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Journal articles on the topic 'Petrology'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 July 2024

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1

Li, Hui. "Petrology’s Role in Unveiling Geochemical Controls on Soil Contamination: China’s Environmental Assessment (2000-2022)." Innovation in Science and Technology 3, no. 1 (January 2024): 40–50. http://dx.doi.org/10.56397/ist.2024.01.06.

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This review explores the pivotal role of petrology in unraveling geochemical controls on soil contamination, focusing on China’s environmental assessment from 2000 to 2022. Petrology, as a cornerstone of geology, investigates rocks’ mineral composition and origin. In the context of soil contamination, it elucidates the geological factors influencing soil composition, contaminant sources, and their interactions. The paper examines the interconnectedness of petrology and geochemistry, emphasizing their symbiotic relationship in understanding soil contamination. Key sections include an overview of petrological techniques, historical context of soil contamination in China, geochemical patterns in Chinese soils, challenges, and future directions. The findings underscore petrology’s significance, offering insights into environmental policies, sustainable soil management, and recommendations for future research. The synthesis of petrological insights proves indispensable in navigating the complexities of soil contamination, fostering informed decision-making, and ensuring sustainable environmental stewardship.

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2

Kretz, Ralph. "Petrology." Earth-Science Reviews 30, no. 3-4 (June 1991): 328–29. http://dx.doi.org/10.1016/0012-8252(91)90008-4.

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3

Michel-Lévy, Mireille Christophe, and Michèle Bourot-Denise. "A New Look at the Galim (a) and Galim (b) Meteorites." Mineralogical Magazine 52, no. 367 (September 1988): 519–25. http://dx.doi.org/10.1180/minmag.1988.052.367.12.

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AbstractSmall stones were recovered from a meteorite shower observed in Cameroon on November 13, 1952. The majority are LL6 specimens, Galim (a), but one is a chondrule-rich enstatite chondrite, Galim (b). Petrology and mineral chemistry were determined on polished sections of both types. Galim (a) has undergone multiple brecciation. During the first, chromite apparently recrystallized in healed fractures under more reducing conditions than those which prevailed when the silicates recrystallized. Galim (b) shows some features of petrologic type 3 but differs considerably from the other unequilibrated E chondrites. It is suggested that Galim (a) and Galim (b) belong to the same meteorite shower.

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4

Gaetani, G. A. "SOFTWARE:Igneous Petrology." Science 282, no. 5395 (December 4, 1998): 1834–35. http://dx.doi.org/10.1126/science.282.5395.1834.

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5

Tankard, Anthony J. "Sedimentary Petrology." Sedimentary Geology 152, no. 1-2 (September 2002): 159–60. http://dx.doi.org/10.1016/s0037-0738(01)00254-8.

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6

Varma, Atul Kumar. "Organic Petrology." Gondwana Research 3, no. 2 (April 2000): 284–86. http://dx.doi.org/10.1016/s1342-937x(05)70115-5.

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7

Burley, Brian J. "Igneous petrology." Geochimica et Cosmochimica Acta 52, no. 3 (March 1988): 798. http://dx.doi.org/10.1016/0016-7037(88)90345-6.

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8

Helz, R. T. "Igneous petrology." Journal of Volcanology and Geothermal Research 24, no. 3-4 (May 1985): 361–62. http://dx.doi.org/10.1016/0377-0273(85)90080-0.

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9

Postma, George. "Sedimentary petrology." Sedimentary Geology 84, no. 1-4 (April 1993): 249. http://dx.doi.org/10.1016/0037-0738(93)90064-c.

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10

Marsh, B. D. "Enclaves and Granite Petrology. Developments in Petrology, 13." Lithos 29, no. 1-2 (December 1992): 158–59. http://dx.doi.org/10.1016/0024-4937(92)90040-6.

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11

Yoder, H. S. "Timetable of Petrology." Journal of Geological Education 41, no. 5 (November 1993): 447–89. http://dx.doi.org/10.5408/0022-1368-41.5.447.

