Giant dike swarms:: Earth, Venus, and Mars

被引:217
|
作者
Ernst, RE
Grosfils, EB
Mège, D
机构
[1] Geol Survey Canada, Ottawa, ON K1A 0E8, Canada
[2] Pomona Coll, Dept Geol, Claremont, CA 91711 USA
[3] Univ Paris 06, ESA CNRS 7072, Lab Techon, F-75252 Paris 05, France
关键词
mantle plume; rift; plate tectonics; graben; dike;
D O I
10.1146/annurev.earth.29.1.489
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Earth, Venus, and Mars all exhibit populations of giant (radiating, linear, and arcuate) mafic dike swarms hundreds to > 2000 km in length. On Earth the dikes are exposed by erosion, while on Venus and Mars their presence is mainly inferred from associated volcanic morphology and surface deformation. The apparent absence of plate tectonics in the geologic record of Venus and Mars means that the observed population of swarms remains geometrically intact, while on Earth plate tectonics has fragmented swarms. About 30 giant radiating swarms have so far been identified on Earth, but with further study the number is expected to rise and may eventually coincide with the hundreds of mantle plume head events now being proposed. On Venus, at least 118 radiating swarms are distributed across the planet, and new high resolution mapping is revealing additional swarms. On Mars, up to 16 giant dike swarms are observed, most associated with the Tharsis region.
引用
收藏
页码:489 / 534
页数:46
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