Earth, Moon, and Planets

, Volume 50, Issue 1, pp 251–304 | Cite as

Tectonic Evolution of Eastern Ishtar Terra, Venus

  • R. W. Vorder Bruegge
  • J. W. Head
Part 3 Regional Geology

Abstract

The complex morphology and topography of Eastern Ishtar Terra have been interpreted as due to tectonic deformation. Models proposed to account for this deformation include: crustal flow through “asthenospheric flow and thermal-gravitational sliding”; rifting, gravity spreading, and fold belt formation; and horizontal convergence and crustal thickening. In this study we map the detailed structural and topographic fabric of this region in order to explore and test these hypotheses. Eastern Ishtar can be divided into four major provinces: Maxwell Montes/Western Fortuna Tessera, a high plateau and mountain belt dominated by long NNW trending ridges; Central Fortuna Tessera, a low region of orthogonally oriented short WNW trending ridges and long, NNE trending troughs; Eastern Fortuna Tessera, a broad, E-W trending topographic rise characterized by ENE trending troughs and a complex pattern of intersecting ridges; and Northern Fortuna Tessera, a region of steep, NE-facing topographic scarps and ridges that trend WNW. On the basis of structural and topographic relationships, the features within these provinces are found to be inconsistent with a formation through either downslope crustal flow or rifting. We find that the mapped features are most consistent with a formation through convergence, collison, and underthrusting of thickened crustal terranes. These terranes are suggested to have been created through processes of seafloor-type spreading and crustal collision. Based on relationships between the different terranes, several accretional events are proposed in which Eastern Ishtar is produced by the collision of crustal terranes beginning at Lakshmi Planum and extending to the east. This sequence is initiated with the formation of Maxwell Montes and Western Fortuna Tessera during east-west crustal convergence, underthrusting, and stacking. The next step involves the northeast to southwest convergence of a preexisting thick block of tessera in Central Fortuna, which produces shear deformation within Western Fortuna. This northeast to southwest convergence also produces Northern Fortuna Tessera through crustal imbrication, a process recognized along the entire northern boundary of Ishtar Terra. Finally, Laima Tessera converges with Fortuna from the southeast and collides with Eastern Fortuna Tessera producing shear within Eastern Fortuna and the linear convergence zones along the edges of Laima. High resolution images returned by the Magellan spacecraft will enable us to examine the features involved in the proposed production and suturing of crustal terranes.

Keywords

Crustal Thickening High Resolution Image Fold Belt Tectonic Deformation High Plateau 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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Copyright information

© Kluwer Academic Publishers 1990

Authors and Affiliations

  • R. W. Vorder Bruegge
    • 1
  • J. W. Head
    • 1
  1. 1.Department of Geological SciencesBrown UniversityProvidenceU.S.A.

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