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李功宇
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( 副教授 )
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的个人主页 https://teachers.jlu.edu.cn/ligongyu/zh_CN/index.htm
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副教授
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性别 :
男
毕业院校 :
吉林大学
学历 :
博士研究生毕业
学位 :
博士
在职信息 :
在职
所在单位 :
地球科学学院
学科 :
构造地质学
办公地点 :
长春市建设街2199号吉林大学地球科学学院格子楼308-2a
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[1] Coupled Basin‐Mountain Data Record the Permian‐Triassic Tectonic Transition Along the Eastern Margin of Eurasia. JGR: Solid Earth
[2] The onset of Paleo-Pacific subduction: Key evidence from the Kaishantun Accretionary Complex, northeastern Eurasia. GSAB
[3] Substantiating the Paleozoic sedimentary record of the tectonic transition from a passive to an active continental margin along the eastern margin of Eurasia. GSAB
[4] The initiation of Paleo-Pacific subduction in Northeast Asia: Key evidence from the Yuejinshan accretionary complex. GSAB
[5] Supercontinent reconstruction of the microcontinents in Northeast China. GSAB
[6] Continental growth in eastern Central Asian Orogenic Belt: Evidence from Middle Permian–Middle Jurassic magmatism. Earth-Science Reviews
[7] Mesozoic intra-arc basin records the tectonic transition from the Paleo- Asian Ocean to the Paleo-Pacific Ocean in northeastern Eurasia. GSAB
[8] The Jiamusi Block: A hinge of the tectonic transition from the Paleo-Asian Ocean to the Paleo-Pacific Ocean regimes. Earth-Science Reviews
[9] The nature and spatial–temporal evolution of suture zones in Northeast China. Earth-Science Reviews
[10] 吉黑东部晚古生代构造体制转换:来自佳木斯兴凯地 块的双增生杂岩及岛弧岩浆岩带的制约. 岩石学报
[11] History of collision between the Jiamusi and Songliao blocks: new constraints from the Luobei complex, NE China. International Journal of Earth Sciences
[12] Late Paleozoic to Mesozoic tectonic transition in northeastern Eurasia: Constraints from two island arc magmatic belts in eastern NE China. GSAB
[13] Tectonic transition from the Paleo-Asian Ocean to the Paleo-Pacific Ocean in central Jilin (NE China): Constraints from the early Mesozoic high-Mg andesites. Gondwana Research
[14] Intraslab remobilization of nitrogen during early subduction facilitates deep nitrogen recycling: Insights from the blueschists in the Heilongjiang Complex in NE China. Chemical Geology
[15] 长春⁃延吉缝合带:性质与意义. 岩石学报
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