Abstract
Oceanic anoxic events (OAEs) are considered as periods of oxygen deficiency in many oceans; accompanied by accumulation of organic-rich black shales. Mesozoic anoxic events were recognized based on the presence of black shales that are rich in organic matter. The most significant anoxic events during the Mesozoic are the Early Toarcian, the Early Aptian, and the Cenomanian–Turonian. The less significant events are the Valanginian-Hauterivian, the Hauterivian-Barremian, the Aptian-Albian, the Late Albian, the Albian-Cenomanian, and the Coniacian-Santonian. The recognized OAEs in Egypt are the Early Aptian (OAE 1a), the Aptian-Albian (OAE 1b), the Late Albian (OAE 1c), the Albian-Cenomanian (Breistroffer, OAE 1d), and the Cenomanian–Turonian (Bonarelli Event, OAE 2). However, the most widely recoded event is the OAE 2. The Cretaceous oceans hosted huge amounts of organic-rich black shales that sufficient to source all of the hydrocarbons. Black shales are considered as the most important source of hydrocarbons. The exploitation of black shales to generate hydrocarbons becomes a vital substitutional resource for energy. Such utilization of black shales may compensate the shortage of hydrocarbons in Egypt. Detailed filed work and analytical data are required before final estimation of black shale resources in Egypt.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Similar content being viewed by others
References
Al Far, D. M. (1966). Geology and coal deposits of Gebel Maghara, north Sinai, Egypt. Geological Survey of Egypt, paper 37, 59.
Algeo, T. J., & Rowe, H. (2012). Paleoceanographic applications of trace-metal concentration data. Chemical Geology, 324–325, 6–18.
Anan, T. (2010). Sedimentology of the Cenomanian-Turonian succession in west central Sinai, Egypt, (p. 171). Unpublished Ph.D Thesis, Mansoura University, Egypt.
Anan, T. (2014). Facies analysis and sequence stratigraphy of the Cenomanian-Turonian mixed siliciclastic–carbonate sediments in west Sinai. Egypt. Sedimentary Geology, 307, 34–46.
Anan, T., El-Shahat, A., Genedi, A., & Grammer, M. (2013). Depositional environments and sequence architecture of the Raha and Abu Qada formations (Cenomanian-Turonian), west central Sinai. Egypt, Journal of African Earth Sciences, 82, 54–69.
Ando, A., Kaiho, K., Kawahata, H., & Kakegawa, T. (2008). Timing and magnitude of early Aptian extreme warming: Unraveling primary δ18O variation in indurated pelagic carbonates at Deep Sea Drilling Project Site 463, central Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 260(3–4), 463–476.
Arthur, M. A., Dean, W. E., & Pratt, L. M. (1988). Geochemical and climatic effects of increased marine organic-carbon burial at the Cenomanian-Turonian boundary. Nature, 335, 714–717.
Arthur, M. A., & Sageman, B. B. (1994). Marine Black Shales: Depositional mechanisms and environments of ancient deposits. Annual Review of Earth and Planetary Sciences, 22, 499–551.
Beerling, D. J., Lomas, M. R., & Gröcke, D. R. (2002). On the nature of methane gas-hydrate dissociation during the Toarcian and Aptian oceanic anoxic events. American Journal of Science, 302, 28–49.
Berry, W. B., & Wilde, P. (1978). Progressive ventilation of the oceans - an explanation for the distribution of the lower Paleozoic black shales. American Journal of Science, 278, 257–275.
Clerici, A., & Alimonti, G. (2015). Oil shale, shale oil, shale gas and non-conventional hydrocarbons. The European Physical Journal Conferences, 98, 03001. https://doi.org/10.1051/epjconf/20159803001
Danelian, T., Tsikos, H., Gardin, S., Baudin, F., Bellier, J. P., & Emmanuel, L. (2004). Global and regional palaeoceanographic changes as recorded in the mid-Cretaceous (Aptian-Albian) sequence of the Ionian zone (NW Greece). Journal of the Geological Society, 161(4), 703–709.
Dyni, J. R. (2003). Geology and resources of some world oil-shale deposits. Oil Shale, 20, 193–252.
Dyni, J. R. (2006). Geology and resources of some world oil-shale deposits. Scientific Investigation Report (2005–5294) (p. 42). Published by the US Department of the Interior, US Geological Survey, Reston, Virginia.
