Cleopatra Patera on Venus: Venera 15/16 evidence for a volcanic origin
The non-concentric nature, anomalous depth, and terraced morphology of the nested craters that compose Cleopatra Patera are more closely analogous to volcanic craters (calderas) than multi-ring impact structures. Associated deposits northeast and downslope of the Patera first recognized on Venera 15/16 radar images are interpreted as volcanic plains related to, and perhaps cogenetic with, Cleopatra. The plains lavas probably originated as effusions from a radial rift zone or ring fissures. Rim deposits surrounding Cleopatra are asymmetric along the structural fabric of the region, also indicating fissure-type eruptions. Finally, a volcanic origin not only is easily reconciled with the tectonic setting of the Patera, it is almost required by the correlation between the Patera and regional structural trend.
Citation Information
Publication Year | 1987 |
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Title | Cleopatra Patera on Venus: Venera 15/16 evidence for a volcanic origin |
DOI | 10.1029/GL014i001p00041 |
Authors | G. G. Schaber, R.C. Kozak, H. Masursky |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Geophysical Research Letters |
Index ID | 70014220 |
Record Source | USGS Publications Warehouse |