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12

BERKEY, CHARLES P. "THE NEW PETROLOGY." Bulletin of the Geological Society of China 1, no. 1-4 (May 29, 2009): 12–26. http://dx.doi.org/10.1111/j.1755-6724.1922.mp11-4004.x.

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13

KHAWLIE, M. "Computer in petrology." Geology Today 4, no. 1 (January 1988): 18. http://dx.doi.org/10.1111/j.1365-2451.1988.tb00535.x.

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14

Turcotte, Donald L. "Fractals in petrology." Lithos 65, no. 3-4 (December 2002): 261–71. http://dx.doi.org/10.1016/s0024-4937(02)00194-9.

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15

McSween, Harry Y. "Petrology on Mars." American Mineralogist 100, no. 11-12 (November 2015): 2380–95. http://dx.doi.org/10.2138/am-2015-5257.

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16

Barker, Daniel S. "Dictionary of petrology." Earth-Science Reviews 22, no. 1 (May 1985): 96. http://dx.doi.org/10.1016/0012-8252(85)90043-1.

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17

Miyashiro, Akiho. "Dictionary of petrology." Journal of Volcanology and Geothermal Research 24, no. 3-4 (May 1985): 367–69. http://dx.doi.org/10.1016/0377-0273(85)90084-8.

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18

Taylor, S. R. "Dictionary of petrology." Lithos 18 (January 1985): 64–65. http://dx.doi.org/10.1016/0024-4937(85)90007-6.

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19

Sabine, Peter A. "Setting Standards in Petrology: The Commission on Systematics in Petrology." Episodes 12, no. 2 (June 1, 1989): 83–86. http://dx.doi.org/10.18814/epiiugs/1989/v12i2/004.

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20

NAUMANN, T. "Petrology and Geochemistry of Volcan Cerro Azul: Petrologic Diversity among the Western Galapagos Volcanoes." Journal of Petrology 43, no. 5 (May 1, 2002): 859–83. http://dx.doi.org/10.1093/petrology/43.5.859.

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21

TORIUMI, Mitsuhiro. "The Modern Metamorphic Petrology and Its Future. Strategy of Metamorphic Petrology." Journal of Geography (Chigaku Zasshi) 106, no. 5 (1997): 745–49. http://dx.doi.org/10.5026/jgeography.106.5_745.

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22

Garcia, Mike. "Volcanology geochemistry & petrology." Eos, Transactions American Geophysical Union 76, no. 17 (April 25, 1995): 172. http://dx.doi.org/10.1029/eo076i017p00172-01.

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23

Williams, Michael L. "Principles of Metamorphic Petrology." Eos, Transactions American Geophysical Union 90, no. 21 (May 26, 2009): 185–86. http://dx.doi.org/10.1029/2009eo210007.

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24

Hoskin, Paul W. O. "Igneous and Metamorphic Petrology." Precambrian Research 128, no. 1-2 (January 2004): 197–98. http://dx.doi.org/10.1016/j.precamres.2003.08.003.

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25

Poli, Stefano, and Max W. Schmidt. "Petrology of Subducted Slabs." Annual Review of Earth and Planetary Sciences 30, no. 1 (May 2002): 207–35. http://dx.doi.org/10.1146/annurev.earth.30.091201.140550.

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26

Cas, Ray. "Sedimentary petrology (2nd ed.)." Chemical Geology 107, no. 1-2 (July 1993): 202. http://dx.doi.org/10.1016/0009-2541(93)90112-v.

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27

Sørensen, Henning. "Enclaves and aranite petrology." Chemical Geology 103, no. 1-4 (January 1993): 293–94. http://dx.doi.org/10.1016/0009-2541(93)90308-6.

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28

Allen, P. A. "Sedimentary petrology (2nd Edition)." Marine and Petroleum Geology 9, no. 1 (February 1992): 107. http://dx.doi.org/10.1016/0264-8172(92)90009-4.

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29

Chalapathi Rao, N. V. "Petrology: Principles and practice." Journal of the Geological Society of India 84, no. 6 (December 2014): 739. http://dx.doi.org/10.1007/s12594-014-0184-1.

