1) Neodevonian
新泥盆世
2) late Devonian
晚泥盆世
1.
Further Study of Sphenophyllum Lungtanense, with a Discussion on the Evolution of the Late Devonian Sphenophyllales in South China;
龙潭楔叶的再研究——兼论华南晚泥盆世楔叶目的演化
2.
Late Devonian pillow basalts and bedded cherts in Changning-Menglian tectonic belt of southwestern Yunnan,China;
滇西南昌宁-孟连构造带晚泥盆世枕状玄武岩和层状硅质岩的特征
3.
Discovery of the Late Devonian and Late Permian radiolarian cherts in tectonic mélanges in the Cêdo Caka area, Shuanghu, northern Tibet, China;
藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩
3) Middle Devonian
中泥盆世
1.
Mineral chemistry and geological significance of clinopyroxenes from Middle Devonian picrite on the southern margin of the Altay Mountain;
阿尔泰山南缘中泥盆世苦橄岩中单斜辉石的成分特征及其地质意义
2.
Sequence Filling Dynamics Model of Passive Continental Margin Depressed Basin——A Case Study on the Early Devonian—Early Middle Devonian Youjiang Basin;
被动陆缘裂陷盆地的层序充填动力学模型——以早泥盆世——中泥盆世早期右江盆地为例
3.
Middle Devonian Picrites of South Margin of Altay Orogenic Belt and Implications for Tectonic Setting and Petrogenesis;
阿尔泰造山带南缘中泥盆世苦橄岩及其大地构造和岩石学意义
4) Early Devonian
早泥盆世
1.
Biogeographic Attribution of Early Devonian Coral in Xainza Area,Tibet;
西藏申扎地区早泥盆世珊瑚类生物地理分析
2.
The Evidence of Intrusive Rocks about Collision-orogenyduring Early Devonian in Eastern Kunlun Area;
东昆仑早泥盆世碰撞造山的侵入岩证据
3.
Sequence Filling Dynamics Model of Passive Continental Margin Depressed Basin——A Case Study on the Early Devonian—Early Middle Devonian Youjiang Basin;
被动陆缘裂陷盆地的层序充填动力学模型——以早泥盆世——中泥盆世早期右江盆地为例
5) the end of the Middle Devonian
中泥盆世末
1.
Distribution patterns of the end of the Middle Devonian tectonic unconformity and their constrain on the development and distribution of favorable stratigraphic traps in the Tarim Basin;
构造不整合的分布样式及其对地层圈闭的制约——以塔里木盆地中泥盆世末为例
6) Middle-Late Devonian
中晚泥盆世
1.
A Review of the Middle-Late Devonian Lycopsids;
中晚泥盆世石松植物研究综述
2.
The Middle-Late Devonian Liuling Group in Shanyang region,Shaanxi Province, located in between the Shang-Dan Fault and Shanyang Fault of the Qinling orogenic belt.
陕南山阳地区中晚泥盆世刘岭群位于秦岭造山带的商丹断裂带与山阳断裂之间。
补充资料：晚投江泽浦即事呈柳兵曹泥
【诗文】：
落日过重霞，轻烟上远沙。移舟冲荇蔓，转浦入芦花。
断岸迂来客，连波漾去槎。故乡何处在，更道向天涯。
【注释】：
【出处】：
全唐诗：卷268_36
落日过重霞，轻烟上远沙。移舟冲荇蔓，转浦入芦花。
断岸迂来客，连波漾去槎。故乡何处在，更道向天涯。
【注释】：
【出处】：
全唐诗：卷268_36
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条