El-Kammar, M. M. (1993). Organic and inorganic composition of the Upper Cretaceous-Lower Tertiary black shales from Egypt and their hydrocarbon potentialities, Ph.D. Thesis, Faculty of Sciences, (p. 227). Cairo University.
El-Kammar, A. (2008). Upper Cretaceous-Lower Tertiary black shales in Egypt: Possible potential source of energy. Invited Talk. Sedimentology of Egypt, 16, 1–5.
El-Kammar, A. (2017). Oil shale resources in Egypt: The present status and future vision. Arabian Journal of Geosciences, 10, 439.
El-Sabbagh, A., Tantawy, A., Keller, G., Khozyem, H., Spangenberg, J., Adatte, T., & Gertsch, B. (2011). Stratigraphy of the Cenomanian-Turonian oceanic anoxic event OAE2 in shallow shelf sequences of NE Egypt. Cretaceous Research, 32(6), 705–722.
El-Shafeiy, M., Birgel, D., El-Kammar, A., El-Barkooky, A., Wagreich, M., Mohamed, M., & Peckmann, J. (2014). Palaeoecological and postdepositional changes recorded in Campanian-Maastrichtian black shales, Abu Tartur Plateau. Egypt. Cretaceous Research, 50, 38–51.
El-Shinnawi, M., & Sultan, I. (1973). Lithostratigraphy of some subsurface Upper Cretaceous sections in the Gulf of Suez area. Egypt. Acta Geologica Academiae Scientiarum Hungaricae, 17, 469–494.
Erba, E. (1992). Calcareous nannofossil distribution in pelagic rhythmic sediments (Aptian-Albian Piobbico core, central Italy). Rivista Italiana Di Paleontologia e Stratigrafia, 97, 455–484.
Farrimond, P., Eglinton, G., Brassell, S. C., & Jenkyns, H. C. (1990). The Cenomanian/Turonian anoxic event in Europe: An organic geochemical study. Marine and Petroleum Geology, 7(1), 75.
Gangl, S. K., Moy, C. M., Stirling, C. H., Jenkyns, H. C., Crampton, J. S., Clarkson, M. O., Ohneiser, C., & Porcelli, D. (2019). High-resolution records of Oceanic Anoxic Event 2: Insights into the timing, duration and extent of environmental perturbations from the palaeo-South Pacific Ocean. Earth and Planetary Science Letters, 518, 172–182.
Gertsch, B., Keller, G., Adatte, T., Berner, Z., Kassab, A. S., Tantawy, A. A., El-Sabbagh, S., & D. (2010). Cenomanian-Turonian transition in a shallow water sequence of the Sinai. Egypt. International Journal of Earth Sciences, 99(1), 165–182.
Ghorab, M. A. (1961). Abnormal stratigraphic features in Ras Gharib oilfields, Egypt. In 3rd Arab Petroleum Congress (pp. 1–10) Alexandria.
de Graciansky, P. C., Deroo, G., Herbin, J. P., Jacquin, T., Magni, F., Montadert, I., & Müller, C. (1986). Ocean-wide stagnation episodes in the Late Cretaceous. Geological Rundschau, 75, 17–41.
Gradstein, F. M., Ogg, J. G., Schmitz, M. D., & Ogg, G. M. (2012). The Geologic Time Scale 2012 (1st ed., p. 1176). UK, Elsevier.
Greenwood, P. F., Brocks, J. J., Grice, K., Schwark, L., Jaraula, C. M. B., Dick, J. M., & Evans, K. A. (2013). Organic geochemistry and mineralogy I. Characterisation of organic matter associated with metal deposits. Ore Geology Reviews, 50, 1–27.
Gröcke, D., Hesselbo, S. P., & Jenkyns, H. C. (1999). Carbon isotope composition of Lower Cretaceous fossil wood: Ocean-atmosphere chemistry and relation to sea-level change. Geology, 27, 155–158.
Hancock, J. M., & Kauffman, E. G. (1979). The great transgressions of the Late Cretaceous. Journal of the Geological Society of London, 136, 175–186.
Haq, B. U., Hardenbol, J., & Vail, P. R. (1987). Chronology of fluctuating sea levels since the Triassic. Science, 235, 1157–1167.
