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Venus tesserae feature layered, folded, and eroded rocks
Geology ( IF 4.8 ) Pub Date : 2020-09-04 , DOI: 10.1130/g47940.1
Paul K. Byrne 1 , Richard C. Ghail 2 , Martha S. Gilmore 3 , A.M. Celâl Şengör 4 , Christian Klimczak 5 , David A. Senske 6 , Jennifer L. Whitten 7 , Sara Khawja 8 , Richard E. Ernst 8, 9 , Sean C. Solomon 10
Affiliation  

1707. [12] Banks B. K. and Hansen V. L. (2000) JGR, 105, 17,655–17,667. [13] Ghent R. and Hansen V. L. (2005) Icarus, 139, 116–136. [14] Cofrade G. et al. (2019) Planet. Space Sci., 178, 104706. [15] Ford P. G. and Pettengill G. H. (1992) JGR, 97, 13,103–13,114. [16] Herrick R. R. et al. (2012) Eos, 93, 125–126. [17] Molinaro M. et al. (2005) Tectonics, 24, TC3007. [18] Li J. et al. (2016) JGR, 121, 3048–3080. [19] Ramsey J. G. (1967) Folding and Fracturing of Rocks. McGraw-Hill, New York. [20] Hansen V. L. and Willis J. J. (1996) Icarus, 123, 296–312. [21] Greeley R. et al. (1984) Icarus, 57, 112–124. [22] Craddock R. A. (2011) Prog. Phys. Geog., 36, 110–124. [23] Selivanov A. S. et al. (1982) Sov. Astron. Lett., 8, 235–236. [24] Carvalho F. P. et al. (2011) ICE J. Mar. Sci., 68, 427–435. [25] McKinnon W. B. et al. (1997) in Venus II (Bougher S. W. et al., eds.), Univ. Ariz. Press, pp. 969–1014. [26] Hansen V. L. et al. (1999) Geology, 27, 1071–1074. [27] Basilevsky A. T. et al. (1985) GSA Bull., 96, 137–144. [28] Ingersoll A. P. (1969) J. Atmos. Sci., 26, 1191–1198. Figure 2: (a) A set of lenticular landforms along the northern margin of Ovda Regio that we interpret as periclinal folds. The image is in orthographic projection, centered at 0.5°N, 80.5°E; Radar look direction is from the left. (b) Periclines in southeast Sichuan basin, China (arrows mark two examples). Image is in orthographic projection, centered at 30°N, 107°E. 2514.pdf 51st Lunar and Planetary Science Conference (2020)
更新日期:2020-09-04
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