“…In 1939, Griggs performed creep studies on rock and reported that rock deformation varied with time at a certain stress level (Griggs, 1939). Researchers have made great efforts to perform experiments to analyze features on different kinds of rock, such as granite (Lin et al, 2009;Chen et al, 2015;Xu et al, 2017), shale (Sone and Zoback, 2014), rock salt (Mansouri and Ajalloeian, 2018), sandstone (Brantut et al, 2014b;Chen et al, 2018), limestone (Brantut et al, 2014a;Nicolas et al, 2017), and coal (Ma et al, 2018;Zhang et al, 2019). Additionally, effects of loading history, including single-stage, multi-level loading (Zhao et al, 2017b;Yang et al, 2018), cycle loading and unloading (Chen et al, 2018) were investigated, and numerous researches focused on the temperatures (Xu et al, 2017), water (Liu and Shao, 2017;Yu C. et al, 2019), as well as initial porosity (Brantut et al, 2013).…”