Abstract
Based on the photogeological and stratigraphic analysis of Venusian coronae, we have found that (1) late manifestations of volcanic activity on Venus, lobate plains, are weakly related to the formation of coronae. The small number of coronae–sources of lobate plains (~17% of the total population of coronae) indicates that the volcanic activity of the coronae ceased mainly in the pre-Atlian time. Thus, the coronae associated with manifestations of late volcanism in the form of lobate plains are either long-lived volcano-tectonic complexes or structures of the final phases of volcanic activity; their locations mark the regions of long-term volcanism; (2) the small number of coronae formed by rift structures (~14% of the total population) indicates that rifting in the Atlian period did not lead to mass formation of coronae. The majority of Venusian coronae was probably formed in the Fortunian–Guineverian periods of the geological history of Venus. A sharp decrease in the number of coronae formed in the Atlian period may be associated with an increase in the thickness of the lithosphere and an increase in its role as a rheological barrier.
REFERENCES
Airey, M.W., Mather, T.A., Pyle, D.M., and Ghail, R.C., The distribution of volcanism in the Beta-Atla-Themis region of Venus: Its relationships to rifting and implications for global tectonic regimes, J. Geophys. Res., 2017, vol. 122, pp. 1626–1649.
Aittola, M. and Kostama, V.-P., Venusian novae and arachnoids: Characteristics, differences and the effect of the geological environment, Planet. Space Sci., 2001, vol. 48, pp. 1479–1489.
Aittola, M. and Raitala, J., Venusian novae: Classification and associations to volcano-tectonic structures, Sol. Syst. Res., 2007, vol. 41, no. 5, pp. 395–412.
Arvidson, R.E., Greeley, R., Malin, M.C., Saunders, R.S., Izenberg, N., Plaut, J.J., Stofan, E.R., and Shepard, M.K., Surface modification of Venus as inferred from Magellan observation of plains, J. Geophys. Res., 1992, vol. 97, pp. 13303–13317.
Baer, G., Shubert, G., Bindschandler, D.L., and Stofan, E.R., Spatial and temporal relations between coronae and extensional belts, northern Lada Terra, Venus, J. Geophys. Res., 1994, vol. 99, pp. 8355–8369.
Barsukov, V.L., Basilevsky, A.T., Burba, G.A., Bobinna, N.N., Kryuchkov, V.P., Kuzmin, R.O., Nikolaeva, O.V., Pronin, A.A., Ronca, L.B., Chernaya, I.M., Shashkina, V.P., Garanin, A.V., Kushky, E.R., Markov, M.S., Sukhanov, A.L., Kotelnikov, V.A., Rzhiga, O.N., Petrov, G.M., Alexandrov, Yu.N., Sidorenko, A.I., Bogomolov, A.F., Skrypnik, G.I., Bergman, M.Yu., Kudrin, L.V., Bokshtein, I.M., Kronrod, M.A., Chochia, P.A., Tyuflin, Yu.S., Kadnichansky, S.A., and Akim, E.L., The geology and geomorphology of the Venus surface as revealed by radar images obtained by Venera 15 and 16, J. Geophys. Res., 1986, vol. 91, pp. D378–D398.
Basilevsky, A.T. and Head, J.W., Global stratigraphy of Venus: Analysis of a random sample of thirty-six test areas, Earth, Moon and Planets, 1995, vol. 66, pp. 285–336.
Basilevsky, A.T. and Head, J.W., The geologic history of Venus: A stratigraphic view, J. Geophys. Res., 1998, vol. 103, pp. 8531–8544.
Basilevsky, A.T. and Head, J.W., Rifts and large volcanoes on Venus: Global assessment of their age relations with regional plains, J. Geophys. Res., 2000a, vol. 105, p. 611.
Basilevsky, A.T. and Head, J.W., Geologic units on Venus: Evidence for their global correlation, Planet. Space Sci., 2000b, vol. 48, pp. 75–111.
Basilevsky, A.T. and Raitala, J., Morphology of selected novae (astra) from the analysis of Magellan images at Venus, Planet. Space Sci., 2002, vol. 50, pp. 21–39.
Basilevsky, A.T., Aittola, M., Raitala, J., and Head, J.W., Venus astra / novae: Estimates of the absolute time duration of their activity, Icarus, 2009, vol. 203, pp. 337–351.
Campbell, D.B., Stacy, N.J.S., Newman, W.I., Arvidson, R.E., Jones, E.M., Musser, G.S., Roper, A.Y., and Schaber, C., Magellan observations of extended impact crater related features on the surface of Venus, J. Geophys. Res., 1992, vol. 97, pp. 16.249–16.277.
Crumpler, L.S. and Aubele, J., Volcanism on Venus, in Encyclopedia of Volcanoes, Houghton, B., Rymer, H., Stix, J., McNutt, S., and Sigurdson, H., Eds., San Diego: Acad. Press, 2000, pp. 727–770.
