Relevant bibliographies by topics / Rocks, Igneous

Contents

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

Academic literature on the topic 'Rocks, Igneous'

Author: Grafiati
Published: 4 June 2021
Last updated: 4 March 2023

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Journal articles on the topic "Rocks, Igneous"

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Lee, Dong-Keun, Duk-Ho Chung, Woong-Hyeon Jeon, and Chul-Min Lee. "Analysis of igneous rock classification process by earth science teachers using eye trackers." Korean Association For Learner-Centered Curriculum And Instruction 22, no. 15 (August 15, 2022): 461–77. http://dx.doi.org/10.22251/jlcci.2022.22.15.461.

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Objectives The purpose of this study is to find out the characteristics that earth science teachers show in the process of classifying igneous rocks and the difficulties in classifying igneous rocks. Methods To this end, the researchers collected gaze data and language data in the process of classifying igneous rocks by using a Eyetracker(Tobii Ⅱ) and a think-aloud method from five high school earth science teachers in Jeollabuk-do. Then, the collected data were analyzed using the gaze analysis program and the semantic network analysis, respectively. Results First, in the process of classifying igneous rocks, earth science teacher’s gaze fixation duration was long in the order of diorite, andesite, rhyolite, gabbro, basalt, and granite. Second, in the semantic network for the classification of igneous rocks by earth science teachers, the eigenvector centrality of words related to the apparent characteristics of rocks such as “particles” and “rock color” was high. Third, in the process of classifying igneous rocks, earth science teachers found it difficult to determine the range of characteristics that determine each igneous rock, that is, the range of rock colors, particle sizes, stripes, etc. In other words, earth science teachers found it most difficult to distinguish diorite, and granite was the easiest to distinguish. In the process of classifying igneous rocks, they classified igneous rocks mainly based on the size of the particles that make up the rocks and the color shown by the rocks rather than the minerals that make up the rocks. In addition, earth science teachers were unclear about the scope of the criteria for classification of igneous rocks. Conclusions Earth science teachers need to clearly establish personal standards for the classification of igneous rocks. And personal standard for rock classification can be established through various observation experiences as well as the geological knowledge they perceive. Therefore, earth science teachers should be provided with various types of rocks and typical rocks for extensive observation experiences, such as activities to observe rocks and various types of rocks.
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Ahadnejad, Vahid, Ann Hirt, Mohammad-Vali Valizadeh, and Saeed Bokani. "The ammonium content in the Malayer igneous and metamorphic rocks (Sanandaj-Sirjan Zone, Western Iran)." Geologica Carpathica 62, no. 2 (April 1, 2011): 171–80. http://dx.doi.org/10.2478/v10096-011-0014-y.

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The ammonium content in the Malayer igneous and metamorphic rocks (Sanandaj-Sirjan Zone, Western Iran)The ammonium (NH4+) contents of the Malayer area (Western Iran) have been determined by using the colorimetric method on 26 samples from igneous and metamorphic rocks. This is the first analysis of the ammonium contents of Iranian metamorphic and igneous rocks. The average ammonium content of metamorphic rocks decreases from low-grade to high-grade metamorphic rocks (in ppm): slate 580, phyllite 515, andalusite schist 242. In the case of igneous rocks, it decreases from felsic to mafic igneous types (in ppm): granites 39, monzonite 20, diorite 17, gabbro 10. Altered granitic rocks show enrichment in NH4+(mean 61 ppm). The high concentration of ammonium in Malayer granites may indicate metasedimentary rocks as protoliths rather than meta-igneous rocks. These granitic rocks (S-types) have high K-bearing rock-forming minerals such as biotite, muscovite and K-feldspar which their potassium could substitute with ammonium. In addition, the high ammonium content of metasediments is probably due to inheritance of nitrogen from organic matter in the original sediments. The hydrothermally altered samples of granitic rocks show highly enrichment of ammonium suggesting external sources which intruded additional content by either interaction with metasedimentary country rocks or meteoritic solutions.
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Xiang, Kui, Liangjun Yan, Zhigang Wang, and Yao Lu. "Comprehensive Physical Properties and Exploration Potential of the Permian Igneous Rocks in the Southwestern Sichuan Basin." Minerals 12, no. 7 (June 21, 2022): 789. http://dx.doi.org/10.3390/min12070789.

