Global drainage patterns and the origins of topographic relief on Earth, Mars, and Titan

被引:33
作者
Black, Benjamin A. [1 ,2 ]
Perron, J. Taylor [3 ]
Hemingway, Douglas [4 ]
Bailey, Elizabeth [5 ]
Nimmo, Francis [6 ]
Zebker, Howard [7 ]
机构
[1] CUNY, City Coll New York, Dept Earth & Atmospher Sci, New York, NY 10021 USA
[2] CUNY, Grad Ctr, Earth & Environm Sci, New York, NY 10017 USA
[3] MIT, Dept Earth Atmospher & Planetary Sci, 77 Massachusetts Ave, Cambridge, MA 02139 USA
[4] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA
[5] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[6] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USA
[7] Stanford Univ, Sch Earth Sci, Dept Geophys, Stanford, CA 94305 USA
关键词
CRATER; EVOLUTION; METHANE; MOON;
D O I
10.1126/science.aag0171
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Rivers have eroded the topography of Mars, Titan, and Earth, creating diverse landscapes. However, the dominant processes that generated topography on Titan (and to some extent on early Mars) are not well known. We analyzed drainage patterns on all three bodies and found that large drainages, which record interactions between deformation and erosional modification, conform much better to long-wavelength topography on Titan and Mars than on Earth. We use a numerical landscape evolution model to demonstrate that short-wavelength deformation causes drainage directions to diverge from long-wavelength topography, as observed on Earth. We attribute the observed differences to ancient long-wavelength topography on Mars, recent or ongoing generation of long-wavelength relief on Titan, and the creation of short-wavelength relief by plate tectonics on Earth.
引用
收藏
页码:727 / +
页数:5
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