https://notaspampeanas.com/tags/paxman-et-al./ Recent content in Paxman Et Al. on Notaspampeanas Hugo -- gohugo.io en © 2026 Notaspampeanas Tue, 14 Apr 2026 00:16:24 -0300 https://notaspampeanas.com/posts/1767106852355-antartida-oriental/ Tue, 14 Apr 2026 00:16:24 -0300 https://notaspampeanas.com/posts/1767106852355-antartida-oriental/ <p> <figure> <img class="my-0 rounded-md" loading="lazy" srcset=" /img/banner_Picadas_740x90_hu3124052656555182758.gif 330w, /img/banner_Picadas_740x90_hu4383330526392310737.gif 660w, /img/banner_Picadas_740x90_hu15808732043218573511.gif 1024w, /img/banner_Picadas_740x90_hu2758223483791455165.gif 2x" src="https://notaspampeanas.com/img/banner_Picadas_740x90_hu4383330526392310737.gif" alt="" /> </figure> </p> <div class="lead text-neutral-500 dark:text-neutral-400 !mb-9 text-xl"> Geophysical observations of the subglacial topography of Coats Land reveal a landscape formed by tectonics and fluvial erosion that influenced the formation of the East Antarctic Ice Sheet. </div> <p> <figure> <img class="my-0 rounded-md" loading="lazy" srcset=" /posts/1767106852355-antartida-oriental/featured_hu6789182397962094133.webp 330w, /posts/1767106852355-antartida-oriental/featured_hu16255979350240577448.webp 660w, /posts/1767106852355-antartida-oriental/featured_hu14573348084006732421.webp 1024w, /posts/1767106852355-antartida-oriental/featured_hu14867948172795218041.webp 2x" src="https://notaspampeanas.com/posts/1767106852355-antartida-oriental/featured_hu16255979350240577448.webp" alt="Magnetic anomaly map of the subglacial topography of Coats Land beneath the East Antarctic Ice Sheet, showing variations in the Earth’s magnetic field. The boundaries between high (red) and low (blue) values indicate steep geological surfaces, such as major fault systems. Credit: Paxman et al. [2026], Figure 1d. JGR: Earth Surface" /> </figure> <strong>Magnetic anomaly map of the subglacial topography of Coats Land beneath the East Antarctic Ice Sheet, showing variations in the Earth’s magnetic field. The boundaries between high (red) and low (blue) values indicate steep geological surfaces, such as major fault systems. Credit: <a href="https://doi.org/10.1029/2025JF008590" target="_blank">Paxman et al. [2026]</a>, Figure 1d. JGR: Earth Surface</strong></p>