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The Permian igneous rocks in the Sichuan Basin represent a major breakthrough, opening up a new prospect for oil and gas exploration, and igneous reservoirs have become a new field of oil and gas exploration. Gravity-magnetic-electric exploration is an effective means of identifying igneous rocks and helps in reducing the multiplicity of the prediction results. However, the lithology of igneous rocks is quite different, and the exploration theory and evaluation techniques need urgently to be improved. In order to deeply study the response characteristics of the gravity-magnetic-electric and physical properties of the Permian igneous rocks in the Sichuan Basin and their relationships with the reservoir parameters, physical property testing was carried out on outcrop samples of the Permian igneous rocks in southwestern Sichuan. The comprehensive physical properties of the samples with different lithologies, including basalt, tuff, and volcanic breccia, were analyzed and studied. Based on the geological characteristics of the igneous rocks, such as the mineral composition, microstructure, and reservoir properties, a multi-parameter intersection relationship model for the resistivity, polarizability, density, magnetic susceptibility, and their relationships with the reservoir parameters was established, and effective parameters favorable for igneous rock identification and reservoir evaluation were identified. The results of this study provide a physical basis and technical support for non-seismic exploration of igneous oil and gas reservoirs in the Sichuan Basin.
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Le Maitre, R. W. "Alkaline Igneous rocks." Geochimica et Cosmochimica Acta 52, no. 9 (September 1988): 2343. http://dx.doi.org/10.1016/0016-7037(88)90137-8.

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De Wit, Maarten J. "Alkaline igneous rocks." Lithos 24, no. 1 (December 1989): 81–82. http://dx.doi.org/10.1016/0024-4937(89)90017-0.

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Reynolds, Owen. "Ambiguous Igneous Rocks." Archives of Dermatology 143, no. 1 (January 1, 2007): 115. http://dx.doi.org/10.1001/archderm.143.1.118.

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Sastrawiharja, Khumaedi, Satria Bijaksana, Umar Fauzi, and Linus Ampang Pasasa. "Anisotropy of Magnetic Susceptibility and Elemental Compositions in Andesitic Rocks." Indonesian Journal of Physics 19, no. 1 (November 3, 2016): 19–22. http://dx.doi.org/10.5614/itb.ijp.2008.19.1.3.

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Igneous rocks, including andesites, are composed of these major elements: Si, Ti, Al, Fe, Mn, Ca, Mg, Na, K, and P. Variation in the composition of these elements, which occur mostly as oxides, determines the overall physical properties of the rocks. Not surprisingly, classification of igneous rocks is also based on the quantity of these major oxides. In this study, elemental compositions of andesitic rocks from the Island of Java will be compared to the anisotropy of magnetic susceptibility (AMS) as a part of our effort to explore the possibility of using rock magnetic parameters in classifying igneous rocks. The objective is to check whether AMS parameters could serve as alternative to chemical analysis. To do so, we have measured the AMS and geochemical composition of andesitic rock samples from 10 different sites across Central Java and Yogyakarta. The results show that there are significant correlations between the abundance of certain elements with AMS parameters, for example, the abundance of Fe and Al with magnetic lineation and the abundance of Al with degree of anisotropy. These results show that magnetic parameters have a good change to be use as predictors for major elements composition in igneous rocks.
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Potter, Joanna, Andrew H. Rankin, Peter J. Treloar, Valentin A. Nivin, Wupao Ting, and Pei Ni. "A preliminary study of methane inclusions in alkaline igneous rocks of the Kola igneous province, Russia: implications for the origin of methane in igneous rocks." European Journal of Mineralogy 10, no. 6 (December 1, 1998): 1167–80. http://dx.doi.org/10.1127/ejm/10/6/1167.

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Sari, Y. K., A. D. Titisari, I. W. Warmada, and F. Hakim. "Petrogenesis of Botorubuh igneous rocks at Gunungkidul: A preliminary study for paleomagmatism phenomenon in the southern beach of Yogyakarta - Indonesia." IOP Conference Series: Earth and Environmental Science 851, no. 1 (October 1, 2021): 012029. http://dx.doi.org/10.1088/1755-1315/851/1/012029.

