1) Late Sinian-Early Cambrian
晚震旦世-早寒武世
2) Neoproterozoic-Lower Cambrain
晚震旦世-早寒武世地层
3) Late Sinian
晚震旦世
1.
Sedimentary characteristics and lithofacies palaeogeography of the Late Sinian and Early Cambrian in middle Yangtze region;
中扬子地区晚震旦世—早寒武世沉积特征及岩相古地理
2.
The Late Sinian microbiolite and its phosphorus enrichment in Central Guizhou Province;
黔中晚震旦世微生物岩及其磷的富集
3.
Based on the discovery of breakup uncomformity between the Lower Sinian Sidingshan Formation and the Fengtai Formation, the field features and geochemical evidence of the unconformity,and the Pb-Pb isochronal dating of silt mudstone interbeds from the Fengtai Formation being 620 Ma,the paper thought that the Fengtai Formation should be deposits of Late Sinian.
本文根据下震旦统顶部与凤台组之间裂离不整合的发现及其意义的讨论,以及凤台组夹层粉砂质泥岩620Ma的Pb-Pb等时线年龄,基本厘定出凤台组时代为晚震旦世。
4) Early Sinian
早震旦世
1.
Sedimentary facies and palaeogeography during the Early Sinian and potential of the rhodochrosite deposits in northeastern Guizhou and its adjacent areas;
黔东北及邻区早震旦世成锰期岩相古地理及菱锰矿矿床
2.
The Lower Sinian of Hunan Province has been divided into five sedimentary formation series and an ideal cross-section showing the Early Sinian tectonics and sedimentary formation of hunan Province has been restored.
主要从沉积建造角度讨论了各种不同构造古地理、古生物、古环境、地球化学及同位素地质，对早震旦世锰矿成矿的控制。
3.
During Early Sinian Nantuo Stage,three sets of incompleted glacial advance glacial recession sedimentary cycles composed of glacial drift and aqueoglacial facies developed in the eastern Yangtze Gorges.
三峡东部早震旦世南沱期，自下而上由冰碛相、冰水相组成三套冰进－ 冰退不完整的沉积旋回。
5) Late Cambrian and Early Ordovicain
晚寒武世至早奥陶世
6) late Cambrian
晚寒武世
1.
Sequence stratigraphy of the Late Cambrian strata on the North China platform and the correlation of the sea-level changes with the North America platform;
华北地台晚寒武世层序地层及其与北美地台海平面变化的对比
2.
Primitive euconodonts are extrmely abundant and varied in the Late Cambrian in western Shandong Province.
鲁西地区晚寒武世地层发育 ,产有数量丰富、分异度大的原始真牙形石分子 ,经笔者研究 ,建立了 2新属、2新种及 2未定种 Camconodontus rotundatus gen et sp。
3.
Based on a detailed petrologic and sedimentological study, five 3 rd-order sedimentary cycles have been distinguished in the Late Cambrian strata in the study area, and the basic characteristics of the sedimentary cycles have been analysed and the main factors which control the cycles have been assessed.
华北北部晚寒武世沉积一套多旋回碳酸盐岩建造,在稳定的构造背景和无陆源物质大量供给条件下,这些旋回主要受海平面变化和气候影响控制。
补充资料：武担东台晚望
【诗文】：
憔悴西窗已一翁，登高意气尚豪雄。
关河霸国兴亡後，风月诗人醉醒中。
病起顿惊双鬓改，春归一扫万花空。
栏边徙倚君知否，直到吴天目未穷。
【注释】：
【出处】：
憔悴西窗已一翁，登高意气尚豪雄。
关河霸国兴亡後，风月诗人醉醒中。
病起顿惊双鬓改，春归一扫万花空。
栏边徙倚君知否，直到吴天目未穷。
【注释】：
【出处】：
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