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Intrusion‐Induced Forced Folding Model for the Origin of Séítah Formation Domes on the Jezero Crater Floor, Mars.

Title: Intrusion‐Induced Forced Folding Model for the Origin of Séítah Formation Domes on the Jezero Crater Floor, Mars.
Authors: Barnes, Robert1 (AUTHOR) robert.barnes@imperial.ac.uk; Gupta, Sanjeev1 (AUTHOR) s.gupta@imperial.ac.uk; Treiman, Allan2 (AUTHOR); Sholes, Steven3 (AUTHOR); Paar, Gerhard4 (AUTHOR); Tate, Christian5 (AUTHOR); Bechtold, Andreas6,7 (AUTHOR); Stack‐Morgan, Katie3 (AUTHOR); Bell, James F.8 (AUTHOR); Maki, Justin3 (AUTHOR); Horgan, Briony9 (AUTHOR); Nuñez, Jorge10 (AUTHOR); Traxler, Chris11 (AUTHOR); Ortner, Thomas4,11 (AUTHOR); Shoemaker Thackston, Emileigh S.12,13,14 (AUTHOR); Hamran, Svein‐Erik15 (AUTHOR); Alwmark, Sanna16 (AUTHOR); Rice, Melissa17 (AUTHOR); Sun, Vivian3 (AUTHOR); Beyssac, Olivier18 (AUTHOR)
Source: Journal of Geophysical Research. Planets. Mar2026, Vol. 131 Issue 3, p1-40. 40p.
Subject Terms: Igneous intrusions; Structural geology; Geological formations; Martian geology; Mars rovers
Abstract: The JPL rover Perseverance's investigations of Jezero crater's floor reveal that the ultramafic Séítah formation and the overlying mafic Máaz formation are deformed into a broad, low‐amplitude structural dome. Mastcam‐Z stereo images processed into digital outcrop models, together with RIMFAX ground‐penetrating radar profiles, were used to reconstruct the three‐dimensional stratal geometry of both units along a SW–NE transect across a southern domain of the dome called south Séítah. Measurements from 3‐D reconstructions show a progression from sub‐horizontal layers in the central parts of the dome to dips
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