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Abstract Botorubuh Beach is located at Southern Beach of Gunungkidul, in the Southern Mountain of Yogyakarta - Indonesia and is a promontory composed of Middle - Late Miocene igneous rock with a columnar jointing structure. This isolated igneous rock area is surrounded by limestone. Therefore, the regional geological map of Surakarta-Giritontro classifies this area as the Punung-Wonosari Formation which is dominated by limestone. Because of the geological phenomenon of the isolated igneous rock area, it is necessary to study the petrogenesis of the igneous rocks at the area. The petrogenesis research is based on a preliminary study of the petrographical and geochemical characteristics of this igneous rock samples. The petrographic identification of andesite samples shows porphyritic, trachytic, oscillatory zoning, and sieve textures. The results of geochemical analysis (major and trace elements) show that the rock samples are are classified to andesite rocks and calc-alkaline suites. These rocks are enriched in LILEs (Rb, Ba, K) and depleted in HFSEs (Nb, Ti, Ce). Additionally, REE shows a slight enrichment of light-REE and a slight negative anomaly of Eu. The patterns of the trace elements including REE show a typical pattern of calc alkaline arc. Petrographical and geochemical characteristics suggest evidence of magma differentiation process, that is by a mechanism of crystallization fractionation. The andesite was formed in relation to a Middle – Late Miocene paleomagmatism and the Late Miocene-Pliocene subduction zone.
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Krivolutskaya, N. A., and N. I. Bryanchaninova. "Olivines of igneous rocks." Russian Journal of General Chemistry 81, no. 6 (June 2011): 1302–14. http://dx.doi.org/10.1134/s1070363211060363.

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Dissertations / Theses on the topic "Rocks, Igneous"

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Esfarjani, H. R. "Engineering properties of basic igneous rocks." Thesis, University of Newcastle Upon Tyne, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.374739.

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Reichow, Marc K. "Permo-Triassic igneous rocks of Siberia, Russia." Thesis, University of Leicester, 2004. http://hdl.handle.net/2381/7669.

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Widespread basaltic volcanism occurred in the region of the West Siberian Basin (WSB) and the Taimyr Peninsula in central Russia, and voluminous A-type magmatism within the Mongolian-Transbaikalian belt in southeast Siberia, during Permo-Triassic times. New 40Ar/39Ar age determinations on plagioclase grains from deep boreholes in the WSB reveal that the basalts were erupted at ~250 million years ago. This is synchronous with the main period of the Siberian Traps volcanism, which was located farther east. The age and geochemical data presented confirm that the WSB basalts are part of the Siberian Traps, and at least double the confirmed area of the volcanic province as a whole. The larger area of volcanism strengthens the link between the volcanism and the end-Permian mass extinction. Furthermore, it is argued that the WSB and Taimyr basalts are genetically related to the Siberian Traps basalts, especially the Nadezhdinsky Suite found at Noril’sk. This suite immediately preceded the main pulse of volcanism that extruded lava over large areas of the Siberian Craton. Magma volume and timing constraints strongly suggest that a mantle plume was involved in the formation of the Earth’s largest continental flood basalt province. The Mongolian-Transbaikalian granitoid belt covers over 600,000 km2 with over 350 single A-type plutons. New U-Pb geochronological data presented here demonstrate that no plutonic complex dated is 250 Ma old. Although mantle-derived material played a prominent role in the granitoid generation, these melts may have been generated by processes other than decompressional melting within the head of a mantle plume. The new U-Pb ages and other observations contradict the idea of a relation between the Siberian plume and magmatic activity in the territory of Transbaikalia. An alternative preferred model inducing up rise of asthenospheric material includes slab break-off after a long period of subduction.
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Chan, Heung-ngai. "Igneous and metamorphic rocks from SW Cyprus and NW Syria evidence for Cretaceous microplate collision and subsequent tectonic events in the Eastern Mediterranean /." Click to view the E-thesis via HKUTO, 2004. http://sunzi.lib.hku.hk/hkuto/record/B30711940.

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Chen, Qinfang. "Geophysical and radiometric investigation of weathered igneous rocks in Hong Kong /." Hong Kong : University of Hong Kong, 2002. http://sunzi.lib.hku.hk/hkuto/record.jsp?B23621497.

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Riter, Joyce Christine Alexis. "Geochemical and tectonic evolution of the Colorado Plateau mantle lithosphere : evidence from Grand Canyon mantle xenoliths /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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Pattie, Andrew J. D. "Hybridization of basic wall rocks in xenolithic igneous complexes." Thesis, Aston University, 1989. http://publications.aston.ac.uk/14371/.

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Lee, Paula M. "Spatial, temporal, and petrogenetic relationship of basaltic and lamprophyric dikes and sills of the Raton Basin, southern Colorado and northern New Mexico." Diss., Columbia, Mo. : University of Missouri-Columbia, 2005. http://hdl.handle.net/10355/5848.

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Thesis (M.S.)--University of Missouri-Columbia, 2005.
The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (July 11, 2006) Includes bibliographical references.
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Getson, Jacqueline. "Effect of plagioclase crystallization on liquid and magma viscosity in the Anorthite-diopside-dorsterite-quartz system." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4628.