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30

Das, Subhajyoti. "Petrology in groundwater study." Journal of the Geological Society of India 85, no. 2 (February 2015): 258–60. http://dx.doi.org/10.1007/s12594-015-0213-8.

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31

Rock, N. M. S. "Enclaves and granite petrology." Earth-Science Reviews 33, no. 1 (August 1992): 41–43. http://dx.doi.org/10.1016/0012-8252(92)90069-6.

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32

Termier, Henri. "Igneous and metamorphic petrology." Chemical Geology 49, no. 4 (June 1985): 457–59. http://dx.doi.org/10.1016/0009-2541(85)90009-9.

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33

Dixon, H. Roberta. "Petrology of metamorphic rocks." Chemical Geology 49, no. 4 (June 1985): 459–60. http://dx.doi.org/10.1016/0009-2541(85)90010-5.

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34

Gromet, L. Peter. "Principles of igneous petrology." Geochimica et Cosmochimica Acta 50, no. 7 (July 1986): 1567. http://dx.doi.org/10.1016/0016-7037(86)90336-4.

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35

Rykkje, Johannes M. "SEM in petrology science." Ultramicroscopy 24, no. 1 (January 1988): 76. http://dx.doi.org/10.1016/0304-3991(88)90357-9.

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36

Yaxley, G. M., and G. P. Brey. "Foreword: The Roles of Petrology and Experimental Petrology in Understanding Global Tectonics." Journal of Petrology 49, no. 4 (October 11, 2007): 587–89. http://dx.doi.org/10.1093/petrology/egn016.

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37

Powolny, Tomasz, and Magdalena Dumańska-Słowik. "Review of existing systems of jaspers nomenclature and classification in Poland and worldwide." Gospodarka Surowcami Mineralnymi 33, no. 2 (June 27, 2017): 43–52. http://dx.doi.org/10.1515/gospo-2017-0011.

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Abstract Nowadays, the term “jasper” is variably defined in petrology and gemology. The unification of the nomenclature and the classification of jaspers seems to be an essential challenge for petrologists worldwide. This misnomer is very commonly used among sellers or collectors of various gemstones. Therefore, a huge diversity in the mineralogical composition, geological settings and genesis of particular “spotted stones” is reported. In this paper the term “jasper” is proposed for all “spotted stones” which have technical properties that make them useful for jewelry and in the production of small stone accessories. Nevertheless, the introduction and approval of the term “true jasper” for rocks of hydrothermal- metasomatic origin and metamorphosed volcanogenic-sedimentary products to petrologic nomenclature is recommended. Different types of jaspers and related rocks have various economic significance. Jaspers or jasper-like rocks are decorative gemstones applied in jewelry, whereas others may be used as refractory materials or feldspar raw materials. In contrast, the petrographic research of jasperoids is useful during prospecting new ore deposits.

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38

Gouanvic, Yves, and Claude Gagny. "Reflection sur l'utilisation des experimentations pour la comprehension de la genese des aplo-pegmatites litees (cas de Santa Comba); reply." Bulletin de la Société Géologique de France I, no. 2 (March 1, 1985): 273–76. http://dx.doi.org/10.2113/gssgfbull.i.2.273.

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Abstract M. Pichavant contests the magmatic character of our aplo-pegmatitic layering. Some methodological considerations are expressed; without questionning the usefulness of data from experimental petrology, the greatest care must be taken in their utilizations without the knowledge of geological objects. The arguments of structural petrology [our article, Y. Gouanvic and C. Gagny, 1983] and new analytical data permit us to refute M. Pichavant's argumentation and to maintain our magmatic hypothesis.

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39

Auzende, Anne-Line, Bertrand Devouard, Sté phane Guillot, Isabelle Daniel, Alain Baronnet, and Jean-Marc Lardeaux. "Serpentinites from Central Cuba: petrology and HRTEM study." European Journal of Mineralogy 14, no. 5 (September 27, 2002): 905–14. http://dx.doi.org/10.1127/0935-1221/2002/0014-0905.

