we present and interpret complex multiparameter petrographic and geochemical analyses of dolomites in the Cambrian Longwangmiao Formation at the Yangsiqiao section. Our data show that these dolomites mainly occur in the middle and upper parts of the Longwangmiao Formation, and we identify two types of dolomites: micrite and fine-medium crystalline dolomites. The micritic dolomites, occasionally coupled with quartz and mica minerals, show dirty crystal surfa

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Mirnov, R., and A. Nikolaev. "Dolomite-sepiolite interaction in Kashira and Podolsk deposits of platform part of Bashkortostan: possible biogenic origin." Vestnik of geosciences, no. 10 (December 2, 2024): 3–11. https://doi.org/10.19110/geov.2024.10.1.

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The article is devoted to the genesis of microcrystalline dolomites of the Kashira and Podolsk horizons of the Moscow stage, which are oil reservoirs in the western part of Bashkortostan. They form consistent layers of low thickness, traceable for tens of kilometers, which determines the relevance of studying the conditions of dolomite formation. Dolomites are composed of crystals 1–10 µm in size with sulfate inclusions and sepiolite admixture. Sepiolites are developed in the intercrystalline space as the finest threads and films enveloping dolomite crystals. A detailed study of sepiolites wit

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Dissertations / Theses on the topic "The Dolomites"

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Sloman, L. E. "Middle triassic Magmatism in the Dolomites, Northern Italy." Thesis, University of Oxford, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.379987.

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Bainbridge, William. "Heritage in the clouds : Englishness in the Dolomites." Thesis, Durham University, 2014. http://etheses.dur.ac.uk/10723/.

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Guided by the romantic compass of Byron, Ruskin and Turner, Victorian travellers to the Dolomites sketched through their wanderings in the mountainous backdrop of Venice a cultural ‘Petit Tour’ of global significance. As they zigzagged across a debatable land consumed by competing frontiers, Victorians discovered a unique geography characterized by untrodden peaks and unfrequented valleys. This landscape blended aesthetic, scientific and cultural values utterly different from those engendered by the bombastic conquests of the Western Alps achieved during the ‘Golden Age of Mountaineering’. Fil

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Hird, Kevin. "Petrography and geochemistry of some Carboniferous and Precambrian dolomites." Thesis, Durham University, 1985. http://etheses.dur.ac.uk/1674/.

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Marangon, Alessandro. "Stratigraphic analysis on Monte Agnello and Latemar platforms (Southern Alps, Dolomites, Italy)." Doctoral thesis, Università degli studi di Padova, 2011. http://hdl.handle.net/11577/3427480.

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Introduction Cyclostratigraphy is emerging as a central focus in stratigraphy, with its impressive record of global climate changes forced by Earth’s astronomical parameters, and with its capacity to provide high- resolution information about geologic time. Shallow-marine cyclostratigraphy, principally from carbonate-rich peritidal facies, represents the main source of information about astronomical forcing and global climate change prior to the Jurassic. Mineral magnetic parameters (MS, ARM, SIRM, S-ratio, ARM/MS and ARM/SIRM ratio) provide new information about shallow-marine cyclostratig

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Shah, Mumtaz Muhammad. "Hydrothermal dolomites in the plateform carbonates (early albian) of the Ranero zone (NW Spain) : Distribution, petrography, geochemistry and their genesis." Thesis, Saint-Etienne, EMSE, 2011. http://www.theses.fr/2011EMSE0627/document.

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Ce mémoire décrit les corps dolomitiques des zones de Ranero et El Moro (vallée de la Karantza, zone Cantabrique, NO de l’Espagne) et précise les variations temporelles et latérales de leurs attributs pétrographiques et géochimiques. Les corps dolomitiques sont portés par les calcaires Albiens, déposés sur la marge du bassin Basque-Cantabrique en période d’intense subsidence. Les dolomies sont formées par replacement et par cémentation, et précédées et suivies par divers types de ciment calcitique. L’étude pétrographique, minéralogique et géochimique (XRD, ICP, XRF, isotopes stables et Sr) est

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Zilocchi, Lucia <1975&gt. "Soil developpment in the Dolomites region (Fassa and San Pellegrino valleys, NE Italy)." Doctoral thesis, Università Ca' Foscari Venezia, 2004. http://hdl.handle.net/10579/110.

