The Early Breakup of Rodinia Supercontinent in the Northeastern Margin of the Yangtze Plate:New Evid

• 作 者: LIAO Jing YUE Baojing DING Xue ZHANG He Y\N Xuebo
• 机 构: Qingdao Institute of Marine Geology,School of Earth and Space Sciences,University of Science and Tec
• 出 处: Acta Geologica Sinica(English Edition)
• 发表日期: 2017年04期
• 关键词: Yangtze Shandong SIMS ocean northeastern margin orogenic magmatic Island deplete

Objective The amalgamation and breakup mechanisms of the Rodinia supercontinent during the Meso-and Neoproterozoic have been the focus of much research.However,few studies have examined the response of Neoproterozoic tectonics and magmatism along the northeastern margin of the Yangtze Plate to synchronous global events.The Qianliyan Uplift is located on the eastern margin of the Sulu orogenic belt in the ocean,but

Objective The amalgamation and breakup mechanisms of the Rodinia supercontinent during the Meso-and Neoproterozoic have been the focus of much research. Despite, few studies have examined the response of Neoproterozoic tectonics and magmatism along the northeastern margin of the Yangtze Plate to synchronous global events. The Qianliyan Uplift is located on the eastern margin of the Sulu orogenic belt in the ocean, but