id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
ajst-16291	Li, Wei; Li, Zhongquan	Study on the Formation Mechanism of The Strike-slip Fracture Zone in the Gulongnan Area of the Songliao Basin	2024	8	.pdf	application/pdf	3613	152	51	In the final stage of stretching, the stretching intensity becomes smaller, the activity of the faults decreases, some of the faults in the previous stage are activated and continue to develop upward, and at the same time, smaller faults of a more subordinate level are also newly formed, which constitutes the present pattern of the fracture zone. elongation stage Fault No. ②: close to the basement fault block, belongs to the companion fault of fault No. ①, and was initially formed during the stretching phase.	cache/ajst-16291.pdf	txt/ajst-16291.txt