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Le attuali conoscenze riguardo la pedogenesi e l'evoluzione della copertura pedologica in ambiente alpino sono ancora lontane dall'essere esaustive. Pochi sono i lavori, a livello nazionale ma anche a livello mondiale, che studiano da un punto di vista puramente pedologico/evolutivo la situazione dei suoli di aree di alta montagna, in particolare questo è vero per suoli che si sviluppano da substrati calcarei. In questa sede vengono presentati i risultati relativi allo studio dei caratteri pedo-ambientali di 56 profili di suolo, ubicati in due valli delle Dolomiti (Valli di Passa e di San Pell

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Fontaneta, Gabriella Talamo. "Dolomitização e fosfogênese na formação bocaina, grupo Corumbá (ediacarano)." Universidade de São Paulo, 2012. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-28022013-102622/.

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Dolomitos são rochas carbonáticas abundantes no registro sedimentar Pré-Cambriano, porém raras no registro Fanerozóico e sua gênese até hoje permanece como um enigma da geologia, conhecido como o \"Problema Dolomito\". As rochas sedimentares fosfáticas são amplamente estudadas por fornecerem dados importantes sobre a evolução sedimentar e condições físico-químicas e biológicas da água do mar durante a sedimentação e a diagênese, além de constituírem os maiores depósitos econômicos de fósforo do mundo. Os dolomitos e fosforitos da Formação Bocaina foram estudados com base na individualização

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Cattadori, Isabella M. C. "Temporal dynamics and spatial patterns of galliform birds in Trentino - Italy." Thesis, University of Stirling, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.311690.

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Emmerich, Axel. "Controlling factors of two Middle Triassic carbonate platforms: Latemar and Rosengarten (Dolomites, Northern Italy)." [S.l. : s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=971776717.

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Cembran, Glenda <1985&gt. "Seeking Cultural Authority in Unbeaten Paths: Amelia Edwards’s Journeys Through the Dolomites and Egypt." Master's Degree Thesis, Università Ca' Foscari Venezia, 2016. http://hdl.handle.net/10579/7434.

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Amelia B. Edwards was a versatile and prolific literary figure of the Victorian period. From a very early age she excelled in many artistic fields, but writing represented for her the most suitable means to earn her living, as she made the arduous choice not to marry and depend on a husband. Edwards worked mainly as a novelist, journalist, Egyptologist and travel writer. Her successful travel books, entitled Untrodden Peaks and Unfrequented Valleys (1873) and A Thousand Miles up the Nile (1877), are the outcomes of two extended journeys through the Dolomites and Egypt respectively. Amelia Edwa

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Books on the topic "The Dolomites"

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Purser, Bruce, Maurice Tucker, and Donald Zenger, eds. Dolomites. Blackwell Publishing Ltd., 1994. http://dx.doi.org/10.1002/9781444304077.

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1750-1801, Dolomieu Déodat de, Purser B. H, Tucker Maurice E, and Zenger Donald H, eds. Dolomites: A volume in honour of Dolomieu. Blackwell Scientific Publications, 1994.

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Mathis, Peter. Visual dualism: Dolomites. FenkART Publishing, 2012.

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Stedman, Henry. Trekking in the Dolomites. Trailblazer, 2001.

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Pauls, Michael. Venice, Venetia & the Dolomites. 4th ed. Cadogan Guides, 2007.

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Doglioni, Carlo. Structural styles & Dolomites field trip: Stili strutturali ed escursioni nelle Dolomiti. ENI, 2008.

