Paleogene alternating carbonatic and clastic sedimentary structures as the substratum for younger, less consolidated sediments. This type of structural setting causes the development of large-scale, gravity-driven DSGSD and slow mass movement. Surface deformations with clear scarps and multiple crest lines triggered planes for large-scale deep mass creeps, and these were related directly to active faults and folds in the geologic structures. Our study offers a new combination 

Please visit our website: https://support.openlms.net/hc/en-us/community/posts/16168709121308-%F0%9D%97%96-%F0%9D%97%9F%F0%9D%97%9F-%F0%9D%97%96%C3%B3%F0%9D%97%BA%F0%9D%97%BC-%F0%9D%97%B5%F0%9D%97%AE%F0%9D%97%B4%F0%9D%97%BC-%F0%9D%98%82%F0%9D%97%BB%F0%9D%97%AE-%F0%9D%97%BD%F0%9D%9

Keywords: https://support.openlms.net/hc/en-us/community/posts/16168709121308-%F0%9D%97%96-%F0%9D%97%9F%F0%9D%97%9F-%F0%9D%97%96%C3%B3%F0%9D%97%BA%F0%9D%97%BC-%F0%9D%97%B5%F0%9D%97%AE%F0%9D%97%B4%F0%9D%97%BC-%F0%9D%98%82%F0%9D%97%BB%F0%9D%97%AE-%F0%9D%97%BD%F0%9D%9