Graben–fissure systems in Guinevere Planitia and Beta Regio (264°–312°E, 24°–60°N), Venus, and implications for regional stratigraphy and mantle plumes-Reference-Cited by-同舟云学术

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Graben–fissure systems in Guinevere Planitia and Beta Regio (264°–312°E, 24°–60°N), Venus, and implications for regional stratigraphy and mantle plumes

Published:2003-08 Issue:2 Volume:164 Page:282-316
ISSN:0019-1035
Container-title:Icarus
language:en
Short-container-title:Icarus

Author:

Ernst R.E,Desnoyers D.W,Head J.W,Grosfils E.B

Publisher

Elsevier BV

Subject

Space and Planetary Science,Astronomy and Astrophysics

Reference63 articles.

1. Dyke-induced graben on Venus and Mars: analogues for Earth's rock record;Aspler,2003

2. Channels and valleys;Baker,1997

3. Small-scale fracture patterns on the volcanic plains of Venus;Banerdt;J. Geophys. Res.,1992

4. Stress and tectonics on Mars;Banerdt,1992

5. Plains tectonics on Venus;Banerdt,1997

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1. Dyke swarms of Onenhste and adjacent coronae in Parga Chasmata, SE of Atla Regio, Venus: Detailed mapping, swarm interactions and geological history;Icarus;2024-12

2. Graben systems and geological history of Mbokomu Mons region, Parga Chasmata, Venus;Icarus;2024-11

3. Heng-o Corona, Venus: Dyke swarms record evolution of its underlying mantle plume;Icarus;2024-07

4. Geological history of the Atira Mons large shield volcano, Beta Regio, Venus.;Planetary and Space Science;2024-05

5. Volcanic and Tectonic Constraints on the Evolution of Venus;Space Science Reviews;2024-04-29

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