您要查找的是不是：
- late Paleozoic basin 晚古生代盆地
- The Evolution of Late Paleozoic Basins in North Margin of North China Block and the Coupling Relationship between Basin and Range 华北地块北缘晚古生代盆地演化及盆山耦合关系
- 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;
- Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental-island arc collusion stage after the close of Paleo-Tethys ocean. 三叠纪沉积盆地建立在晚古生代褶皱基底之上,形成于古特提斯洋闭合后,造山早期的弧陆碰撞阶段。
- The sedime ntary conglomerates in Late Paleozoic from Daqingshan coalfield was tightly rela ted to the rising of northern orogenic zone and deposited in foreland basin. 大青山煤田晚古生代沉积砾岩的形成与北部造山带的隆升密切相关,它们是前陆盆地的沉积产物。
- Zhifang region of east Junggar is situated at the Late Paleozoic trench arc basin system of northeast Junggar and south marginal active belt of Junggar. 纸房地区位于准噶尔东北晚古生代沟－弧－盆系和准噶尔南陆缘活动带。
- 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?
- Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental island arc colliusion stage after the close of Paleo Tethys ocean. 三叠纪沉积盆地建立在晚古生代褶皱基底之上，形成了古特提斯洋闭合后，造山早期的弧陆碰撞阶段。
- 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?
- Under the tectonic backgrounds of island arc belt, fore-arc trench belt, back-arc basin, and epicontinental active belt of Late Paleozoic, it has different volcanic rock characteristics. 在晚古生代岛弧带、弧前海沟带、弧后盆地或陆缘活动带等构造环境下发育有不同的火山岩组合。
- The Tianshan Mountains formed after the closing of the Late Paleozoic oceanic basin and the geomorphological features of the present mountains are the production of Late Cenozoic crustal movement. 天山山脉形成于古生代晚期古洋盆关闭以后，现今山脉的地貌特征则是新生代晚期地壳变动的产物。
- 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。
- 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。
- 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。
- 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。
- In Mesozoic, Guangdong flora had a big change, the gymnosperm was prosperous, but it was evolved from the late Paleozoic Cathaysian flora as a whole. 中生代，广东植物区系成分发生了很大的变化，裸子植物大量繁盛，但总体上是在本区晚古生代华夏植物区系的基础上演化而来的。
- The Late Paleozoic volcanic rocks (from Early Devonian to Early Permian) were widely distributed in the south margin of the Altai Mountains. 阿尔泰山南缘晚古生代火山岩十分发育,从早泥盆世到早二叠世均有发育。
