大连金石滩国家地质公园地层特征

大连金石滩海岸带地层剖面由凉水湾始,经大林子海岸至葛屯金石滩港止,沿途可见新元古代震旦纪营城子组、十三里台组、马家屯组、崔家屯组、兴民村组和早古生代寒武纪葛屯组、大林子组、碱厂组及馒头组.其中,葛屯组和大林子组为二组层型剖面的命名地.除碱厂组和馒头组以外,其他各组命名地均来自大连地层小区,为大连地区独有.在考察珍贵地层剖面的同时,还可欣赏玫瑰园景群、恐龙园景群、南秀园景群和鳌滩园景群等丰富的地质地貌遗迹.

The stratigraphic characteristics of Jinshitan national geological park in Dalian

The stratigraphic profile of Jinshitan stretches from Liangshui bay, through Dalinzi coast to Jinshitan port of Getun. Go along the Jinshitan profile, we can see Yingchengzi Formation, Shisanlitai Formation, Majiatun Formation, Cuijiatun Formation and Xingmincun Formation which formed in Neoproterozoic Sinian period; and we can see Getun Formation, Dalinzi Formation, Jianchang Formation and Mantou Formation which formed in Early Paleozoic Cambrian period. The Getun Formation and Dalinzi Formation are named after stratotype profile. The others are named after local sub-areas of Dalian area except Jianchang Formation and Mantou Formation. During geological survey of the stratigraphic profile, we can enjoy the geological and geomorphological landscape of ‘Rose garden’, ‘Dinosaur garden’, ‘Nanxiu garden’ and ‘Turtle garden’.