1) terminal proterozoic
末元古代
2) terminal Neoproterozoic
末元古纪
1.
Cloudina was known as the first animal acquired mineralized skeleton at the terminal Neoproterozoic,but it was not the only exception that could secret minerals.
末元古纪以Cloudina为代表的管状动物化石是目前世界上公认最早的具矿化骨骼的生物类群,在世界许多地区都有发现,但它并不是当时唯一的矿化生物类型,更多的动物骨骼化化石证据在寒武纪大爆发之前的沉积物中时有发现。
3) Paleoproterozoic
古元古代
1.
The Minerogenic Fluids of Magnesite and Talc Deposits in the Paleoproterozoic Mg-rich Carbonate Formations in Eastern Liaoning Province;
辽东古元古代富镁质碳酸盐岩建造菱镁矿滑石矿床成矿流体研究
2.
Paleoproterozoic events in the North China Craton.;
华北克拉通古元古代构造事件
3.
Magma recording of Paleoproterozoic orogeny in central segment of northern margin of North China Craton:Geochemical characteristics and zircon SHRIMP dating of S-type granitoids;
华北克拉通北缘中段古元古代造山作用的岩浆记录:S型花岗岩地球化学特征及锆石SHRIMP年龄
4) Palaeoproterozoic
[pæliəuprəterə'zəuik]
古元古代
1.
The Palaeoproterozoic Erdaowa Group distributed in the north Hohhot, Nei Mongol is composed of metamorphic detrital sediment and carbonate with intermidiate basic volcanics.
研究表明 ,二道洼群是古元古代早期产物 ,2 4 50~ 2 4 0 0Ma开始接受沉积 ,大约在 2 2 0 0~2 10 0Ma之间开始褶皱回返 ,遭受了低角闪岩相变质作用 ,具有碰撞造山带的变质P T t轨迹。
2.
The rhyolites in the Upper Luliang Group of Shanxi Province of China are Palaeoproterozoic A-type volcanic rocks.
山西吕梁群流纹岩是一个古元古代的弱碱性火山岩。
3.
Palaeoproterozoic formation lacks variety of standard fossils, thus it become difficult to compare the whole world formations or large .
古元古代地层缺乏种类繁多的标准化石,这使大区域性的、全球性的地层对比难以实现。
5) Paleo-Mesoproterozoic
古-中元古代
1.
Sm and Nd isotopic geochemistry of Paleo-Mesoproterozoic meta-basic volcanics from Middle Hainan,China;
琼中古-中元古代变质基性火山岩地球化学特征
2.
Chronology and geological implication of the Paleo-Mesoproterozoic alkaline-rich intrusions belt from the northern part in the North China Craton.;
华北克拉通北部地区古-中元古代富碱侵入岩年代学及意义
6) Neoproterozoic Era
新元古代
1.
The Discovery of Neoproterozoic Era Digging Trace Fossil in Huainan China and Its Geological Significance;
中国淮南新元古代掘迹化石发现及其意义
2.
The Study on Sedimentary Facies of Changlongshan Formation of Neoproterozoic Era in Huailai, Hebei;
河北省怀来新元古代长龙山组沉积相研究
3.
The epoch adscript to the Neoproterozoic Era and that the phosphorite bed located in the Sinian System.
海州—大悟地区变质磷矿含磷岩系(锦屏岩群、宿松岩群、红安岩群)岩层组合,标志岩层,微量、稀土元素特征和沉积环境皆可与鄂西陡山沱期磷矿类比,时代归属为新元古代,其中磷矿层属震旦系。
补充资料:笃笃末末
1.盘盘旋旋。
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