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40

Hovorka, Dušan. "Mineralogy and petrology serving society: challenges for the 21st century." Mineralogia 40, no. 1-4 (January 1, 2009): 15–30. http://dx.doi.org/10.2478/v10002-009-0005-0.

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Mineralogy and petrology serving society: challenges for the 21st centuryOne of the topical problems of science in general at present is spreading the newest discoveries among population as well as among the decision-makers. "Mineralogical sciences" (mineralogy, geochemistry, petrology) affect the wide spectrum of human activities. Such an influence can already be traced in prehistory, and in the modern age the significance of the mentioned geoscience branches is on the increase. The author presents here a review of selected applications of mineralogical sciences in the development of mankind.

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41

Ohba, Tsukasa. "Case study and event analysis for mitigation of unpredictable volcanic hazard." Impact 2020, no. 3 (May 13, 2020): 26–28. http://dx.doi.org/10.21820/23987073.2020.3.26.

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Volcanology is an extremely important scientific discipline. Shedding light on how and why volcanoes erupt, how eruptions can be predicted and their impact on humans and the environment is crucial to public safety, economies and businesses. Understanding volcanoes means eruptions can be anticipated and at-risk communities can be forewarned, enabling them to implement mitigation measures. Professor Tsukasa Ohba is a scientist based at the Graduate School of International Resource Studies, Akita University, Japan, and specialises in volcanology and petrology. Ohba and his team are focusing on volcanic phenomena including: phreatic eruptions (a steam-driven eruption driven by the heat from magma interacting with water); lahar (volcanic mudflow); and monogenetic basalt eruptions (which consist of a group of small monogenetic volcanoes, each of which erupts only once). The researchers are working to understand the mechanisms of these phenomena using Petrology. Petrology is one of the traditional methods in volcanology but has not been applied to disastrous eruptions before. The teams research will contribute to volcanic hazard mitigation.

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42

Resimic-Saric, Kristina, Vladica Cvetkovic, and Kadosa Balogh. "Radiometric K/ag data as evidence of the geodynamic evolution of the Zdraljica ophiolitic complex, central Serbia." Annales g?ologiques de la Peninsule balkanique, no. 66 (2005): 73–79. http://dx.doi.org/10.2298/gabp0566073r.

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The study presents age data and petrologic characteristics of igneous rocks of the Zdraljica ophiolitic complex (ZOC), situated in central Serbia, 150 km south of Belgrade. The complex consists predominately of a MORB/VAB-like tholeutic suite, represented mostly by gabbros and diabases. The tholeiitic suite is intruded by calc-alkaline intermediate and acid magmas of a VA-affinity, which presumably formed in a pre-collisional setting. The whole complex is intruded by peraluminous granite magmas. The crystallization age of the calc-alkaline pre-collisional quartzdiorite is 168.4?6.7 Ma and it post-dates the formation of the here exposed ocean?ic crust. Geological evidence suggest that the emplacement of the complex occurred during the Upper Jurassic. With respect to their petrology and age, the Zdraljica ophiolitic rocks are similar to the south Apuseni Mts. ophiolites, situated to the north, and to the Kursumija and Guevgeli ophiolites, situated to the south. All these ophiolites probably formed as parts of a single Jurassic belt, which can be termed the eastern branch of the Vardar Zone.

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43

Li, Hui. "Geochemistry and Petrology: Collaborative Roles in Resource Exploration and Environmental Research." Innovation in Science and Technology 2, no. 5 (September 2023): 33–37. http://dx.doi.org/10.56397/ist.2023.09.04.

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Geochemistry and petrology, as distinct yet interrelated fields within geology, play pivotal roles in understanding Earth’s composition, processes, and history. This paper explores the collaborative synergy between these disciplines and their significance in resource exploration and environmental research. It delves into their fundamental principles, applications, and emerging trends, highlighting successful interdisciplinary projects. Despite communication challenges and funding limitations, the future promises exciting opportunities for innovation and discovery through continued collaboration. As we address pressing global challenges, the partnership between geochemistry and petrology remains vital for a sustainable and resilient future.

