山东灵山岛北背来石剖面下白垩统顺层砂脉的特征及其成因动力学分析*
钟建华1, 孙宁亮2, 郝兵2, 倪良田2, 宋冠先2, 薛纯琦2, 毛毳3, 邵珠福3, 葛毓柱4, 陈彬2, 刘圣鑫2, 彭超峰2, 谷东辉2, 王永强2, 李聪2

Characteristics and dynamics origin of the Lower Cretaceous sill in northern Beilaishi section of Lingshan Island, Shandong Province
Zhong Jian-Hua1, Sun Ning-Liang2, Hao Bing2, Ni Liang-Tian2, Song Guan-Xian2, Xue Chun-Qi2, Mao Cui3, Shao Zhu-Fu3, Ge Yu-Zhu4, Chen Bin2, Liu Sheng-Xin2, Peng Chao-Feng2, Gu Dong-Hui2, Wang Yong-Qiang2, Li Cong2
松原地震(2018年5月)液化砂和液化喷流 A—大型砂火山口和内部液化砂层,深0.2~1.0 m;B—液化砂喷出地表。注意喷流柱后面的大量喷出水汇集成“河”,均揭示了喷流含水极高。图片均引自网易新闻,网址为https://dy.163.com/article/DJDA9O6H0525TC5F.htm