Structural evolution of western Fortuna Tessera, Venus

M. E. Pritchard, V. L. Hansen, J. J. Willis

Research output: Contribution to journalArticlepeer-review

11 Scopus citations


Western Fortuna Tessera, Ishtar Terra, records polyphase deformation. Structures include: ribbons forming long, narrow, steep-sided troughs that reflect surface layer extension; N-trending folds related to Maxwell Montes deformation; short, wide, NW-trending graben that reflect late local extension; and, within the southwestern map area, gentle, E-trending warps, which postdate ribbon structures. Flood lava flows postdate deformation. Ribbon structures change orientation radially from NNE to WNW. These observations caution against the correlation of Fortuna Tessera with tessera elsewhere on Venus and against the proposal that tessera forms a global stratigraphic layer.

Original languageEnglish (US)
Pages (from-to)2339-2342
Number of pages4
JournalGeophysical Research Letters
Issue number18
StatePublished - 1997

Fingerprint Dive into the research topics of 'Structural evolution of western Fortuna Tessera, Venus'. Together they form a unique fingerprint.

Cite this