1) 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。
2) Neoproterozoic-Lower Cambrain
晚震旦世-早寒武世地层
3) Late Sinian-Early Cambrian
晚震旦世-早寒武世
4) late Sinian to early Paleozoic
晚震旦世-早古生代
5) 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。
6) late sinian phosphate bearing sequence
晚震旦世含磷层
1.
A sedimentary environment and quantitative analysis of the late sinian phosphate bearing sequence in the west of Zhejiang Province;
本文运用最优预报面成图法（缩写为ＭＰＳ）对浙西晚震旦世含磷层进行定量分析，通过两组（地质和地理）变量之间的典型相关分析和趋势面分析，得到满意的相等值沉积环境图，指导浙西找磷方向。
补充资料：早世
早逝：吾上有三兄，皆不幸早世。
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