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1)  Jiaoliao Luxi and Xuhuai area
胶辽鲁西徐淮地区
1.
According to study on rock property combination, palaeobio characteristics and sesmic event strata, Neoproterozoic strata in Jiaoliao Luxi and Xuhuai area can be multi-divided and contrasted as follows: Heishanguan formation and Erqingshan formation in Luxi area are conformity with Diaoyutai formation and Nanfen formation, while Baoshankou fomation can contrast with Nanfen formation.
依据岩性组合、古生物特征及地震事件层研究 ,对胶辽鲁西徐淮地区新元古代地层可作如下多重划分对比 :鲁西黑山官组、二青山组分别与辽东的钓鱼台组、南芬组相当 ,胶东豹山口组可与南芬组对比 ,它们同属青白口系。
2)  Jiao-Liao-Xu-Huai
胶辽徐淮
1.
The application of Sr and C isotope evolution to the dating of Neoproterozoic strata:a case study of the Jiao-Liao-Xu-Huai area in northern China;
锶、碳同位素演化在新元古代地层定年中的应用——以胶辽徐淮地层分区为例
3)  Xu-Huai region
徐淮地区
1.
Petrology and geochemistry of xenoliths of amphibolite and gneiss from Mesozoic intrusive complex in Xu-Huai region,China:constraint on components of the deep crust;
徐淮地区中生代侵入杂岩中角闪岩和片麻岩类捕虏体的岩石学和地球化学:对深部地壳物质组成的制约
4)  Jiaodong and Luxi areas
胶东和鲁西地区
1.
Jiaodong and Luxi areas are separated by Yishu fault.
胶东和鲁西地区被沂沭断裂带所分隔 ,在中侏罗世末期 ,由于郯庐断裂带发生大规模左旋平移运动 ,二个地区最终拼合在一起。
5)  West Liaoning
辽西地区
1.
The Environment Disaster Events and the Evolution of Man-land Relation in the West Liaoning During 5 000 a BP;
5000 a BP以来辽西地区环境灾害事件与人地关系演变
2.
Finite element modeling of the Mesozoic lithosphere structure and evolution of West Liaoning, Northeast China;
辽西地区中生代岩石圈结构与演化的有限元模拟
6)  western Liaoning
辽西地区
1.
Improvement of Pure Pinus tabulaeformis Forests and Its Control Effect on Caterpillars in Western Liaoning;
辽西地区油松纯林改造及对松毛虫的控制
2.
Analysis of soil anti-erodibility in western Liaoning;
辽西地区林地土壤抗蚀性分析
3.
The major types of soil conservancy plantations in western Liaoning and structural features;
辽西地区水土保持林主要林分类型及结构特征分析
补充资料:观校猎,上淮西相公
【诗文】:
龙骧校猎邵陵东,野火初烧楚泽空。师事黄公千战后,
身骑白马万人中。笳随晚吹吟边草,箭没寒云落塞鸿。
三十拥旄谁不羡,周郎少小立奇功。



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【出处】:
全唐诗:卷151_19
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