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Cicchetti, Manuel. Monocrome: Walking through the Ampezzo Dolomites = camminando tra le Dolomiti d'Ampezzo. The Music Company, 2018.

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Pignatti, Erika, and Sandro Pignatti. Plant Life of the Dolomites. Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-662-48032-8.

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Pignatti, Erika, and Sandro Pignatti. Plant Life of the Dolomites. Springer Berlin Heidelberg, 2017. http://dx.doi.org/10.1007/978-3-662-53051-1.

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Pignatti, Erika, and Sandro Pignatti. Plant Life of the Dolomites. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-31043-0.

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Book chapters on the topic "The Dolomites"

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Greensmith, J. T. "Magnesian limestones and dolomites." In Petrology of the Sedimentary Rocks. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-011-9640-6_8.

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Pignatti, Erika, and Sandro Pignatti. "The Flora of the Dolomites." In Plant Life of the Dolomites. Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-662-53051-1_3.

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Pignatti, Erika, and Sandro Pignatti. "The Landscape of the Dolomites." In Plant Life of the Dolomites. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31043-0_19.

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Pignatti, Erika, and Sandro Pignatti. "The Landscape of the Dolomites." In Plant Life of the Dolomites. Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-662-48032-8_19.

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Picard, M. Dane. "Through the Dolomites and Apennines." In Mountains and Minerals/Rivers and Rocks. Springer US, 1993. http://dx.doi.org/10.1007/978-1-4684-6444-3_17.

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Bucher, Kurt. "Metamorphism of Dolomites and Limestones." In Springer Textbooks in Earth Sciences, Geography and Environment. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-12595-9_6.

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Bucher, Kurt, and Martin Frey. "Metamorphism of Dolomites and Limestones." In Petrogenesis of Metamorphic Rocks. Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-04914-3_6.

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Bucher, Kurt, and Martin Frey. "Metamorphism of Dolomites and Limestones." In Petrogenesis of Metamorphic Rocks. Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-662-03000-4_6.

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Bucher, Kurt, and Rodney Grapes. "Metamorphism of Dolomites and Limestones." In Petrogenesis of Metamorphic Rocks. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-540-74169-5_6.

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Pignatti, Erika, and Sandro Pignatti. "History of the Floristic Exploration in the Dolomites." In Plant Life of the Dolomites. Springer Berlin Heidelberg, 2016. http://dx.doi.org/10.1007/978-3-662-53051-1_1.

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Conference papers on the topic "The Dolomites"

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Sagues, A. A., S. K. Sherman, and V. K. Sethi. "Erosion of Carbon Steel by Pneumatically Conveyed Limestones and Dolomites." In CORROSION 1986. NACE International, 1986. https://doi.org/10.5006/c1986-86094.

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Abstract A test method was developed that can be used to rank atmospheric fluidized bed combustor (AFBC) sulfur sorbent stones for relative erosivity of pneumatic feed systems. The method features easy normalization and low sensitivity to sample preparation parameters. The stones tested showed a wide range of erosivities when using a carbon steel target. The erosivity ranking does not have a straightforward correlation with selected physical or chemical properties of the stones. However, dolomites as a group showed higher erosivity than limestones.

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Tortoreto, Giuliano, and Seyed Mahed Mousavi. "Dolomites@#SMM4H 2024: Helping LLMs “Know The Drill” in Low-Resource Settings - A Study on Social Media Posts." In Proceedings of The 9th Social Media Mining for Health Research and Applications (SMM4H 2024) Workshop and Shared Tasks. Association for Computational Linguistics, 2024. http://dx.doi.org/10.18653/v1/2024.smm4h-1.5.

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Aluvihara, Suresh, C. S. Kalpage, and P. W. S. K. Bandaranayake. "The Advanced Applications of Earth Materials based upon the Adsorption and Absorption Processes." In 5th World Conference on Chemistry and Chemical Engineering and 5th World Conference on Advanced Materials, Nanoscience and Nanotechnology. Eurasia Conferences, 2024. https://doi.org/10.62422/978-81-970328-7-5-027.

