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- W2024661801 abstract "Wrinkle ridges are nearly ubiquitous landforms on the plains of Venus. By analogy with similar structures on other planets, venusian wrinkle ridges are inferred to trend normal to the direction of maximum principal compression in the crust, an inference that is verified by geometrical relationships with positive and negative relief features on Venus. Because plains are the dominant terrain on Venus, wrinkle ridges provide an excellent opportunity to determine the orientations of shallow crustal principal stress trajectories over most of the planet. In most places there are two or more sets of wrinkle ridges, and commonly one of these persists over a very large area, defining a regional stress domain. Intersection relationships indicate that these domains differ in age." @default.
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- W2024661801 date "1993-11-05" @default.
- W2024661801 modified "2023-10-13" @default.
- W2024661801 title "Wrinkle ridges, stress domains, and kinematics of Venusian plains" @default.
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- W2024661801 doi "https://doi.org/10.1029/93gl02635" @default.
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