Electrical Resistivity Structures of the Beishan Block, NW China, and Tectonic Implications
作者机构:Center for Geophysical SurveyChina Geological Survey Technology Innovation Center for Earth Near Surface DetectionChina Geological Survey
出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))
年 卷 期:2024年第S1期
页 面:90-93页
核心收录:
学科分类:070904[理学-构造地质学] 081801[工学-矿产普查与勘探] 081802[工学-地球探测与信息技术] 0709[理学-地质学] 07[理学] 08[工学] 0818[工学-地质资源与地质工程]
摘 要:The Central Asian Orogenic Belt(CAOB) is a giant orogenic belt located between the Siberian Plate, the Tarim Plate, and the North China Plate, which records the longterm and complex geologic evolution of the Paleo-Asian Ocean from the Early Neoproterozoic(ca. 1000 Ma) to the Late Paleoproterozoic(ca. 250 Ma) process. The Beishan Block is located in the middle and southern edge of the Central Asian orogenic belt, at the intersection of the Tarim plate, the Siberian Plate and the Kazakhstan Plate.