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1)  Yangtze Region
扬子区
1.
The discovery of the Early Cambrian phosphatized small shell fossils (SSFs) in the Yangtze Region is of importance to the studies on the early evolution of animals and the division and correlation of the Sinian-Cambrian boundary strata.
扬子区早寒武世早期的磷酸盐化小壳化石的发现,为早期动物演化及震旦系-寒武系界线地层的划分与对比研究做出了重要贡献。
2.
The Ordovician lithofacies and biofacies change greatly at different localities of the Yangtze Region, South China.
华南扬子区不同地点奥陶纪的岩相、生物相变化显著。
3.
The Middle Ordovician Llandovery rugose corals are abundant in the Yangtze region, especially in the Early Silurian.
扬子区中奥陶世—志留纪兰多维利世四射珊瑚产出丰富 ,尤以兰多维利世最为繁盛。
2)  Lower Yangtze Area
下扬子区
1.
Sequence stratigraphic division of the Sinian-Middle Triassic marine strata in the Lower Yangtze area of the Jiangsu-Anhui zone;
苏皖下扬子区震旦纪—中三叠世海相层序地层
2.
Discussion on tectonopalaeogeography of Lower Yangtze Area during the Caledonian Period;
扬子区加里东期构造古地理问题
3.
Thermo-tectonic history of the Lower Yangtze area since Late Cretaceous:evidence from apatite fission track analysis of sandstones from Pukou Formation
苏皖下扬子区晚白垩世以来的构造—热历史:浦口组砂岩磷灰石裂变径迹证据
3)  Yangtze area
扬子地区
1.
Lithofacies paleogeography and petroleum geology of the Silurian in Yangtze area;
扬子地区志留纪岩相古地理与石油地质条件研究
2.
Biogenetic barium distribution from the Upper Ordovician to Lower Silurian in the Yangtze area and its significance to paleoproductivity
扬子地区上奥陶—下志留统生物钡特征及其古生产力意义
3.
Through a long-term compaction and geological history, the orlginal porosity and permeability of the marine reservoir rocks in the Lower Yangtze area are greatly decreased, most of them are characterized by low porosity and low permeability.
下扬子地区海相储集岩经过长期压实和地史演化,原生孔隙度和渗透率急剧减小,大部分岩石呈低孔、低渗特征。
4)  Yangtze region
扬子地区
1.
Based on the study of the distribution,age and the characteristics of the assemblage of Triassic marine reptiles of the Yangtze region,combined with the analysis of the relations on the diversification of marine reptiles with sea-level changes,volcanic activities and paleogeographical changes,this paper deals with the origin of the Guanling biota and its taphonomic evolution.
在系统介绍扬子地区三叠纪海生爬行动物分布、时代和组合特征基础上,结合海生爬行动物多样性特点及其与海平面变化、火山活动和古地理变化关系的讨论,分析和讨论了关岭生物群的起源与环境演化特点,指出关岭生物群是古生代末期全球生物大绝灭之后,中生代早期海洋生物复苏和生态系统重新建立过程中,在扬子地台三叠纪浅海陆棚环境中的生物与环境协同演化发展所形成的,以海生爬行动物为特色,集多门类脊椎和无脊椎于一体的生物群落。
2.
In the Yangtze region, Ordovician paleogeographic conditions were favorable to the development of source, reservoir and seal rocks in petroleum systems.
扬子地区奥陶纪古地理条件有利于含油气系统生储盖层的发育。
3.
Based on the study of the distribution,age and the characteristics of the assemblage of Triassic marine reptiles of the Yangtze region,combined with the analysis of the relations on the diversification of marine reptiles with sea-level changes,volcanic activities and paleogeographical changes,this paper deals with the origin of the Guanling biota and its taphonomic evolution.
在系统介绍扬子地区三叠纪海生爬行动物分布、时代和组合特征基础上,结合海生爬行动物多样性特点及其与海平面变化、火山活动和古地理变化关系的讨论,分析和讨论了关岭生物群的起源与环境演化特点, 指出关岭生物群是古生代末期全球生物大绝灭之后,中生代早期海洋生物复苏和生态系统重新建立过程中,在扬子地台三叠纪浅海陆棚环境中的生物与环境协同演化发展所形成的,以海生爬行动物为特色,集多门类脊椎和无脊椎于一体的生物群落。
5)  middle Yangtze area
中扬子区
1.
Cambrian sequence stratigraphy of the middle Yangtze area;
扬子区寒武纪层序地层研究
6)  Upper Yangtze Region
上扬子区
1.
Sequence stratigraphic framework and its palaeogeographic setting for the Loushanguan Group dolostones of Cambrian in Upper Yangtze Region;
扬子区寒武系娄山关群白云岩层序地层格架及其古地理背景
2.
This genus is widespread in the Upper Yangtze region Silurian, especially in the Ningqiang Formation (middle-upper Telychian)of southern Shaanxi and northern Sichuan, the Daluzhai Formation (middle-upper Telychian), northeastern Yunnan and the Shamao Formation, western Hube.
该属在我国上扬子区广泛分布于上兰多维列统(Llandovery)特列奇阶(Telychian)中,主要产自川北、陕南的宁强组、云南大关的大路寨组(中、上Telychian阶))、湖北长阳的纱帽组及四川朝天的王家湾组(下特列奇阶)。
3.
The Lower Silurian (Llandovery) rugose coral assemblage zones of Upper Yangtze region is reviewed based on the study of rugose coral fauna succession and sequence stratigraphy.
根据动物群演替和层序地层的研究,厘定上扬子区下志留统(Llandovery)四射珊瑚组合带序列:(1)香树园组DinophylumRhabdocyclus组合带,时限为Aeronian期;(2)雷家屯组下部StauriaBriantelasma组合带;(3)雷家屯组上部MaikotiaKodonophylum组合带,它们对应于Telychian早期;(4)宁强组GyalophyloidesIdiophylum组合带,相当于Telychian晚期。
补充资料:扬·比比扬历险记

《扬·比比扬历险记》是保加利亚著名作家埃林·彼林(1877~1949)保加利亚著名作家最著名的一部作品,描写一个顽劣的、不听教导的男孩,干了许多坏事,最后还在小魔鬼阿嘘的诱惑下,被换掉了脑袋,骗入魔鬼王国。在魔鬼王国中,他的智慧和善良慢慢苏醒了,终于战胜了恶魔米里莱莱,冲出了魔鬼王国并找到了自己的脑袋,成了一个好孩子。 后来作家还写过一部《月亮上的扬·比比扬》,同样受到孩子们的欢迎。

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