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Relevant bibliographies by topics / Petrography

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Academic literature on the topic 'Petrography'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 May 2024

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Journal articles on the topic "Petrography"

1

Babine, Karen. "Petrography." River Teeth: A Journal of Nonfiction Narrative 8, no. 1 (2006): 5–16. http://dx.doi.org/10.1353/rvt.2006.0000.

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Pearson, Geoffrey L., John E. Prentice, and Alastair W. Pearson. "Three English Romanesque Lecterns." Antiquaries Journal 82 (September 2002): 328–39. http://dx.doi.org/10.1017/s0003581500073856.

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Three surviving stone lecterns are described and analysed in terms of their petrography and sculptural style. The similarity between their petrography strongly suggests that they share a common origin, traceable to a quarry or quarries in the immediate vicinity of Much Wenlock, and that the similarity of sculptural style and dimensions points to them being a product of a single workshop. Furthermore, the authors suggest that the petrographie and stylistic characteristics show striking similarities to the Much Wenlock lavabo, thus adding support to the notion of a Much Wenlock workshop.

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Middleton, Andrew. "Ceramic petrography." Revista do Museu de Arqueologia e Etnologia. Suplemento, supl.2 (December 10, 1997): 73. http://dx.doi.org/10.11606/issn.2594-5939.revmaesupl.1997.113441.

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Morad, Sadoon. "Sedimentary petrography." Sedimentary Geology 92, no. 3-4 (September 1994): 292–94. http://dx.doi.org/10.1016/0037-0738(94)90114-7.

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Di Febo, Roberta, Lluís Casas, Jordi Rius, Riccardo Tagliapietra, and Joan Melgarejo. "Breaking Preconceptions: Thin Section Petrography For Ceramic Glaze Microstructures." Minerals 9, no. 2 (February 15, 2019): 113. http://dx.doi.org/10.3390/min9020113.

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During the last thirty years, microstructural and technological studies on ceramic glazes have been essentially carried out through the use of Scanning Electron Microscopy (SEM) combined with energy dispersive X-ray analysis (EDX). On the contrary, optical microscopy (OM) has been considered of limited use in solving the very complex and fine-scale microstructures associated with ceramic glazes. As the crystallites formed inside glazes are sub- and micrometric, a common misconception is that it is not possible to study them by OM. This is probably one of the reasons why there are no available articles and textbooks and even no visual resources for describing and characterizing the micro-crystallites formed in glaze matrices. A thin section petrography (TSP) for ceramic glaze microstructures does not exist yet, neither as a field of study nor conceptually. In the present contribution, we intend to show new developments in the field of ceramic glaze petrography, highlighting the potential of OM in the microstructural studies of ceramic glazes using petrographic thin sections. The outcomes not only stress the pivotal role of thin section petrography for the study of glaze microstructures but also show that this step should not be bypassed to achieve reliable readings of the glaze microstructures and sound interpretations of the technological procedures. We suggest the adoption by the scientific community of an alternative vision on glaze microstructures to turn thin section petrography for glaze microstructures into a new specialized petrographic discipline. Such an approach, if intensively developed, has the potential to reduce the time and costs of scientific investigations in this specific domain. In fact, it can provide key reference data for the identification of the crystallites in ceramic glazes, avoiding the repetition of exhaustive protocols of expensive integrated analyses.

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Geschwind, Carl-Henry. "The Beginnings of Microscopic Petrography in the United States, 1870-1885." Earth Sciences History 13, no. 1 (January 1, 1994): 35–46. http://dx.doi.org/10.17704/eshi.13.1.x3888321461141qu.