Heimhofer, U., Hochuli, P. A., Herrle, J. O., Andersen, N., & Weissert, H. (2004). Absence of major vegetation and palaeoatmospheric pCO2 changes associated with oceanic anoxic event 1a (Early Aptian, SE France). Earth and Planetary Science Letters, 223(3–4), 303–318.
Hetzel, A., Böttcher, M. E., Wortmann, U. G., & Brumsack, H. J. (2009). Paleoredox conditions during OAE2 reflected in Demerara Rise sediment geochemistry (ODP Leg 207). Palaeogeography, Palaeoceanography, Palaeoecology, 273(3–4), 302–328.
Huyck, H. L. (1990). Proposed definition of “black shale” and “metalliferous black shale” for IGCP #254. Book of Abstracts, 8th IAGOD Symposium (pp. A183-184). GSC.
Ismail, A. (2002). The biostratigraphic and sequence stratigraphic applications on the Upper Cretaceous succession of Wadi Feiran, southwestern Sinai. Egypt. Egyptian Journal of Geology, 46, 515–533.
Jenkyns, H. C. (1985). The early Toarcian and Cenomanian-Turonian anoxic events in Europe: Comparisons and contrasts. Geologische Rundschau, 74, 505–518.
Jenkyns, H. C. (1988). The Early Toarcian (Jurassic) anoxic event: stratigraphic, sedimentary, and geochemical evidence. American Journal of Science, 288, 101–151.
Jenkyns, H. C. (2010). Geochemistry of oceanic anoxic events. Geochemistry, Geophysics, Geosystems, 11, Q03004.
Jenkyns, H. C., Gröcke, D. R., & Hesselbo, S. P. (2001). Nitrogen isotope evidence for water mass denitrification during the Early Toarcian (Jurassic) Oceanic Anoxic Event. Paleoceanography, 16, 593–603.
Jenkyns, H. C., Jones, C. E., Gröcke, D. R., Hesselbo, S. P., & Parkinson, D. N. (2002). Chemostratigraphy of the Jurassic system; applications, limitations and implications for palaeoceanography. Journal of the Geological Society of London, 159(4), 351–378.
Jenkyns, H. C., Matthews, A., Tsikos, H., & Erel, Y. (2007). Nitrate reduction, sulfate reduction, and sedimentary iron isotope evolution during the Cenomanian-Turonian oceanic anoxic event. Paleoceanography, 22, PA3208.
Kafousia, N., Karakitsios, V., & Jenkyns, H. C. (2010). Preliminary data from the first record of the Toarcian Oceanic Anoxic Event in the sediments of the Pindos Zone (Greece). Bulletin of the Geological Society of Greece, 43(2), 627–633.
Kaiser, D., Konovalov, S., Schultz-Bull, D., & Waniek, J. J. (2017). Organic matter along longitudinal and vertical gradients in the Black Sea. Deep Sea Research Part I: Oceanographic Research Papers, 129, 22–31.
Karakitsios, V., Kafousia1, N., & Tsikos, H. (2010). A Review of Oceanic Anoxic Events as recorded in the Mesozoic sedimentary record of mainland Greece. Hellenic Journal of Geosciences, 45, 123–132.
Kassem, A., Sharaf, L., Baghdady, A., & El-Naby, A. (2020). Cenomanian/Turonian oceanic anoxic event 2 in October oil field, central Gulf of Suez. Egypt. Journal of African Earth Sciences., 165, 103817.
Keller, G., Adatte, T., Burns, S., & Tantawy, A. A. (2002). High-stress paleoenvironment during the late Maastrichtian to early Paleocene in central Egypt. Palaeogeography, Palaeoclimatology, Palaeoecology, 187, 35–60.
Kemp, D. B., Coe, A. L., Cohen, A. S., & Schwark, L. (2005). Astronomical pacing of methane release in the Early Jurassic period. Nature, 437(7057), 396–399.
Khalil, H. (2007). Macrobiostratigraphical, paleoecological and palaeobiographical studies of the Cenomanian/Turonian transition of Wadi Watir (El Sheikh Attia), Sinai. Egypt. Egyptian Journal of Paleontology, 7, 245–267.
