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- Transgression of Late Paleozoic Era in Ordos Area 鄂尔多斯地区晚古生代的海侵
- THE DELTA DEPOSITIONAL SYSTEM DISTRIBUTION OF LATE PALEOZOIC ERA IN ORDOS BASIN 鄂尔多斯盆地晚古生代三角洲沉积体系平面展布特征
- STUDY OF THE DISPOSITIONAL PROVENANCE OF THE TERRIGENOUS DETRI TUS IN ORDOS BASIN IN LATE PALEOZOIC ERA 鄂尔多斯盆地晚古生代陆源碎屑沉积源区分析
- late Paleozoic Era 晚古生代
- South Tianshan: a Late Paleozoic or a Triassic orogen? 南天山:晚古生代还是三叠纪碰撞造山带?
- South Tianshan:a Late Paleozoic or a Triassic orogen? 南天山:晚古生代还是三叠纪碰撞造山带?
- Cambrian The earliest period of the Paleozoic era, about 590-510 million years ago. 寒武纪:地质年代古生代的第一个纪，在五亿九千万到五亿一千万前。
- Of,belonging to,or designating the geologic time,system of rocks,and sedimentary deposits of the seventh and last period of the Paleozoic Era. 二叠纪的，二叠岩的是、属于或标明为古生代第七个和最后一个阶段的地质时期、岩层及沉积矿藏。
- The following examples of oil and gas fields in distributary and delta-fringe sand bodies range in age from Late Paleozoic to Middle Cenozoic. 下面所列举的是分布于分流和三角洲前绿砂体的油气田的例子，在地质时代上从晚古生代至中新生代。
- Cambrian: the beginning of the Paleozoic Era Animals with hard-shells appeared in great numbers for the first time during the Cambrian. 寒武纪：古生代的开始（距今5亿1,400万年前），具有硬壳的生物在寒武纪第一次大量出现。
- Research on brachiopod fauna and stratigraphy of the late paleozoic in north China platform II. 华北地台晚古生代腕足动物群及其地层研究2。
- The foreland basin of Late Paleozoic is accumulated by the Upper Devonian and Lower Carboniferous. 晚古生代在前陆盆地率先接受了上泥盆统、下石炭统沉积;
- Of, belonging to, or designating the geologic time, system of rocks, and sedimentary deposits of the seventh and last period of the Paleozoic Era. 二叠纪的，二叠岩的是、属于或标明为古生代第七个和最后一个阶段的地质时期、岩层及沉积矿藏
- From the end of Late Paleozoic to early of Mesozoic, the blocks combined with Laurasia at the south margin. 将介于劳亚大陆和冈瓦纳大陆之间的古陆体，称之谓华夏古陆群。
- The formation of Guangdong modem flora can be traced back to the development of native late Paleozoic cathaysian flora. 摘要广东现代植物区系的形成可以追溯到本区晚古生代华夏植物群的发展。
- The rock combination and lithofacies of the Late Paleozoic marine volcanic rocks are quite complex. 晚古生代海相火山岩相岩石组合较复杂。
- The major structure in the area is the NE-NNE folded belt consisting of Banxi Group of the Middle Proterozoic era to the Ordovician system of the Early Paleozoic era. 由新元古界板溪群至下古生界奥陶系所构成的NE-NNE向褶皱带为区内主体构造；
- Cathaysia Flora, one of the four famous floras of Late Paleozoic, is always the focus of study to palaeobotanists at home and abroad. 作为晚古生代全球四大著名植物群之一的华夏植物群 (CathaysiaFlora),一直是国内外古植物学家研究的焦点。
- The deposits are related to each other, forming a genetic system from Late Paleozoic to Early Mesozoic eras in Zhenan-Xunyang area. 它们构成镇安－旬阳地区晚古生代到早中生代的一个互有联系的成因体系。