Davaille, A., Smrekar, S.E., and Tomlinson, S., Experimental and observational evidence for plume-induced subduction onVenus, Nature Geosci., 2017, vol. 10, no. 5, pp. 349–355.
Grindrod, P.M. and Hoogenboom, T., Coronae on Venus, Astron. Geophys., 2006, vol. 47, p. 21.
Guseva, E.N. and Ivanov, M.A., Spatiotemporal relationships of the groove belts, coronal structures, and rift zones of Venus, Sol. Syst. Res., 2019, vol. 53, no. 6, pp. 411–422.
Guseva, E.N. and Ivanov, M.A., Structures of coronae on Venus: Results of topographic and geologic analysis, Sol. Syst. Res., 2020, vol. 54, no. 6, pp. 497–503.
Guseva, E.N. and Ivanov, M.A., Coronae of Venus: Geological, topographic and morphometric characteristics, Sol. Syst. Res., 2022, vol. 56, no. 2, pp. 76–83.
Hamilton, V.E. and Stofan, E.R., The geomorphology and evolution of Hecate Chasma, Venus, Icarus, 1996, vol. 121, pp. 171–194.
Head, J.W., Crumpler, L.S., Aubele, J.C., Guest, J., and Saunders, R.S., Venus volcanism: Classification of volcanic features and structures, associations, and global distribution from Magellan data, J. Geophys. Res., 1992, vol. 97, pp. 13.153–13.197.
Ivanov, M.A. and Head, J.W., Geology of Venus: Mapping of a global geotraverse at 30N latitude, J. Geophys. Res., 2001, vol. 106, no. E8, pp. 17515–17566.
Ivanov, M.A. and Head, J.W., The Lada Terra rise and Quetzalpetlatl Corona: A region of long-lived mantle upwelling and recent volcanic activity on Venus, Planet. Space Sci., 2010, vol. 58, pp. 1880–1894.
Ivanov, M.A. and Head, J.W., Global geological map of Venus, Planet. Space Sci., 2011, vol. 59, pp. 1559–1600.
Ivanov, M.A. and Head, J.W., The history of volcanism on Venus, Planet. Space Sci., 2013, vol. 84, pp. 66–92.
Ivanov, M.A. and Head, J.W., The history of tectonism on Venus: A stratigraphic analysis, Planet. Space Sci., 2015, vols. 113–114, pp. 10–32.
Ivanov, M.A., Head, J.W., and Basilevsky, A.T., History of the long-wavelength topography of Venus, Sol. Syst. Res., 2015, vol. 49, no. 1, pp. 1–11.
Janes, D.M., Squyres, S.W., Bindschadler, D.L., Baer, G., Schubert, G., Sharpton, V.L., and Stofan, E.R., Geophysical models for the formation and evolution of coronae on Venus, J. Geophys. Res., 1992, vol. 97, no. E10, pp. 16055–16068.
Jellinek, A.M., Lenardic, A., and Manga, M., The influence of interior mantle temperature on the structure of plumes: Heads for Venus, tails for the Earth, Geophys. Res. Lett., 2002, vol. 29, no. 11, pp. 27-1–27-4.
Johnson, C.L. and Richards, M.A., A conceptual model for the relationship between coronae and large-scale mantle dynamics on Venus, J. Geophys. Res., 2003, vol. 108, no. E6, pp. 12-1–12-18.
Jurdy, D.M. and Stefanick, M., Correlation of Venus surface features and geoid, Icarus, 1999, vol. 139, pp. 93–99.
Koch, D.M. and Manga, M., Neutrally buoyant diapirs: A model for Venus coronae, Geophys. Res. Lett., 1996, vol. 23, no. 3, pp. 225–228.
Konopliv, A.S., Banerdt, W.B., and Sjogren, W.L., Venus gravity: 180th degree and order model, Icarus, 1999, vol. 139, pp. 3–18.
Krassilnikov, A.S. and Head, J.W., Novae on Venus: Geology, classification, and evolution, J. Geophys. Res.: Geol., 2003, vol. 108, no. E9, p. 15222148.
Krassilnikov, A.S., Kostama, V.-P., Aittola, M., Guseva, E.N., and Cherkashina, O.S., Relationship of coronae, regional plains and rift zones on Venus, Planet. Space Sci., 2012, vol. 68, pp. 56–75.
Martin, P., Stofan, E.R., Glaze, L.S., and Smrekar, S.E., Coronae of Parga Chasma, Venus, J. Geophys. Res., 2007, vol. 112, no. E4, pp. 1–23.
Masursky, H., Eliason, E., Ford, P.G., McGill, G.E., Pettengill, G.H., Schaber, G.G., and Schubert, G., Pioneer-Venus radar results: Geology from the images and altimetry, J. Geophys. Res., 1980, vol. 85, no. A13, pp. 8232–8260.
McGill, G.E., Steenstrup, S.J., Barton, C., and Ford, P.G., Continental rifting and the origin of Beta Regio, Venus, Geophys. Res. Lett., 1981, vol. 8, no. 7, pp. 737–740.
