On the oriented specimens of three types tectonite, collected from near the fault on Pi-Shi-Kou of Mt. Laoshan, the microstructure of rocks and the orientation patterns of quartz are here studied. According to the features of the microstructure and the orientation patterns of quartz, the pair of small-circle girdle type, parallel to the ac plan, and in connection with the field observation data it is suggested that the fault might be of compression-torsion fault in predominance of compression.
. 1975, 山东崂山劈石口断裂的岩组学初步研究. 地质科学, 10(1): 65-71.
. PRELIMINARY PETROFABRIC ANALYSIS OF THE PI-SHI-KOU FAULT OF MT. LAOSHAN, SHANTUNG PROVINCE[J]. Chinese Journal of Geology, 1975, 10(1): 65-71.