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In the 1860's and 70's, microscopic petrography flourished in Germany, where descriptions and classifications of rocks were highly valued for their own sake. American geologists, however, were more interested in stratigraphical correlations and had relatively little use for petrographical details. Thus, such Americans as George Hawes and Alexis Julien, who attempted to introduce the microscope for purely petrographical work in the early 1870's, had great difficulties in finding an audience. During the late 1870's, however, a number of American geologists-including federal geologists working amongst the volcanic rocks of the West, state geologists mapping in the Lake Superior region, and mining geologists examining the Comstock Lode and the Leadville district-came to appreciate the aid microscopic petrography could provide for stratigraphical correlations. This growing interest led to the hiring of a number of microscopic petrographers around 1880. These petrographers were trained in Germany, where they had imbibed the German passion for petrography for its own sake, but most of them adapted themselves to the American practice of using petrography for stratigraphy. Unlike many of their German counterparts, these American petrographers spent a substantial portion of their time in the field and combined mapping with microscopic examinations to solve stratigraphical problems. Thus, the different scientific cultures of Germany and the U.S. significantly affected the ways in which the petrographic microscope was used.

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Safari Farrokhad, Sajad, Gholam Reza Lashkaripour, Nasser Hafezi Moghaddas, Saeed Aligholi, and Mohanad Muayad Sabri Sabri. "The Effect of the Petrography, Mineralogy, and Physical Properties of Limestone on Mode I Fracture Toughness under Dry and Saturated Conditions." Applied Sciences 12, no. 18 (September 15, 2022): 9237. http://dx.doi.org/10.3390/app12189237.

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Determining the fracture toughness of rock materials is a challenging, costly, and time-consuming task, as fabricating a sharp crack in rock specimens will lead to failure of the specimen, and preparing specimens for determining the rock fracture toughness requires special equipment. In this paper, the relationship between mode I fracture toughness (KIC) with the rock index properties, mineralogy, and petrography of limestone is investigated using simple nonlinear and simple/multiple linear regression analyses to provide alternative methods for estimating the fracture toughness of limestones. The cracked chevron notched Brazilian disk (CCNBD) method was applied to 30 limestones with different petrographic and mineralogical characteristics under both dry and saturated conditions. Moreover, the index properties of the same rocks, including the density, porosity, electrical resistivity, P and S wave velocities, Schmidt rebound hardness, and point load index, were determined. According to the statistical analyses, a classification based on the petrography of the studied rocks was required for predicting the fracture toughness from index properties. By classifying the limestones based on petrography, reliable relationships with high correlations can be introduced for estimating the fracture toughness of different limestones using simple tests.

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Van den Kerkhof, Alfons M., and Ulrich F. Hein. "Fluid inclusion petrography." Lithos 55, no. 1-4 (January 2001): 27–47. http://dx.doi.org/10.1016/s0024-4937(00)00037-2.

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Sajid, Muhammad, Muhammad Yaseen, Muhammad Zeeshan Ullah, and Ghulam Murtaza. "Textural Implications in Assessment of Physico-Mechanical behaviour of Metavolcanic Rocks from Dir Upper, north western Pakistan." International Journal of Economic and Environmental Geology 11, no. 3 (December 4, 2020): 1–10. http://dx.doi.org/10.46660/ijeeg.vol11.iss3.2020.469.

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The Dir-Utror meta-volcanics from the south western portion of the Kohistan arc in northern Pakistan areanalyzed in term of their petrography, physico-mechanical properties. Field observations and petrography show thecollected representative samples to be fine-grained meta-andesites (FMA), coarse-grained meta-andesites (CMA) andagglomerate (AG). The relationship between petrography and physico-mechanical properties has been investigatedwhich inferred the grain size to be the major factor, alongside grains’ shape, arrangement and size distribution as wellas degree of mineral alteration significantly affecting the mechanical behavior of rocks. The CMA yield more strength(98 MPa) than FMA (93 MPa) due to its lesser degree of mineral alteration, inequigranular texture, lack of preferredmineral alignment, relatively low porosity and water absorption. The lower strength of agglomerate (57 MPa)corresponds to abundance of soft minerals (calcite), exotic rock fragments and coarse-grained texture. Based onphysico-mechanical properties including specific gravity, bulk density, aggregate impact value, Los Angeles abrasionvalue and unconfined compressive strength (UCS), these rocks fall within permissible range to be utilized for multipleengineering purposes including dimension stones and foundation materials for other civil structures. However,petrographic investigations reveal excessive amount of reactive silica in these rocks making them prone to alkali-silicareactivity in concrete works with ordinary Portland cement (OPC). Hence these rocks are not recommended for use assole aggregate material or low-alkali cement is recommended, if used.