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Thesis (M.S.) University of Missouri-Columbia, 2006.
The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (June 25, 2007) Includes bibliographical references.
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Rabae, Abdussalam. "Geophysical investigations of the Anglo-Brabant Massif." Thesis, University of Bristol, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.386227.

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Jarvis, Richard Allan. "Crystallization and melting in geological fluid mechanics." Thesis, University of Cambridge, 1991. https://www.repository.cam.ac.uk/handle/1810/275236.

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Books on the topic "Rocks, Igneous"

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Le Maitre, R. W., A. Streckeisen, B. Zanettin, M. J. Le Bas, B. Bonin, and P. Bateman, eds. Igneous Rocks. Cambridge: Cambridge University Press, 2002. http://dx.doi.org/10.1017/cbo9780511535581.

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Oxlade, Chris. Igneous rocks. Chicago, Ill: Heinemann Library, 2011.

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Owings, Lisa. Igneous Rocks. Minneapolis, MN: Core Library, an imprint of ABDO Publishing, 2015.

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Oxlade, Chris. Igneous rocks. Chicago, Ill: Heinemann Library, 2011.

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Unearthing igneous rocks. New York: PowerKids Press, 2014.

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G, Fitton J., Upton B. G. J, and Geological Society of London, eds. Alkaline igneous rocks. Oxford [Oxfordshire]: Published for the Geological Society by Blackwell Scientific Publications, 1987.

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Igneous petrology. 3rd ed. Sudbury, Mass: Jones and Bartlett Publishers, 2007.

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McBirney, Alexander R. Igneous petrology. 2nd ed. Boston: Jones and Bartlett Publishers, 1993.

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Igneous rock. Oxford: Raintree, 2008.

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Igneous rock. Oxford: Raintree, 2007.

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Book chapters on the topic "Rocks, Igneous"

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de Oliveira Frascá, Maria Heloisa Barros, and Eliane Aparecida Del Lama. "Igneous Rocks." In Selective Neck Dissection for Oral Cancer, 1–6. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-12127-7_166-1.

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Okrusch, Martin, and Hartwig E. Frimmel. "Igneous Rocks." In Springer Textbooks in Earth Sciences, Geography and Environment, 249–74. Berlin, Heidelberg: Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-662-57316-7_13.

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Fernandes, Isabel, Helena Martins, Maria dos Anjos Ribeiro, Fernando Noronha, Maarten A. T. M. Broekmans, and Ian Sims. "Igneous Rocks." In Petrographic Atlas: Characterisation of Aggregates Regarding Potential Reactivity to Alkalis, 9–41. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-017-7383-6_2.

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Zhang, Jianfang, Chaohui Zhu, Longwu Wang, Xiaoliang Cai, Ruijun Gong, Xiaoyou Chen, Jianguo Wang, Mingguang Gu, Zongyao Zhou, and Yuandong Liu. "Igneous Rocks." In The China Geological Survey Series, 173–255. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-1788-4_3.

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Corretge, L. G., O. Suarez, and G. Galan. "Igneous Rocks." In Pre-Mesozoic Geology of Iberia, 115–28. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-83980-1_10.

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Sanchez Carretero, R., L. Eguiluz, E. Pascual, and M. Carracedo. "Igneous Rocks." In Pre-Mesozoic Geology of Iberia, 292–313. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-83980-1_19.

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Corretge, L. G., and O. Suarez. "Igneous Rocks." In Pre-Mesozoic Geology of Iberia, 72–79. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-83980-1_5.

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Frascá, Maria Heloisa Barros de Oliveira, and Eliane Aparecida Del Lama. "Igneous Rocks." In Encyclopedia of Earth Sciences Series, 504–9. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73568-9_166.

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Bennison, G. M. "Igneous rocks." In An Introduction to Geological Structures and Maps, 58–63. Boston, MA: Springer US, 1990. http://dx.doi.org/10.1007/978-1-4615-9630-1_8.

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Davis, Donald W. "Uranium–Lead, Igneous Rocks." In Encyclopedia of Scientific Dating Methods, 894–98. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_202.

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Conference papers on the topic "Rocks, Igneous"

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Anuka, Agnes, Celestine Udie, and Grace Aquah. "Prospects, Challenges and Way Forward in the Use of Hydraulic Fracturing For Oil and Gas Production From Igneous Rocks." In SPE Nigeria Annual International Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/207106-ms.