Kora, M., Shahin, A., & Semiet, A. (1993). Biostratigraphy and macrofauna of the Cenomanian exposures in west central Sinai. Egypt. Mansoura Science Bulletin, 20, 227–260.
Kuroda, J., & Ohkouchi, N. (2006). Implication of spatiotemporal distribution of black shales deposited during the Cretaceous Oceanic Anoxic Event-2. Paleontological Research, 10(4), 345–358.
Kuypers, M. M., Pancost, R. D., Nijenhuis, I. A., & Sinninghe Damsté, J. S. (2002). Enhanced productivity led to increased organic carbon burial in the euxinic North Atlantic basin during the late Cenomanian oceanic anoxic event. Paleoceanography, 17(4), 1051. https://doi.org/10.1029/2000PA000569
Leckie, R. M., Bralower, T. J., & Cashman, R. (2002). Oceanic anoxic events and plankton evolution: biotic response to tectonic forcing during the Mid-Cretaceous. Paleoceanography, 17, PA1041.
Lille, U. (2003). Current knowledge on the origin and structure of Estonian kukersite kerogen. Oil Shale, 20, 253–263.
Lipinski, M., Warning, B., & Brumsack, H. J. (2003). Trace metal signatures of Jurassic/Cretaceous black shales from the Norwegian shelf and the Barents Sea. Palaeogeography Palaeoclimatology Palaeoecology, 190, 459–475.
Lüning, S., Kolonic, S., Belhadj, E. M., Belhadj, Z., Cota, L., Baric, G., & Wagner, T. (2004). Integrated depositional model for the Cenomanian-Turonian organic-rich strata in North Africa. Earth Science Reviews, 64, 51–117.
Malinverno, A., Erba, E., & Herbert, T. D. (2010). Orbital tuning as an inverse problem: Chronology of the early Aptian oceanic anoxic event 1a (Selli Level) in the Cismon APTICORE, Paleoceanography, 25, PA2203. https://doi.org/10.1029/2009PA001769.
Mazzini, A., Svensen, H., Leanza, H. A., Corfu, F., & Planke, S. (2010). Early Jurassic shale chemostratigraphy and U-Pb ages from the Neuquén Basin (Argentina(: Implications for the Toarcian oceanic anoxic event. Earth and Planetary Science Letters, 297, 633–645.
Meyers, S. R., Siewert, S. E., Singer, B. S., Sageman, B. B., Condon, D. J., Obradovich, J. D., Jicha, B. R., & Sawyer, D. A. (2012). Intercalibration of radio isotopic and astrochronologic time scales for the Cenomanian-Turonian boundary interval, Western Interior Basin, USA. Geology, 40, 7–10.
Miller, K. G., Miller, M. A., Browning, J. V., Wright, J. D., Mountain, G. S., Katz, M. E., Sugarman, P. J., Cramer, B. S., Christie-Blick, N., & Pekar, S. (2005). The Phanerozoic Record of Global Sea-Level Change. Science, 310, 1293–1298.
Mort, H. P., Adatte, T., Keller, G., Bartels, D., Föllmi, K. B., Steinmann, P., Berner, Z., & Chellai, E. H. (2008). Organic carbon deposition and phosphorus accumulation during oceanic anoxic event 2 in Tarfaya. Morocco, Cretaceous Research, 29, 1008–1023.
Mustafa, A., & Ghaly, E. L. (1964). Survey of Quseir shales and other carbonaceous shales in Egypt. Journal of Chemical and Engineering Data, 9(4), 557–567.
Nagm, E., El-Qot, G., & Wilmsen, M. (2014). Stable-isotope stratigraphy of the Cenomanian-Turonian (Upper Cretaceous) boundary event (CTBE) in Wadi Qena, Eastern Desert. Egypt Journal of African Earth Sciences, 100, 524–531.
North, F. K. (1979). Episodes of source-sediment deposition (1). Journal of Petroleum Geology, 2, 199–218.
Parviainen, A., & Loukola-Ruskeeniemi, K. (2019). Environmental impact of mineralised black shales. Earth-Science Reviews, 192, 65–90.