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French, W. J. "Concrete petrography: a review." Quarterly Journal of Engineering Geology and Hydrogeology 24, no. 1 (February 1991): 17–48. http://dx.doi.org/10.1144/gsl.qjeg.1991.024.01.03.

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Dissertations / Theses on the topic "Petrography"

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Ergene, Muge. "Petrography." Master's thesis, METU, 2009. http://etd.lib.metu.edu.tr/upload/2/12610105/index.pdf.

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Dorans, Hugh. "METEX: An expert system for metamorphic petrography." Thesis, Aston University, 1988. http://publications.aston.ac.uk/14370/.

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Classification of metamorphic rocks is normally carried out using a poorly defined, subjective classification scheme making this an area in which many undergraduate geologists experience difficulties. An expert system to assist in such classification is presented which is capable of classifying rocks and also giving further details about a particular rock type. A mixed knowledge representation is used with frame, semantic and production rule systems available. Classification in the domain requires that different facets of a rock be classified. To implement this, rocks are represented by 'context' frames with slots representing each facet. Slots are satisfied by calling a pre-defined ruleset to carry out the necessary inference. The inference is handled by an interpreter which uses a dependency graph representation for the propagation of evidence. Uncertainty is handled by the system using a combination of the MYCIN certainty factor system and the Dempster -Shafer range mechanism. This allows for positive and negative reasoning, with rules capable of representing necessity and sufficiency of evidence, whilst also allowing the implementation of an alpha-beta pruning algorithm to guide question selection during inference. The system also utilizes a semantic net type structure to allow the expert to encode simple relationships between terms enabling rules to be written with a sensible level of abstraction. Using frames to represent rock types where subclassification is possible allows the knowledge base to be built in a modular t'ashion with subclassirication frames only defined once the higher level of classification is functioning. Rulesets can similurly be added in modular fashio'n with the individual rules being essenrially declurative allowing for simple updating and maintenance. The knowledge base so far developed for metamorphic classification serves to demonstrate the performance of the interpreter design whilst also moving some way towards providing a useful assistant to the non-expert metamorphic petrologist. The system demonstrates the possibilities for a fully developed knowledge base to handle the classification of igneous, sedimentary and metamorphic rocks. The current knowledge base and interpreter have been evaluated by potential users and experts. The results of the evaluation show that the system performs to an acceptable level and should be of use as a tool for both undergraduates and rese:1rchers from outside the metamorphic petrogr:1phy field.

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Eakin, Paul Andrew. "The organic petrography and geochemistry of uraniferous hydrocarbons." Thesis, Queen's University Belfast, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.336031.

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Skopec, Robert A. "Geomechanical evaluation of a poorly consolidated sandstone with applications to horizontal drilling, borehole stability, reservoir compaction, and sand control." Thesis, University of Aberdeen, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.274852.