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Abstract Commercial accumulation of hydrocarbons occurs mostly in sedimentary rocks due to their high porosity and permeability. Increased global energy demand has necessitated the need for unconventional methods of oil production. The world is gradually moving away from reliability on conventional oils. The need to ensure global energy sustainability has necessitated an urgent diversion to unconventional oils. In recent times, hydrocarbon accumulations have been found in igneous rocks. Their low porosity and permeability however prevents commercial production as oil and gas found in these rocks will not flow. Hydraulic fracturing is useful in increasing rock porosity as it involves the breaking of rocks to allow oil and gas trapped inside to flow to producing wells. This method is useful in developing unconventional resources such as oil and gas found in igneous rocks. This research explores the prospects, challenges and way forward in the use of hydraulic fracturing to increase the porosity of igneous rock for commercial production of oil and gas.
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Meredith, Philip, and John Browning. "MICROSTRUCTURAL CONTROLS ON THERMAL CRACKING IN IGNEOUS ROCKS." In PRF2022—Progressive Failure of Brittle Rocks. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022pr-376046.

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Millett, J. C. F. "The shock Hugoniot of two igneous rocks." In Shock compression of condensed matter. AIP, 2000. http://dx.doi.org/10.1063/1.1303687.

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Shekov, Vitali. "CORRELATION OF MULTI-DIMENSIONAL FRACTURING IN IGNEOUS ROCKS." In 16th International Multidisciplinary Scientific GeoConference SGEM2016. Stef92 Technology, 2016. http://dx.doi.org/10.5593/sgem2016/b12/s03.027.

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Hasenstab, Eric, Christiane Schnabel, Jonas Tusch, Christian S. Marien, Jörg Elis Hoffmann, Martin Van Kranendonk, and Carsten Münker. "138La-138Ce Isotope Systematics of Archean Igneous Rocks." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.969.

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Long, Leon E. "CHARACTERIZING IGNEOUS ROCKS AND MINERALS USING MATRIX ANALYSIS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283528.

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Hurter, S. J., and H. N. Pollack. "Cooling of Igneous Rocks from the Serra Geral Event." In 3rd International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609-pdb.324.672.

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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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Ge, Yunlong, Wensheng Wu, Ruigang Wang, and Liuqiong He. "Porosity evaluation of igneous rocks based on deep learning." In SEG Technical Program Expanded Abstracts 2019. Society of Exploration Geophysicists, 2019. http://dx.doi.org/10.1190/segam2019-3211813.1.

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Denisova, Iu V. "History of accessory minerals from igneous rocks Subpolar Ural." In ТЕНДЕНЦИИ РАЗВИТИЯ НАУКИ И ОБРАЗОВАНИЯ. НИЦ «Л-Журнал», 2019. http://dx.doi.org/10.18411/lj-03-2019-103.

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Reports on the topic "Rocks, Igneous"

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Champion, D. C., L. Highet, and J. P. Thorne. Archean alkaline and related igneous rocks of Australia. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.036.

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Champion, D. C., L. Highet, and M. Buddee. Mesozoic alkaline and related igneous rocks of Australia. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.038.

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Hickmott, D. D., J. W. Carey, J. Stimac, A. Larocque, R. Abell, E. Gauerke, and A. Eppler. Lead immobilization in thermally remediated soils and igneous rocks. Office of Scientific and Technical Information (OSTI), June 1997. http://dx.doi.org/10.2172/481516.

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Peterson, T. D., and K. L. Currie. Analcite-bearing igneous rocks from the Crowsnest Formation, southwestern Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134223.

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Bédard, J. H., and A. N. LeCheminant. Alnöites and related rocks, Monteregian Hills alkaline igneous province, Québec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/211711.

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Wypych, Alicja. Geochemical interpretation of samples of igneous rocks from northeast Tanacross. Alaska Division of Geological & Geophysical Surveys, 2020. http://dx.doi.org/10.14509/30542.

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Solie, D. N., T. K. Bundtzen, and W. G. Gilbert. K/Ar ages of igneous rocks in the McGrath Quadrangle, Alaska. Alaska Division of Geological & Geophysical Surveys, 1991. http://dx.doi.org/10.14509/1517.

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Pe-Piper, G., D. J. W. Piper, M. J. Keen, and N. J. McMillan. Igneous rocks of the continental margin [Chapter 2: tectonic and geophysical overview]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/132696.

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9

Wypych, Alicja. Geochemistry of the igneous rocks in the Ladue River-Mount Fairplay area. Alaska Division of Geological & Geophysical Surveys, August 2021. http://dx.doi.org/10.14509/30739.

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Pe-Piper, G., J. Nagle, and D. J. W. Piper. Igneous rocks and hydrothermal alteration of Lower Carboniferous sedimentary rocks, Clarke Head, Minas Fault Zone, western Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/306289.

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