1) Sinian-Triassic
震旦-三叠纪
2) Sinian-Middle Triassic
震旦系-中三叠统
3) pre-Sinian
前震旦纪
1.
Further discussion of mapping method in South China outcroppedareas of pre-Sinian low-grade metamorphic rocks;
再论华南前震旦纪浅变质岩区区调方法
2.
Features of the pre-Sinian structural deformation in North Jiangxi and its dynamic significance;
赣北前震旦纪构造变形特征及其动力学意义
3.
Zircon Pb-Pb ages of Pre-Sinian basement in central Guangdong Province and their geological significance;
粤中前震旦纪基底锆石Pb-Pb蒸发年龄及其地质意义
4) Sinian
震旦纪
1.
Preliminary discussion on ecological characteristics and buried environments of Miaohe-type Biota during the Late Doushantuoian of Sinian in northeastern Guizhou Province;
黔东北震旦纪陡山沱晚期庙河型生物群的生态特征及埋藏环境初探
2.
Sinian Lithostratigraphic Classification and Correlation in Jiangxi Province;
江西省震旦纪岩石地层划分与对比
3.
Sedimentational Geochemical Characteristics of the Sinian Cap Carbonate from the Upper Yangtze Region;
上扬子区震旦纪南沱冰期后碳酸盐岩帽沉积地球化学特征
6) Sinian period(system)
震旦纪(系)
补充资料：二叠纪三叠纪灭绝事件
二叠纪-三叠纪灭绝事件，是发生在大约2亿5,200万年前二叠纪和三叠纪交替时期的生物集群灭绝事件。
这一事件导致了70%的陆生物种和90%的海洋物种灭绝。古生代海洋中由海百合-腕足动物-苔藓虫组成的表生、固着生物群落迅速退出历史舞台，为中生代由现代软体动物-甲壳动物-硬骨鱼构成的内生、移动生物群落的崛起创造了条件。
有多种理论解释了灭绝的原因，包括：
撞击事件
板块构造
超新星
火山作用
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