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Decreasing strength with increasing effective compressive strength, referred to as "cap" behavior is often attributed to pore collapse and a reduction in pore throat apertures during early drawdown. Over-consolidation with only a slight increase in effective stress creates secondary fine particles that leads to formation damage and permeability decline. Grain crushing and the creation of a secondary fines population exacerbates pore blockage that results from mobilization of loosely attached kaolinite or other non-load bearing fine particles. Pore volume compressibility data indicate that compaction effects are significant and pose a potentially serious production problem during depletion. Pore volume lost during depletion is non-recoverable and will not "rebound." Re-injection of water will not re-establish the pore volume lost during compaction as a result of reservoir depletion. Compressibility and compaction trends in the Lower Captain Sandstone contradict several petroleum industry theories. Effective confining pressure and effective mean stress were higher under uniaxial strain boundary versus triaxial conditions and play a greater role in compaction than shear stresses. Captain pseudo shales exhibit strain-softening behavior and peak strengths are quite close to residual strengths. Captain pseudo shales clearly have residual load-bearing capacity and strain-softening promotes plasticicity. Use of standard core analysis methods to measure pore volume compressibility and fines migration potential are highly discouraged in unconsolidated as well as consolidated sandstones. Petrographic, mineralogical, and routine petrophysical analyses are essential in the interpretation of rock mechanics data.

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Kenyon-Roberts, Stephen M. "The petrography and distribution of some calcite sea hardgrounds." Thesis, University of Reading, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.318580.

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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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Rothschild, Alison. "Ground ice petrography, Sand Hills Moraine, southern Banks Island, N.W.T." Thesis, University of Ottawa (Canada), 1986. http://hdl.handle.net/10393/5504.

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Grimmer, Stephen C. "Geochemistry and petrography of alkali volcanics from the Oslo Palaeorift Norway." Thesis, Keele University, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.293779.

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Röser, Georg. "Petrography, physical properties, and geotechnical behavior ofmodern sediments, Southern Chile Trench." [S.l. : s.n.], 2007. http://nbn-resolving.de/urn:nbn:de:bsz:25-opus-42037.

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Ali, Abdulmajid Muhammad. "Integrated Petrography, Geochemistry and Petrophysical Characteristics of Miri Formation, Sarawak, Malaysia." Thesis, Curtin University, 2022. http://hdl.handle.net/20.500.11937/87929.

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An integrated approach (Petrography, Mineralogy, Geochemistry, and Petrophysics) was used to elucidate the paleoweathering, provenance and tectonic setting of the Miri Formation and its reservoir potential. The research suggests that the sediments of the Miri Formation were mainly recycled from the Rajang Group, undergone moderate to intense weathering and deposited in an evolving active to passive margin setting. The reservoir quality of the Miri Formation has been assessed and their controlling factors are addressed.

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Books on the topic "Petrography"

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Sedimentary petrography. Englewood Cliffs, N.J: PTR Prentice Hall, 1993.

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Petrography laboratory manual: Handspecimen and thin section petrography. 3rd ed. Long Grove, Ill: Waveland Press, 2009.

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Hibbard, M. J. Petrography to petrogenesis. Englewood Cliffs, N.J: Prentice Hall, 1995.

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DeHayes, SM, and D. Stark, eds. Petrography of Cementitious Materials. 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959: ASTM International, 1994. http://dx.doi.org/10.1520/stp1215-eb.

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1953-, DeHayes Sharon M., Stark D, and Symposium on the Petrography of Cementitious Materials (1993 : Atlanta, Ga.), eds. Petrography of cementitious materials. Philadelphia, PA: ASTM, 1994.

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1904-, Pettijohn F. J., ed. Manual of sedimentary petrography. Tulsa, Okla: Society of Economic Paleontologists and Mineralogists, 1988.

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1946-, Vaughan David J., ed. Ore microscopy and ore petrography. 2nd ed. New York: Wiley, 1994.

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1946-, Vaughan David J., ed. Ore microscopy and ore petrography. 2nd ed. New York: Wiley, 1994.

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Philpotts, Anthony R. Petrography of igneous and metamorphic rocks. Englewood Cliffs, N.J: Prentice Hall, 1989.

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1936-, Betancourt Philip P., ed. Thin-section petrography of ceramic materials. Philadelphia, Pa: INSTAP Academic Press, 2009.

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Book chapters on the topic "Petrography"

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Whitbread, Ian K. "Petrography." In Encyclopedia of Geoarchaeology, 660–64. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_23.

