The Jiangshan–Shaoxing fault zone(JSFZ)was formed by the amalgamation of the Yangtze and Cathaysia blocks in the Neoproterozoic.Since the Paleozoic,the JSFZ ha
The Yining Block is located in the southwestern part of the Central Asian Orogenic Belt(CAOB),which is characterized by widespread Carboniferous volcanic rocks.
Traditional surface exposure methods,such as trenching and exploratory shaft sinking,have their own limitations and do harm to the environment.Thus,shallow dril
Recently,through implementation of the National Nature Science Foundation of China(No.41303027)and Special Fund for Basic Scientific Research of Central College