Nikishin, A.M., Hot sport tectonics on Venus: Implications for rifting and doming, Lunar Planet. Sci. XVII, 1986, pp. 615–616.
Nikishin, A.M., Tectonics of Venus: A review, Earth, Moon, and Planets, 1990, vols. 50/51, pp. 101–125.
Piskorz, D., Elkins-Tanton, L.T., and Smrekarr, S.E., Coronae formation on Venus via extension and lithospheric instability, J. Geophys. Res.: Planets, 2014, vol. 119, pp. 2568–2582.
Pronin, A.A. and Stofan, E.R., Coronae on Venus: Morphology and distribution, Icarus, 1990, vol. 87, pp. 452–474.
Roberts, K.M. and Head, J.W., Large-scale volcanism associated with coronae on Venus: Implications for formation and evolution, Geophys. Res. Lett., 1993, vol. 20, pp. 1111–1114.
Romeo, I., Monte carlo models of the interaction between impact cratering and volcanic resurfacing on Venus: The effect of the Beta–Atla–Themis anomaly, Planet. Space Sci., 2013, vol. 87, pp. 157–172.
Schaber, G.G., Venus: limited extension and volcanism along zones of lithospheric weakness, Geophys. Res. Lett., 1982, vol. 9, pp. 499–502.
Sjogren, W.L., Banerdt, W.B., Chodas, P.W., Konopliv, A.S., Balmino, G., Barriot, J.P., Arkani-Hamed, J., Colvin, T.R., and Davies, M.E., The Venus gravity field and other geodetic parameters, in Venus II, Bougher, S.W., Hunten, D.M., and Phillips, R.J., Eds., Univ. Arizona Press, 1997, pp. 1125–1161.
Smrekar, S.E. and Stofan, E.R., Corona formation and heat loss on Venus by coupled upwelling and delamination, Science, 1997, vol. 277, pp. 1289–1294.
Smrekar, S.E., Stofan, E.R., and Kiefer, W.S., Large volcanic rises on Venus, in Venus II, Bougher, S.W., Hunten, D.M., and Phillips, R.J., Eds., Univ. Arizona Press, 1997, pp. 845–878.
Smrekar, S.E. and Parmentier, E.M., The interaction of mantle plumes with surface thermal and chemical boundary layers: Applications to hotspots on Venus, J. Geophys. Res., 1996, vol. 101, pp. 5397–5410.
Solomon, S.C., Smrekar, S.E., and Bindshadler, D., Venus tectonics: An overview of Magellan observations, J. Geophys. Res., 1992, vol. 97, pp. 13199–13256.
Squyres, S.W., Janes, D.M., Baer, G., Bindschandler, D.L., Shubert, G., Sharpton, V.L., and Stofan, E.R., The morphology and evolution of coronae on Venus, J. Geophys. Res., 1992, vol. 97, pp. 13.611–13.634.
Stefanick, M. and Jurdy, D.M., Venus coronae, craters, and chasmata, J. Geophys. Res., 1996, vol. 101, pp. 4637–4644.
Stofan, E.R., Sharpton, V.L., Schubert, G., Baer, G., Bindschadler, D.L., Janes, D.M., and Squyres, S.W., Global distribution and characteristics of coronae and related features on Venus: Implications for origin and relation to mantle processes, J. Geophys. Res., 1992, vol. 97, no. E8, pp. 13.347–13.378.
Stofan, E.R., Smrekar, S.E., Bindschadler, D.L., and Senske, D.A., Large topographic rises on Venus: Implications for mantle upwelling, J. Geophys. Res., 1995, vol. 100, pp. 23.317–23.327.
Stofan, E.R., Hamilton, V.E., Janes, D.M., and Smrekar, S.E., Coronae on Venus: Morphology and origin, in Venus II, Bougher, S.W., Hunten, D.M., and Phillips, R.J, Eds., Univ. Arizona Press, 1997, pp. 931–965.
Stofan, E.R., Smrekar, S.E., Tapper, S.W., Guest, J.E., and Grindrod, P.M., Preliminary analysis of an expanded corona database for Venus, Geophys. Res. Lett., 2001, vol. 28, pp. 4267–4270.
Stofan, E.R. and Smrekar, S.E., Large topographic rises, coronae, large flow field, and large volcanoes on Venus: Evidence for mantle plumes?, Geol. Soc. Am. Spec. Pap., 2005, vol. 388, pp. 841–861.
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The study was carried out under the State Assignment of the Vernadsky Institute of the Russian Academy of Sciences.
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Guseva, E.N., Ivanov, M.A. Spatial and Genetic Relations of Coronae, Lobate Plains, and Rift Zones of Venus. Sol Syst Res 57, 112–121 (2023). https://doi.org/10.1134/S003809462302003X
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DOI: https://doi.org/10.1134/S003809462302003X