A Fault on Mercury Revealed in 3-Dimensions

Autor: Susan J. Conway, David L. Pegg, David A. Rothery, Matthew R. Balme
Přispěvatelé: Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Jazyk: angličtina
Rok vydání: 2020
Předmět:
Zdroj: EPSC Abstracts
14th Europlanet Science Congress 2020
14th Europlanet Science Congress 2020, Oct 2020, held online, Unknown Region. ⟨10.5194/epsc2020-81⟩
DOI: 10.5194/epsc2020-81⟩
Popis: Mercury's tectonic history has been dominated by global contraction as the planet cools and shrinks. Previously, fault dips have been estimated by measuring offsets to the rims of craters displaced by fault movement. Here we present the first observations of a fault surface that has been exposed in three dimensions by a volcanic vent. Contractional tectonism is manifested through features such as lobate scarps, wrinkle ridges, and high relief ridges 1,2. The stresses in Mercury's crust that generated this contractional tectonism have multiple possible origins. These include global contraction 3, tidal despinning 4, true polar wander 5, and mantle convection 6. A combination of factors probably generates many faults, but the dominant driver of contractional tectonics on Mercury is the global contraction of the planet 7. This shrinking may be up to 10 km radially. The estimates of the actual amount of reduction in global radius recorded by Mercury’s crust is 7.1 km if the average fault dip is 25o but as little as 4.7 km if the average fault dip is 35o 11. An understanding of the dip of the faults on Mercury provides better input into these estimates and hence offers constraints on Mercury's thermal history. In the past, only indirect means were available to calculate dips of thrust faults, by using the shortening and vertical offset of craters that straddle faults 10,12. These studies derived an average dip of 25o. Until now, no-fault dip on Mercury has been measured by direct means. A crater located at 147.6oE, -65.6o N shows a small fault scarp that is visible on the side of a volcanic vent, and the trace is expressed also on the vent wall and floor. This is the first known fault surface on Mercury that is exposed in three dimensions. While a dip determination on a single fault is not conclusive, this result suggests that the shallower dip estimates are likely more representative estimates for average fault dips on Mercury and so adds weight to the higher end of the estimates of global contraction. Unfortunately, the resolution is insufficient for us to measure displacement by means of off-set features. BepiColombo will provide further opportunities to identify and measure similar features elsewhere on Mercury, and so help constrain the planet’s tectonic processes. References: Dzurisin, D. The tectonic and volcanic history of mercury as inferred from studies of scarps, ridges, troughs, and other lineaments. J. Geophys. Res. Solid Earth 83, 4883–4906 (1978). Watters, T. R. et al. The tectonics of Mercury: The view after MESSENGER’s first flyby. Earth Planet. Sci. Lett. 285, 283–296 (2009). Watters, T. R. & Nimmo, F. The Tectonics of Mercury. in Planetary Tectonics 15–80 (2010). Melosh, H. J. & Dzurisin, D. Mercurian global tectonics: A consequence of tidal despinning? Icarus 35, 227–236 (1978). Matsuyama, I. & Nimmo, F. Gravity and tectonic patterns of Mercury: Effect of tidal deformation, spin-orbit resonance, nonzero eccentricity, despinning, and reorientation. J. Geophys. Res. E Planets 114, 1–23 (2009). King, S. D. Pattern of lobate scarps on Mercury’s surface reproduced by a model of mantle convection. Nat. Geosci. 1, 229–232 (2008). Klimczak, C., Byrne, P. K. & Solomon, S. C. A rock-mechanical assessment of Mercury’s global tectonic fabric. Earth Planet. Sci. Lett. 416, 82–90 (2015). Solomon, S. C. The relationship between crustal tectonics and internal evolution in the moon and Mercury. Phys. Earth Planet. Inter. 15, 135–145 (1977). Grott, M., Breuer, D. & Laneuville, M. Thermo-chemical evolution and global contraction of mercury. Earth Planet. Sci. Lett. 307, 135–146 (2011). Galluzzi, V. et al. Faulted craters as indicators for thrust motions on Mercury. Geol. Soc. London, Spec. Publ. 401, 313–325 (2015). Byrne, P. K. et al. Mercury’s global contraction much greater than earlier estimates. Nat. Geosci. 7, 301–307 (2014). Galluzzi, V. et al. Structural analysis of the Victoria quadrangle fault systems on Mercury: timing, geometries, kinematics and relationship with the high‐Mg region. Journal of Geophysical Research: Planets (2019). doi:10.1029/2019je005953.
Databáze: OpenAIRE
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