Percival, L. M. E., Tedeschi, L. R., Creaser, R. A., Bottini, C., Erba, E., Giraud, F., Svensen, H., Savian, J., Trindade, R., Coccioni, R., Frontalini, F., Jovane, L., Mather, T. A., & Jenkyns, H. C. (2021). Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a). Global and Planetary Change, 103461.
Remírez, M. N., & Algeo, T. J. (2020). Carbon-cycle changes during the Toarcian (Early Jurassic) and implications for regional versus global drivers of the Toarcian oceanic anoxic event. Earth-Science Reviews, 209, 103283.
Rimstidt, J. D., Chermak, J. A., & Schreiber, M. E. (2017). Processes that control mineral and element abundances in shales. Earth-Science Reviews, 171, 383–399.
Röhl, J., Schmid-Röhl, A., Oschmann, W., Frimmel, A., & Schwark, L. (2001). The Posidonia Shale (Lower Toarcian) of SW-Germany: An oxygen-depleted ecosystem controlled by sea level and palaeoclimate. Palaeogeography Palaeoclimatology Palaeoecology, 165, 27–52.
Sageman, B. B., & Lyons, T. W. (2003). Geochemistry of fine-grained sediments and sedimentary rocks. In MacKenzie, F. (Ed.), Treatise on Geochemistry (Vol. 7, pp. 115–158). Elsvier.
Sageman, B. B., Meyers, S. R., & Arthur, M. A. (2006). Orbital time scale and new C-isotope record for Cenomanian-Turonian boundary stratotype. Geology, 34, 125–128.
Said, R. (1962). The Geology of Egypt (p. 377). Elsevier.
Said, R. (1990). The Geology of Egypt (p. 729). Elsevier.
Salama, Y., & Abdel-Gawad, G. (2018). Early Cretaceous Oceanic Anoxic Events in Rudist-Bearing Succession, North Egypt. In Boughdiri, M., Bádenas, B., Selden, P., Jaillard, E., Bengtson, P., & Granier, B. (Eds.), Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas. Proceedings of the 1st Springer Conference of the Arabian Journal of Geosciences (CAJG-1) (pp. 183–185).
Schlanger, S. O., & Cita, M. B. (1982). Nature and Origin of Cretaceous Carbon-rich Facies (p. 229). Academic Press.
Schlanger, S. O., & Jenkyns, H. C. (1976). Cretaceous oceanic anoxic events: Causes and consequence. Geologie En Mijnbouw, 55(3–4), 179–184.
Schouten, S., Van Kaam-Peters, H. M. E., Rijpstra, W. I. C., Schoell, M., & Sinninghe Damsté, J. S. (2000). Effects of an oceanic anoxic event on the stable carbon isotopic composition of Early Toarcian carbon. American Journal of Science, 300, 1–22.
Shahin, A. (2007). Oxygen and carbon isotopes and foraminiferal biostratigraphy of the Cenomanian-Turonian succession in Gabal Nezzazat, southwestern Sinai. Egypt. Revue De Paléobiologie, Genève, 26, 359–379.
Slack, J. F., Selby, D., & Dumoulin, J. A. (2015). Hydrothermal, biogenic, and seawater components in metalliferous Black Shales of the Brooks Range, Alaska: Synsedimentary metal enrichment in a carbonate ramp setting. Economic Geology, 110, 653–675.
Takashima, R., Nishi, H., Yamanaka, T., Hayashi, K., Waseda, A., Obuse, A., Tomosugi, T., Deguchi, N., & Mochizuki, S. (2010). High-resolution terrestrial carbon isotope and planktic foraminiferal records of the upper Cenomanian to the lower Campanian in the Northwest Pacific. Earth and Planetary Science Letters, 289(3–4), 570–582.
Thiede, J., & van Andel, T. H. (1977). The palaeo- environment of anaerobic sediments in the late Mesozoic South Atlantic Ocean. Earth and Planetary Science Letters, 33, 301–309.
Troger, U. (1984). The oil shale potential of Egypt. Berliner Geowissenschaftliche Abhandlungenen (a), 50, 375–380.
Tsikos, H., Jenkyns, H. C., Walsworth-Bell, B., Petrizzo, M. R., Forster, A., Kolonic, S., Erba, E., Premoli Silva, I., Baas, M., Wagner, T., & Sinninghe Damsté, J. S. (2004). Carbon-isotope stratigraphy recorded by the Cenomanian-Turonian Oceanic Anoxic Event: Correlation and implications based on three key localities. Journal of the Geological Society of London, 161, 711–719.
