Magnetic Study of the Heated and Unheated Sedimentary Fillings of Sebkha Mhabeul, Southeast Tunisia: A Geophysical Method for Paleoclimatic Investigation and Tephrochronological Dating

<table class="table-group" id="tab1"><tr><td><table class="table"><tr><td class="thead-hr" colspan="4"><hr/></td></tr><tr class="thead"><td align="left"> </td><td align="center">
                  25°C</td><td align="center">250°C</td><td align="center">700°C</td></tr><tr><td class="thead-hr" colspan="4"><hr/></td></tr><tr><td align="left">Mean</td><td align="center">46.0064342</td><td align="center">47.5064684</td><td align="center">200.516467</td></tr><tr><td align="left">Minimum</td><td align="center">21.9594</td><td align="center">22.4225</td><td align="center">53.12956</td></tr><tr><td align="left">Maximum</td><td align="center">90.4496</td><td align="center">94.3186</td><td align="center">434.4831</td></tr><tr><td align="left">Standard deviation</td><td align="center">16.7722996</td><td align="center">17.7733736</td><td align="center">82.5223499</td></tr><tr class="table-tr"><td colspan="4"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Mean, minimum, maximum, and standard deviation values after heating at different temperatures.

International Journal of Geophysics

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Table 1

Table 1: Magnetic Study of the Heated and Unheated Sedimentary Fillings of Sebkha Mhabeul, Southeast Tunisia: A Geophysical Method for Paleoclimatic Investigation and Tephrochronological Dating 

Table 1 | Magnetic Study of the Heated and Unheated Sedimentary Fillings of Sebkha Mhabeul, Southeast Tunisia: A Geophysical Method for Paleoclimatic Investigation and Tephrochronological Dating 