Kollision der kontinentalen Anteile zweier tektonischer Platten: Entstehung eines jungen Faltengebirges (z.B. Alpen, Himalaya)
<p>Original .gif: USGS <br>
Original SVG version: <a href="//commons.wikimedia.org/wiki/User:Nefronus" title="User:Nefronus">Nefronus</a> <br></p>
Modified and translated (using Inkscape 0.92 and text editor): <a href="//commons.wikimedia.org/wiki/User:Gretarsson" title="User:Gretarsson">Gretarsson</a>
<p><a href="//commons.wikimedia.org/wiki/File:Continental-continental_convergence_Fig21contcont.gif" title="File:Continental-continental convergence Fig21contcont.gif">Continental-continental convergence Fig21contcont.gif</a>, modified according to
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<ul><li><a rel="nofollow" class="external text" href="https://www.researchgate.net/figure/MECHANISM-OF-A-SUBDUCTION-ZONE-A-AND-CONTINENTAL-COLLISION-B-MARSHAK-2001_fig11_318599581">Fig. 11</a> in: C.J.S. Fourie, D. Johnson (2017): <i>Analysis of the Geothermal Structures of Aliwal North, South Africa</i> (Conference Paper). Power-Gen Africa 2017, Johannesburg, 18–20 July (<a rel="nofollow" class="external text" href="https://www.researchgate.net/publication/318599581">ResearchGate</a>)</li>
<li>Various figs. in: Yaoling Niu: <i>Slab breakoff: a causal mechanism or pure convenience?</i> Science Bulletin 62(7):456–461, <a href="//doi.org/10.1016/j.scib.2017.03.015" class="extiw" title="doi:10.1016/j.scib.2017.03.015">doi:10.1016/j.scib.2017.03.015</a> (Open Access)</li></ul>