摘要
During the late Paleozoic to early Mesozoic,a tectonic transition occurred in Northeast China,marking a shift from the Paleo-Asian Ocean to the Mongolian Okhotsk and Paleo-Pacific tectonic domains[1].As a result of regional compression induced by oceanic closure and continental collision,stratigraphic records from this period are scarce,but such records are essential for elucidating the tectonic and paleographic evolution of the region during the transition.
基金
supported by the National Natural Science Foundation of China(42102129 and 41790453).
作者简介
Corresponding author:Yulong Huang,is an associate professor at College of Earth Sciences,Jilin University.He received his M.A.and Ph.D.degrees in marine geology and mineral resource prospecting&exploration,respectively,at Jilin University.His research interest includes reservoir geology,petroleum geology and volcanology.E-mail address:long@jlu.edu.cn;Zhuolong Yang,is a Ph.D.candidate of the College of Earth Sciences,Jilin University.His research interest includes the sedimentology,volcanologyand stratigraphy of the petroliferous basins in the Northeast of China.