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Earth materials are unevenly distributed in the world in different forms and phases. Solid earth materials play an outstanding preface among earth materials in other phase because of the availabilities in their manifold forms both natural or manmade forms such as the bulky forms and powdered forms. Adsorption is an outstanding characteristic regarding some solid materials based upon the adsorption capacities of such materials with respect to some specific compounds that presence in liquids and gases. Clays and dolomites are predominantly having multi physic-chemical characteristics. As the gen

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Washington, Paul A., and Steven A. Chisick. "DISTINGUISHING BETWEEN AUTHIGENIC AND PRIMARY DOLOMITE SEDIMENT IN STRATIGRAPHIC DOLOMITES BASED ON GRAIN MORPHOLOGY." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382381.

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Imperl, Jernej, Mitja Kolar, Vilma Ducman, Gorazd Žibret, and Lea Žibret. "Selective separation of magnesium from Slovenian dolomites." In Proceedings of XVI International Mineral Processing and Recycling Conference, Belgrade, 28-30.05.2025. University of Belgrade, Technical Faculty, Bor, 2024. https://doi.org/10.5937/imprc25113i.

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Although magnesium is one of the most abundant elements on Earth by weight, the demand for magnesium is constantly increasing due to its widespread use in a diverse range of industries such as metal alloys, electronics, batteries, agricultural and pharmaceutical compounds. For this reason, magnesium is categorised as a critical raw material by the European Union. Dolomite CaMg(CO3)2 is one of the most important mineral sources of magnesium, which in its pure form contains 13.18 % magnesium by weight. Various pyrometallurgical and hydrometallurgical processes have been developed and are used to

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Ayupov, Amir Rustamovich, Sergey Faizovich Khafizov, and Kurmangazy Orinbgazievich Iskaziev. "Influence of Secondary Alterations on the Structure of the Pore Space of the Upper Permian Carbonate Deposits of the Northern Side Zone of the Caspian Basin." In SPE Annual Caspian Technical Conference. SPE, 2021. http://dx.doi.org/10.2118/207049-ms.

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Abstract The analysis of the facies distribution of reservoirs within the Moscow-Artinskian sedimentation rim within the Northern part of the Pre-Caspian Basin was carried out. The Teplovsko-Tokarevskaya group of deposits is a chain of carbonate structures stretched in the sub-latitudinal direction. They are consist mainly of bioherm structures, which include tubifytes, foraminifera, crinoidea, ostracods, ostracods, etc. From the lithological point of view, the reservoir rocks are represented by dolomite-limestone differences-from organic limestones to secondary chemogenic dolomites. The influ

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Ayupov, Amir Rustamovich, Sergey Faizovich Khafizov, and Kurmangazy Orinbgazievich Iskaziev. "Influence of Secondary Alterations on the Structure of the Pore Space of the Upper Permian Carbonate Deposits of the Northern Side Zone of the Caspian Basin." In SPE Annual Caspian Technical Conference. SPE, 2021. http://dx.doi.org/10.2118/207049-ms.

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Abstract The analysis of the facies distribution of reservoirs within the Moscow-Artinskian sedimentation rim within the Northern part of the Pre-Caspian Basin was carried out. The Teplovsko-Tokarevskaya group of deposits is a chain of carbonate structures stretched in the sub-latitudinal direction. They are consist mainly of bioherm structures, which include tubifytes, foraminifera, crinoidea, ostracods, ostracods, etc. From the lithological point of view, the reservoir rocks are represented by dolomite-limestone differences-from organic limestones to secondary chemogenic dolomites. The influ

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Runyan, Daniel M., Virginia T. McLemore, Evan J. Owen, and Ethan B. Haft. "High-Magnesium Dolomites in South-Central New Mexico." In 2023 New Mexico Geological Society Annual Spring Meeting. New Mexico Geological Society, 2023. http://dx.doi.org/10.56577/sm-2023.2924.

