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<blockquote style="position: relative; padding-left: 55px;"><section><a href="https://bertha.social/users/leouieda/statuses/113685701002884491">Leonardo Uieda (leouieda@bertha.social)'s status on Saturday, 21-Dec-2024 06:06:34 JST</a><a href="https://bertha.social/@leouieda" title="leouieda@bertha.social"><img src="https://gnusocial.jp/avatar/265310-48-20240614115753.webp" width="48" height="48" alt="Leonardo Uieda" style="position: absolute; left: 0; top: 0;">Leonardo Uieda</a></section><article><p>We have a new preprint out on EarthArXiv which introduces Euler inversion, a new method for finding the location and approximate geometry of sources of gravity and magnetic anomalies.</p><p>Big thank you to my co-authors Gelson F. Souza-Junior, India Uppal, and Vanderlei C. Oliveira Jr.!</p><p>Read more about it: <a href="https://www.compgeolab.org/news/euler-inversion-preprint.html" rel="nofollow noreferrer">https://www.compgeolab.org/news/euler-inversion-preprint.html</a></p><p><a href="https://bertha.social/tags/Geophysics" rel="tag">#Geophysics</a> <a href="https://bertha.social/tags/EarthSciences" rel="tag">#EarthSciences</a> <a href="https://bertha.social/tags/Gravity" rel="tag">#Gravity</a> <a href="https://bertha.social/tags/Magnetics" rel="tag">#Magnetics</a> <a href="https://bertha.social/tags/InverseProblems" rel="tag">#InverseProblems</a></p></article><footer><a rel="bookmark" href="https://gnusocial.jp/conversation/4226423#notice-8259776">In conversation</a><time datetime="2024-12-21T06:06:34+09:00" title="Saturday, 21-Dec-2024 06:06:34 JST">about 4 months ago</time> <span>from <span><a href="https://bertha.social/@leouieda/113685701002884491" rel="external" title="Sent from bertha.social via ActivityPub">bertha.social</a></span></span><a href="https://bertha.social/@leouieda/113685701002884491">permalink</a><h4>Attachments</h4><ol><li><label><a rel="external" href="https://gnusocial.jp/attachment/3742123">Left panel: Euler inversion is a new method for finding depths from gravity and magnetic data. It's much more robust to noise and interfering sources than Euler deconvolution and can estimate the structural index.Right panel: Map with red-white-blue colored dots representing the magnetic anomaly. There are several dipolar looking anomalies and some linear anomalies in the NE-SW direction. Overlaid are small triangles, circles, and squares which follow the dipolar and linear anomalies.</a></label><br><a href="https://bertha.social/system/media_attachments/files/113/685/698/591/871/496/original/2c1500eb6de251fb.jpg" rel="external">https://bertha.social/system/media_attachments/files/113/685/698/591/871/496/original/2c1500eb6de251fb.jpg</a></li><li><article><header><div>Domain not in remote thumbnail source whitelist: www.compgeolab.org</div><h5><a href="https://www.compgeolab.org/news/euler-inversion-preprint.html#Geophysics">A better method for locating sources of gravity and magnetic anomalies | Computer-Oriented Geoscience Lab</a></h5><div></div></header><div>We have a new preprint out on EarthArXiv which introduces Euler inversion, a new method for finding the location and approximate geometry of sources of gravity and magnetic anomalies. We’re very...</div><footer></footer></article></li></ol></footer></blockquote>

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Leonardo Uieda (leouieda@bertha.social)'s status on Saturday, 21-Dec-2024 06:06:34 JST Leonardo Uieda
We have a new preprint out on EarthArXiv which introduces Euler inversion, a new method for finding the location and approximate geometry of sources of gravity and magnetic anomalies.
Big thank you to my co-authors Gelson F. Souza-Junior, India Uppal, and Vanderlei C. Oliveira Jr.!
Read more about it: https://www.compgeolab.org/news/euler-inversion-preprint.html
#Geophysics #EarthSciences #Gravity #Magnetics #InverseProblems
In conversationabout 4 months ago from bertha.socialpermalink
Attachments
1. Left panel: Euler inversion is a new method for finding depths from gravity and magnetic data. It's much more robust to noise and interfering sources than Euler deconvolution and can estimate the structural index. Right panel: Map with red-white-blue colored dots representing the magnetic anomaly. There are several dipolar looking anomalies and some linear anomalies in the NE-SW direction. Overlaid are small triangles, circles, and squares which follow the dipolar and linear anomalies.
  https://bertha.social/system/media_attachments/files/113/685/698/591/871/496/original/2c1500eb6de251fb.jpg
2. Domain not in remote thumbnail source whitelist: www.compgeolab.org
  A better method for locating sources of gravity and magnetic anomalies | Computer-Oriented Geoscience Lab
  We have a new preprint out on EarthArXiv which introduces Euler inversion, a new method for finding the location and approximate geometry of sources of gravity and magnetic anomalies. We’re very...

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