上扬子区下古生界在贵州及其邻区发育较为完整。
The Early Palaeozoic strata of the upper-Yangtze region are fully developed in Guizhou Province and its adjacent areas.
下扬子区再生型和后生型成藏组合具有一定的勘探前景。
The plays of regenerated type and epigenotype in the Middle and Lower Yangtze areas have certain exploration prospects, too.
贵州镇远竹坪地区寒武纪时处于扬子区与江南区之间的过渡区。
In Cambrian, Zhuping of Zhenyuan county, Guizhou province, was located in the transitional zone between the Yangtze platform and the Jiangnan area.
提出了层序样式的概念：研究了中扬子区层序样式基本类型和特点；
The concept of sequence style was suggested, and the basic catalogues and characteristics of sequence style in the Mid-Yangtze area were studied.
无锡嵩山下三叠统碳酸盐浅滩相剖面在中下扬子区具有特殊性和代表性。
The Lower Triassic carbonate bank section of Songshan, Wuxi is particular and typical in the Middle and Lower Yangtze Region.
扬子区早—中三叠世短期变化曲线与世界曲线一致，而长期曲线则不相符。
The Early - Middle Triassic short - term changes of Yangtze are briefly concordant with those of Haq's world curve, whereas its long-term changes are discordant.
与全球海平面变化相比，下扬子区的海平面升降旋回有所不同，有其特殊性。
Compared with the global change of sea level, the eustatic cycle of Lower Yangtze area is somewhat different because of its particularity.
扬子区早志留世珊瑚群与澳大利亚东部、北美东部同期珊瑚也有一定的相似性。
There are also resemblances among Early Silurian rugose coral faunas of the Yangtze region, eastern Australia, and eastern North America to some extent.
下三叠统海相烃源岩是下扬子区最有利的烃源岩，陆相沉积也具有一定的生烃潜力。
The Lower Triassic Marine source rock is the most favorable one in the Lower Yangtze area, and the continental deposit has certain hydrocarbon generating potential.
上扬子区在加里东运动过程中形成前陆盆地，主要经历了三次挤压、挠曲沉降至松驰、抬升过程。
The tectonic subsidence is the main controlling factor in the foreland basin, which went through three periods, namely press, flexure subsidence to laxitas, uplift.
江苏下扬子区的海相中—古生界构造演化经历了前扬子板块、稳定地台和西太平洋活动陆缘等三大阶段。
Marine Meso-Paleozoic structures in the region have undergone three evolution stages of Pre-Yangzi Plate, stable platform and West Pacific active continental margin.
笔者建立了中扬子区寒武系层序地层格架，研究了中扬子区层序界面和体系域特点，分析了中扬子区层序样式的基本类型及其特征。
The present paper deals with the Cambrian sequence stratigraphic framework, sequence boundaries, sequence patterns and systems tracts, in the middle Yangtze area.
笔者建立了中扬子区寒武系层序地层格架，研究了中扬子区层序界面和体系域特点，分析了中扬子区层序样式的基本类型及其特征。
The present paper deals with the Cambrian sequence stratigraphic framework, sequence boundaries, sequence patterns and systems tracts, in the middle Yangtze area.
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