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44

Hole, Malcolm J. "Chapter 4.1b Antarctic Peninsula: petrology." Geological Society, London, Memoirs 55, no. 1 (2021): 327–43. http://dx.doi.org/10.1144/m55-2018-40.

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AbstractScattered occurrences of Miocene–Recent volcanic rocks of the alkaline intraplate association represent one of the last expressions of magmatism along the Antarctic Peninsula. The volcanic rocks were erupted after the cessation of subduction which stopped following a series of northward-younging ridge crest–trench collisions. Volcanism has been linked to the development of a growing slab window beneath the extinct convergent margin. Geochemically, lavas range from olivine tholeiite through to basanite and tephrite. Previous studies have emphasized the slab-window tectonic setting as key to allowing melting of peridotite in the asthenospheric void caused by the passage of the slab beneath the locus of volcanism. This hypothesis is revisited in the light of more recent petrological research, and an origin from melting of subducted slab-hosted pyroxenite is considered here to be a more viable alternative for their petrogenesis. Because of the simple geometry of ridge subduction, and the well-established chronology of ridge crest–trench collisions, the Antarctic Peninsula remains a key region for understanding the transition from active to passive margin resulting from cessation of subduction. However, there are still some key issues relating to their tectonomagmatic association, and, principally, the poor geochronological control on the volcanic rocks requires urgent attention.

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45

Van Houten, Franklyn B. "Krynine, Pettijohn, and Sedimentary Petrology." Journal of Geological Education 37, no. 4 (September 1989): 241–42. http://dx.doi.org/10.5408/0022-1368-37.4.241.

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46

Admakin, L. A. "Petrology of uranium-bearing coal." Coke and Chemistry 53, no. 3 (March 2010): 77–81. http://dx.doi.org/10.3103/s1068364x10030014.

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47

SUWA, Kanenori. "Amalgamators of mineralogy and petrology." Journal of the Mineralogical Society of Japan 19, no. 5 (1990): 265–72. http://dx.doi.org/10.2465/gkk1952.19.265.

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48

SAITO, Takeshi. "Magnetic Petrology: Applications to Volcanology." Journal of Geography (Chigaku Zasshi) 114, no. 2 (2005): 296–308. http://dx.doi.org/10.5026/jgeography.114.2_296.

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49

Zack, Thomas, and Ellen Kooijman. "Petrology and Geochronology of Rutile." Reviews in Mineralogy and Geochemistry 83, no. 1 (February 1, 2017): 443–67. http://dx.doi.org/10.2138/rmg.2017.83.14.

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50

Katagas, Ch. "WANDERING ABOUT MINERALOGY AND PETROLOGY." Bulletin of the Geological Society of Greece 43, no. 1 (January 19, 2017): 247. http://dx.doi.org/10.12681/bgsg.11178.

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Over the past few years an intense amount of research on various themes stimulated the development of Mineralogy and all its diversity, and many exciting discoveries have been made. New or technologically developed analytical and experimental methods such as ion microprobe, powerful MAS NMR, LA-ICP-MS, IR, Raman, XAS spectroscopies, beams of high intensity, Synchrotron radiation that enhanced the sensitivity of conventional spectroscopic and XRD techniques, beams of neutrons, widely available information and tremendous computing and modelling facilities have turned out to be excellent tools, promoting the ability of mineralogy in solving global and societal challenges. Mineralogy today offers insights into important scientific issues, including sustainable development, evolution of the Earth and origins of life, deep Earth processes, physics and chemistry of Earth materials, fluids, magmas, igneous rocks and time scales, archaeomineralogy, nano-, geo-, and bio- environmental sciences. The mineralogical sciences today are going through a period of rapid expansion and diversification and this trend is going to continue in future. There is now great potential for much interesting work in the latter areas but also the need to somehow protect the coherence of our discipline.

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