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Ghose, Naresh Chandra, Nilanjan Chatterjee, and Fareeduddin. "Petrography." In A Petrographic Atlas of Ophiolite, 57–78. New Delhi: Springer India, 2013. http://dx.doi.org/10.1007/978-81-322-1569-1_5.

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Whitbread, Ian K. "Petrography." In Encyclopedia of Geoarchaeology, 1–5. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-44600-0_23-1.

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Pande, Chaitanya B. "Petrography." In Geology, Petrography and Geochemistry of Basaltic Rock in Central India, 25–60. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-30574-0_2.

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Dittrich, Thomas, Thomas Seifert, Bernhard Schulz, Steffen Hagemann, Axel Gerdes, and Jörg Pfänder. "Petrography and Mineralogy." In SpringerBriefs in World Mineral Deposits, 61–75. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10943-1_3.

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Garrison, Ervan. "Petrography for Archaeological Geology." In Natural Science in Archaeology, 145–78. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-30232-4_6.

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Garrison, Ervan G. "Petrography for Archaeological Geology." In Natural Science in Archaeology, 153–205. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05163-4_6.

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Hutton, Adrian C. "Organic Petrography: Principles and Techniques." In Composition, Geochemistry and Conversion of Oil Shales, 1–16. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0317-6_1.

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Hutton, Adrian C. "Organic Petrography of Oil Shales." In Composition, Geochemistry and Conversion of Oil Shales, 17–33. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0317-6_2.

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Hassan, Safiya M. "Petrography of Carbonates (Microfacies Association)." In Sequence Stratigraphy of the Lower Miocene Moghra Formation in the Qattara Depression, North Western Desert, Egypt, 89–108. Heidelberg: Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-00330-6_4.

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Conference papers on the topic "Petrography"

1

Tacker, R. C., and Marissa L. Jerden. "INFRARED PETROGRAPHY OF THIN SECTIONS." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312322.

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Prayoga, A. "Geochemical Characteristics of Oil and Reservoir Depositional Environment Analysis of Talang Akar Formation (TAF) in The “AMP” Field, Jabung Block, Jambi Sub-Basin, South Sumatra Basin." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-sg-249.

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The purpose of this study is to determine the oil characteristics consisting of the source of the organic material and depositional environment in which oil samples that charged the reservoir develop and the depositional environment of the potential reservoir of TAF in the "AMP" Field. Oil characteristics analysis used geochemical data of oil samples from the TAF using biomarker data from GC/GCMS namely the Pristane/Phytane (Pr/Ph) value ratio, Pristane/nC17 (Pr/nC17), Hopane/Sterane, C27 Sterane, C28 Sterane, C29 Sterane, and carbon isotope data were showing the depositional environmental conditions in which oil samples develop. Subsurface data such as core, well logs, mud logs and petrography have an excellent resolution to determine lithology, texture, sedimentary structure and composition of rocks that can be used to determine the depositional environment by integrating with biostratigraphy data. Petrography data and RCAL were used to determine porosity and permeability. The analysis of the value from the Pr/Ph ratio with Pr/nC17 show that oil samples are developed in an environment of terrestrial oxic conditions, and are supported by the comparison of Hopane/Sterane values with Pr/Ph ratio, which shows that samples were deposited in an environment of the highly oxidizing terrestrial condition. It can be interpreted that the oil sample has an organic material source dominantly derived from a high level of vegetation based at the terrestrial environment on the triangle C27-C28-C29. Carbon isotope data also show that oil samples have a dominant source of organic material from terrestrial. Based on the core, well logs, mud logs, petrography, and biostratigraphy analysis, depositional of reservoir rock is a subaqueous distributary channel that formed in the Early Miocene age (NN1-NN3). Petrographic observation shows that subaqueous distributary channel sandstones as a reservoir rock have visible porosity values from 5.6% to 12.8% (poor to fair), RCAL data shows that measured porosity has values from 7.2% to 24.9% (fair to very good) and permeability from 0.03 mD to 654 mD.

