The dispersal of pyroclasts from Apollinaris Patera, Mars: Implications for the origin of the Medusae Fossae Formation
نویسندگان
چکیده
The Medusae Fossae Formation (MFF) has long been thought to be of Amazonian age, but recent studies propose that a significant part of its emplacement occurred in the Hesperian and that many of the Amazonian ages represent modification (erosional and redepositional) ages. On the basis of the new formational age, we assess the hypothesis that explosive eruptions from Apollinaris Patera might have been the source of the Medusae Fossae Formation. In order to assess the likelihood of this hypothesis, we examine stratigraphic relationships between Apollinaris Patera and the MFF and analyze the relief of the MFF using topographic data. We predict the areal distribution of tephra erupted from Apollinaris Patera using a Mars Global Circulation Model (GCM) combined with a semi-analytical explosive eruption model for Mars, and compare this with the distribution of the MFF. We conclude that Apollinaris Patera could have been responsible for the emplacement of the Medusae Fossae Formation. 2011 Elsevier Inc. All rights reserved.
منابع مشابه
The dispersal of pyroclasts from ancient explosive volcanoes on Mars: Implications for the friable layered deposits
A number of voluminous, fine-grained, friable deposits have been mapped on Mars. The modes of origin for these deposits are debated. The feasibility for an origin by volcanic airfall for the friable deposits is tested using a global circulation model to simulate the dispersal of pyroclasts from candidate source volcanoes near each deposit. It is concluded that the Medusae Fossae Formation and E...
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The nature of strong martian crustal field sources is investigated by mapping and modeling of Mars Global Surveyor magnetometer data near Apollinaris Patera, a previously proposed volcanic source, supplemented by large-scale correlative studies. Regional mapping yields evidence for positive correlations of orbital anomalies with both Apollinaris Patera and Lucus Planum, a nearby probable extrus...
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Introduction: The Medusae Fossae Formation (MFF) is an enigmatic and discontinuous formation located in the southern parts of Elysium Planitia and Amazonis Planitia (130°-230°E and 12°S-12°N), covering an area of approximately 2.1 x 10 km and having an estimated volume of 1.4 x 10 km [1]. It is thought to have been deposited during the Amazonian period [2,3]. However, much of the cratering reco...
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0019-1035/$ see front matter 2009 Elsevier Inc. A doi:10.1016/j.icarus.2009.10.001 * Corresponding author. Address: Geological Scie Brook St., Box 1846, Providence, RI 02912, USA. Fax: E-mail address: [email protected] (L. Kerb The Medusae Fossae Formation (MFF), covering about 2.1 10 km (with an estimated volume of 1.4 10 km) and straddling the equatorial region of Mars east of Tharsis, h...
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0019-1035/$ see front matter 2012 Elsevier Inc. A http://dx.doi.org/10.1016/j.icarus.2012.11.037 ⇑ Corresponding author. Fax: +33 06 41 67 41 62. E-mail address: [email protected] (L. Kerber). A planetary global circulation model developed by the Laboratoire de Météorologie Dynamique (LMD) was used to simulate explosive eruptions of ancient martian volcanoes into paleo-atmospheres with high...
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