论著获奖 |
第一/通讯作者期刊论文: [1]李加好,宋传中,任升莲,涂文传,张欢张浩然. 2010.秦岭商丹断裂带的构造样式和变形分析.地学前缘, 7(4): 197-205 [2]李加好,宋传中,任升莲,王中,涂文传,张欢,张浩然. 2011.秦岭商丹构造带商南段岩石变形与变质条件探讨.地质论评, 57(5): 641-649 [3]李加好,宋传中, Shoufa Lin,任升莲,王道轩,涂文传,张欢. 2013.秦岭商丹断裂带南侧弧前沉积体的变形特征及其构造意义.地质科学, 48(3): 626-637 [4]李加好,任升莲,张妍,王薇,涂文传,张欢. 2014.北秦岭二郎坪岩群两侧韧性剪切带的构造变形及其意义.地质科学, 49(2): 513-528 [5]李加好,宋传中,任升莲,张妍,杨帆,王微,汪佩佩. 2015.蚌埠隆起区煌斑岩锆石U-Pb测年及其地质意义.地质科学, 50(3): 773-784 [6]杨挺宇,李加好*,任升莲,兰瑞煊,陈守文. 2019.北秦岭商南岩体的构造变形、地球化学特征及其地质意义,地质科学, 54(1): 1000-1015 [7]兰瑞烜,李加好*,杨挺宇. 2020.秦岭岩群早古生代晚期构造热事件及地质意义.威尼斯432888cam学报(自然科学版), 43(11):1550-1555. [8]Li JH, Lan RX, Ren SL, Song CZ, Li LM. 2020. Subduction and collision processes between the North China and South China blocks constrained by the geochronology and geochemistry of the Wuguan Complex in the Qinling orogen, China. International Geology Review, 62(12): 1538-1554. [9]杨挺宇,李加好*,任升莲,陈守文,谭静,宋传中. 2021.秦岭岩群古生代构造变形分析.地质科学, 56(1): 136-157 [10]李加好,邓聚,王晴,杨挺宇,任升莲,宋传中,谭静,陈守文. 2021.龟山杂岩的形成时代、构造属性及变质条件:对秦岭-桐柏造山带构造演化的指示.地质学报, 95(8): 2396-2410 [11]谭静,李加好*,陈守文,袁峰,宋传中,任升莲,张妍,蒋仁. 2022.郯庐断裂带肥东段第四纪活动特征及最新活动时代.地质科学, 57(2): 356-374 [12] Chen SW,Li JH*, Yuan F, Deng YF, Zhang DY, Li XH, Jiang R. 2022. Deformation history of the Feidong Segment of the Tan-Lu Fault zone in the Early Cretaceous: Implications for the tectonic evolution in eastern China. Geological Journal, 57(9): 3668-3685 [13] Guan M,Li JH*, Jia GQ, Ren SL, Song CZ. 2022. U–Pb Zircon Ages and Geochemistry of the Wuguan Complex and Liuling Group: Implications for the Late Paleozoic Tectonic Evolution of the Qinling Orogenic Belt, Central China. Minerals, 12(8), 1026 [14] Chen SW,Li JH*, Yuan F, Li LM, Deng YF, Simon M. Jowitt SM, Jiang R, Li ZW, Yuan F, Li Y, Tan J. 2022. Geochemistry and geochronology of I–type granites of the Feidong Complex, eastern China: implications for the Paleoproterozoic tectonic evolution of the Yangtze Craton. Precambrian Research 382, 106884. [15]Chen SW,Li JH*, Yuan F, Jowitt SM, Li LM, Deng YF, Liu H, Jiang Ren. 2023. Modern–stylesubduction during the late Neoarchean to early Paleoproterozoic? Geochemical evidence from ca. 2.45 Gaarc–type magmatism in the Feidong Complex, northeastern Yangtze Craton, South China.Precambrian Research 388,106999. 奖励荣誉: 2019/10第二届全国大学青年教师地质课程教学比赛三等奖 2020/01安徽省教学成果二等奖奖(R4) 2021/07威尼斯432888cam优秀共产党员 2022/04安徽省教学成果二等奖奖(R3) 2022/10安徽省教学成果奖三等奖(R3) |