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Adenan, Noorhashima Binti, Che Aziz Ali, and Kamal Roslan Mohamed. "Dolomites petrography and geochemistry of the Chuping Formation, Malaysia." In THE 2013 UKM FST POSTGRADUATE COLLOQUIUM: Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2013 Postgraduate Colloquium. AIP Publishing LLC, 2013. http://dx.doi.org/10.1063/1.4858696.

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Whitney, John W., Ahmed Banakar, Abdulla M. Memesh, et al. "MULTIPLE EPISODES OF YARDANG EVOLUTION IN SAUDI ARABIAN DOLOMITES." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281501.

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Reports on the topic "The Dolomites"

1

Hanson, G. N., and W. J. Meyers. Geochemistry and origin of regional dolomites. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/5085323.

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2

Hanson, G., and W. Meyers. Geochemistry and origin of regional dolomites. Office of Scientific and Technical Information (OSTI), 1989. http://dx.doi.org/10.2172/7003817.

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3

Hanson, G. N., and W. J. Meyers. Geochemistry and origin of regional dolomites. Final report. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/64178.

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4

Paradis, S., G. J. Simandl, N. Drage, R J D'Souza, D. J. Kontak, and Z. Waller. Carbonate-hosted deposits (Mississippi Valley-type, magnesite, and REE-F-Ba) of the southeastern Canadian Cordillera: a review and isotopic data comparison. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/327995.

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The Mississippi Valley-type, magnesite, and REE-F-Ba deposits in the southeastern Canadian Cordillera are in the weakly deformed/metamorphosed Paleozoic carbonate platform of the Rocky Mountains. Most are hosted in dolostones of the middle Cambrian Cathedral, upper Cambrian Jubilee, and Upper Devonian Palliser formations and spatially associated with hydrothermal dolomite. They occur along structurally controlled facies transitions between the shallow-water carbonate platform and deeper water basin rocks of the Paleozoic continental margin. Their location and morphology reflect episodic riftin

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5

Lavoie, D., S. Zhang, and N. Pinet. Hydrothermal dolomites in Hudson Bay platform: preliminary field and geochemical data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289303.

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6

Hanson, G. N., and W. J. Meyers. Geochemistry and origin of regional dolomites. Technical progress report, July 26, 1991--April 21, 1992. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/10153275.

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7

Hanson, G., and W. Meyers. Geochemistry and origin of regional dolomites: Annual progress report, July 26, 1988--April 15, 1989. Office of Scientific and Technical Information (OSTI), 1989. http://dx.doi.org/10.2172/5940423.

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8

Beauheim, R. L., and G. J. Ruskauff. Analysis of hydraulic tests of the Culebra and Magenta Dolomites and Dewey Lake Redbeds conducted at the Waste Isolation Pilot Plant Site. Office of Scientific and Technical Information (OSTI), 1998. http://dx.doi.org/10.2172/303943.

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9

Carter, T. R., C E Logan, and H. A. J. Russell. Three-dimensional model of dolomitization patterns in the Salina Group A-1 Carbonate and A-2 Carbonate units, Sombra Township, Lambton County, southern Ontario. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332363.

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Abstract:

Dolomitization of carbonate rocks is a subject of considerable interest due to association with oil and gas reservoirs and Mississippi Valley Type ore deposits. Conceptual two-dimensional models of dolomitization are common in the literature, however numeric models supported by high quality data are rare to nonexistent. This paper presents three-dimensional (3-D) dolomitization patterns in the Salina Group A-1 Carbonate Unit and A-2 Carbonate Unit located in Sombra Township, Lambton County. The source data consists of percent dolomite measurements collected from 9727 drill cutting samples, sta

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10

Collings, R. K., and P. R. A. Andrews. Magnesite, brucite and dolomite. Natural Resources Canada/CMSS/Information Management, 1990. http://dx.doi.org/10.4095/328629.

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