the China-Association of Southeast Asian Nations(ASEAN)Maritime Cooperation Fund(grant No.12120100500017001);the China National Natural Science Foundation Project(grant No.41672120);the Shandong University of Science and Technology(SDUST)Research Fund(grant No.2015TDJH101)for their financial support。
The Late Cambrian(Furongian)Chaomidian Formation accumulated in an epeiric sea that covered a large part of the North China Plate and extended from China to Korea.The depositional environment of the formation is commo...
At present, there are no criteria to distinguish soft-sediment deformation structures (SSDS) formed by earthquakes from SSDS formed by the other 20 triggering mechanisms (see a companion paper in Vol 5, No. 4 of th...