Voigt, S., Erbacher, J., Mutterlose, J., Weiss, W., Westerhold, T., Wiese, F., Wilmsen, M., & Wonik, T. (2008). The Cenomanian—Turonian of the Wunstorf section (north Germany): Global stratigraphic reference section and new orbital time scale for oceanic anoxic event 2. Newsletters on Stratigraphy, 43, 65–89.
Voigt, S., Gale, A. S., & Voigt, T. (2006). Sea-level change, carbon cycling and palaeoclimate during the Late Cenomanian of northwest Europe; an integrated palaeoenvironmental analysis. Cretaceous Research, 27, 836–858.
Wang, C. S., Hu, X. M., Jansa, L., Wan, X. Q., & Tao, R. (2001). The Cenomanian-Turonian anoxic event in southern Tibet. Cretaceous Research, 22(4), 481–490.
Westermann, S., Stein, M., Matera, V., Fiet, N., Fleitmann, D., Adatte, T., & Föllmi, K. B. (2013). Rapid changes in the redox conditions of the western Tethys Ocean during the early Aptian oceanic anoxic event. Geochimica Et Cosmochimica Acta, 121, 467–486.
Wignall, P. (1994). Black Shales (p. 127). Clarendon Press.
Wignall, P. B., Hallam, A., Newton, R. J., Sha, J. G., Reeves, E., Mattioli, E., & Crowley, S. (2006). An eastern Tethyan (Tibetan) record of the Early Jurassic (Toarcian) mass extinction event. Geobiology, 4(3), 179–190.
Wignall, P B. & Twitchett, R. J. (2002). Extent, duration, and nature of the Permian-Triassic superanoxic event. In Koeberl, C. & Leod, K. G. (Eds.), Catastrophic Events and Mass Extinctions: Impacts and beyond (Vol. 356, pp. 395–413). Geological Society of America Special Paper.
**e, X., Li, M., Xu, J., Snowdon, L. R., & Volkman, J. K. (2020). Geochemical characterization and artificial thermal maturation of kerogen density fractions from the Eocene Huadian oil shale. NE China. Organic Geochemistry, 144, 103947.
Young, S., Loukola-Ruskeeniemi, K., & Pratt, L. (2013). Reactions of hydrothermal solutions with organic matter in Palaeoproterozoic black shales at Talvivaara, Finland: Evidence from multiple sulfur isotopes. Earth Planetary Science Letters, 367, 1–14.
Zhang, L., Zhang, X., Li, S., & Wang, Q. (2012). Comprehensive utilization of oil shale and prospect Analysis. Energy Procedia, 17, 39–43.
Zhou, X., Jenkyns, H. C., Owens, J. D., Junium, C. K., Zheng, X. Y., Sageman, B. B., Hardisty, D. S., Lyons, T. W., Ridgwell, A., & Lu, Z. (2015). Upper ocean oxygenation dynamics from I/Ca ratios during the Cenomanian-Turonian OAE 2. Paleoceanography, 30, 510–526.
Zhuravlev, A. Y., & Wood, R. A. (1996). Anoxia as the cause of the mid-Early Cambrian (Botomian) extinction event. Geology, 24, 311–314.
Zobaa, M., Oboh-Ikuenobe, F., & Ibrahim, M. (2011). The Cenomanian/Turonian oceanic anoxic event in the Razzak Field, north Western Desert, Egypt: Source rock potential and paleoenvironmental association. Marine and Petroleum Geology, 28, 1475–1482.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2023 The Author(s), under exclusive license to Springer Nature Switzerland AG
About this chapter
Cite this chapter
Anan, T., El-Shahat, A. (2023). Mesozoic Oceanic Anoxic Events and the Associated Black Shale Deposits as a Potential Source of Energy. In: Hamimi, Z., et al. The Phanerozoic Geology and Natural Resources of Egypt. Advances in Science, Technology & Innovation. Springer, Cham. https://doi.org/10.1007/978-3-030-95637-0_7
Download citation
DOI: https://doi.org/10.1007/978-3-030-95637-0_7
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-030-95636-3
Online ISBN: 978-3-030-95637-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)