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Koeshidayatullah, Ardiansyah, Jonathan L. Payne, Daniel J. Lehrmann, Michele Morsilli, and Khalid Al-Ramadan. "REAL-TIME CARBONATE PETROGRAPHY WITH DEEP LEARNING." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356742.

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Remeysen, K., and R. Swennen. "Combination of Computed Tomography and Petrography in Reservoir Characterization." In IOR 2005 - 13th European Symposium on Improved Oil Recovery. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.12.p04.

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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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Mason, Daniel, Chase Rerrick, David Gibson, and Darren Mark. "PETROGRAPHY, AGE AND PROVENANCE OF MAFIC DIKES, WESTERN MAINE." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311027.

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Perrier, Jhamila A. "PETROGRAPHY OF TRIASSIC IGNEOUS ROCKS FROM THE NORTH PAMIR." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323228.

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O'Keefe, Jennifer M. K., Thomas D. Demchuk, Christopher N. Denison, and Nicholas Cowey. "ORGANIC PETROGRAPHY OF HOOPER FORMATION COALS, CENTRAL TEXAS, USA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305547.

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Armenta Mejía, Jorge Rafael, Lorenzo Mattos, and César O. Torres. "Automated coal petrography for macerals characterization using histograms technique." In 8th Ibero American Optics Meeting/11th Latin American Meeting on Optics, Lasers, and Applications, edited by Manuel Filipe P. C. Martins Costa. SPIE, 2013. http://dx.doi.org/10.1117/12.2026389.

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Gibson, David, Donald Osthoff, and Chase Rerrick. "Field Relations, Petrography and Provenance of Mafic Dikes, Western Maine." In New England Intercollegiate Geological Conference. Bates College, 2017. http://dx.doi.org/10.26780/2017.001.0015.

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Reports on the topic "Petrography"

1

Jarrett, A. J. M., D. Gross, B. Horsfield, and C. J. Boreham. Organic petrography of Proterozoic shales from northern Australia. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.035.

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Nentwich, F. W. Petrography of Kugmallit Sequence Sandstones, Beaufort - Mackenzie Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/130773.

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Bustin, R. M. High pressure methane absorption isotherms, petrography and vitrinite reflectance analyses. Alaska Division of Geological & Geophysical Surveys, 2002. http://dx.doi.org/10.14509/2859.

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Nentwich, F. W. Petrography of Kugmallit Sequence Sandstones, Beaufort - Mackenzie Basin, Part 1. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/130774.

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Miryan, Jawaduddin, and Tamer Rizaoğlu. Geochemistry and Petrography of Acidic Pumice from Kaymaklı-Nevşehir/Turkey. "Prof. Marin Drinov" Publishing House of Bulgarian Academy of Sciences, January 2018. http://dx.doi.org/10.7546/crabs.2018.01.09.

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Miryan, Jawaduddin, and Tamer Rizaoğlu. Geochemistry and Petrography of Acidic Pumice from Kaymaklı-Nevşehir/Turkey. "Prof. Marin Drinov" Publishing House of Bulgarian Academy of Sciences, January 2018. http://dx.doi.org/10.7546/grabs2018.1.09.

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Myers, M. D. Petrography of Upper Cretaceous and lower Tertiary sandstones: Beaufort-MacKenzie Basin. Alaska Division of Geological & Geophysical Surveys, 1989. http://dx.doi.org/10.14509/1432.

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Pratt, K. C. Technical Note: Custom programming of image analysis applications for coal petrography. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126756.

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Nentwich, F. W. Petrography of Kugmallit Sequence Sandstones, Beaufort - Mackenzie Basin, Part 2, Appendices. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127241.

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Nentwich, F. W. Petrography of Kugmallit Sequence Sandstones, Beaufort - Mackenzie Basin, Part 3, Photographs. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127242.

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