摘要
依据吉林省新生代沉积盆地的演化、岩石地层序列中区域性不整合接触关系的确认,结合区域火山岩的同位素年代学资料,初步确定喜山构造旋回经历了伊普尔期/路特期、普里亚本期/吕珀尔期、夏特期/阿基坦期、赛拉瓦勒期/托尔托纳期、墨西拿期/赞克尔期和皮亚琴察期/格拉斯期等6个构造运动幕,而后进入新构造运动发展期。其中普里亚本期/吕珀尔期幕为构造主幕,波及了整个中国东部,乃致改变了滨西太平洋大陆边缘的构造样式。
Based on the evolution of Cenozoic sedimentary basins and the confirmation of the regional uncon- formity contact relationship in lithostratigraphic sequences in Jilin Province, the authors confirm that the Himalayan (Xishan) structural cycle has experienced six movement episodes including Ypresian/Lutetian, Priabonian/Rupe- lian, Chattian/Aquitanian, Serravallian/Tortonian, Messinian/Zanclean and Piacenzian/Gelasian, subsequently, the Himalayan period gets into the developmental ore of neoteetonics. The Priabonian/Rupelian is the main episode of structural cycle, which effects the whole eastern China, even change the structural style of the continental margin of West Pacific Ocean region.
出处
《世界地质》
CAS
2015年第2期419-425,共7页
World Geology
关键词
喜山旋回
运动幕
吕珀尔期主幕
吉林省
Himalayan cycle
movement episode
Rupelian episode
Jilin Province