Infrared Temperature Law and Deformation Monitoring of Layered Bedding Rock Slope under Static Load

<table class="table-group" id="tab1"><tr><td><table class="table"><tr><td class="thead-hr" colspan="5"><hr/></td></tr><tr class="thead"><td class="align_left">Rock section</td><td class="align_center">Rock section name</td><td class="align_center">Lithological composition</td><td class="align_center">Thickness (m)</td><td class="align_center">Distribution characteristics</td></tr><tr><td class="thead-hr" colspan="5"><hr/></td></tr><tr><td class="align_left">Second</td><td class="align_center">Schist section</td><td class="align_center">Composition of amphibolite schist, mica feldspar quartz schist and mica quartz schist</td><td class="align_center">500</td><td class="align_center">East of the mining area, from Heibeigou to Tieshan</td></tr><tr><td class="align_left">Third</td><td class="align_center">Iron-bearing rock section</td><td class="align_center">Green curtain angle flash (slice) rock and magnet quartzite, quartz green mud schist, iron ore layer and black cloud green mud schist</td><td class="align_center">350</td><td class="align_center">Chaxingou to Huangbai gully, integrated on the schist</td></tr><tr><td class="align_left">Fourth</td><td class="align_center">Mica quartz schist section</td><td class="align_center">Integrated on the third layer of iron</td><td class="align_center">40–100</td><td class="align_center">South of Miaoergou–Huangbaiyu</td></tr><tr class="table-tr"><td colspan="5"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

<div>Characteristics of typical rock sections of the Dagugou Formation.</div>

Advances in Civil Engineering

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Table 1: Infrared Temperature Law and Deformation Monitoring of Layered Bedding Rock Slope under Static Load 