GIANT DIKE SWARMS: EARTH, VENUS, AND MARS

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dc.contributor.author Ernst R.E.
dc.contributor.author Grosfils E.B.
dc.contributor.author Mège D.
dc.date.accessioned 2021-04-05T12:39:59Z
dc.date.available 2021-04-05T12:39:59Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=14214945
dc.identifier.citation Annual Review of Earth and Planetary Sciences, 2001, 29, С. 4, 489-534
dc.identifier.issn 0084-6597
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27471
dc.description.abstract 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.
dc.subject mantle plume
dc.subject rift
dc.subject plate tectonics
dc.subject graben
dc.subject dike
dc.title GIANT DIKE SWARMS: EARTH, VENUS, AND MARS
dc.type Статья


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