Fractal Characteristics of Organic Nanopores in Naturally Deformed Shales from the Dabashan Thrust-Fold Belt, Northeast Sichuan Basin
Tectonic activity can induce deformation or failure of shale formations, thereby altering their macroscopic and microscopic structures to varying degrees. Naturally deformed shale samples from the Lower Cambrian Qiongzhusi Formation in the Dabashan Thrust-fold Belt, northeast Sichuan Basin, were investigated using scan...