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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。
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?
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。
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 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。
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。
From late Paleozoic to early Mesozoic, there was a complex trench-arc-basin system between Yangtze and Cathaysia blocks. 从晚古生代-早中生代，扬子陆块和华夏陆块之间可能存在一个复杂的沟弧盆体系。
From the Early Triassic to Late Tiassic,the depocenter and subsidence center moved southward progressively,while the frontal uplift retreated toward the foreland continually. 从早三叠世到晚三叠世，盆地的沉积和沉降中心持续南迁，前缘隆起则持续向前陆方向后退。
At the early stage of Late Paleozoic, the Paleo-Asian Ocean, paleo Atlantic and paleo-Tethys were formed by sea-floor spreading, the main plates were also formed at the same time. 晚白垩世中期喜马拉雅-印度地块快速北移，新特提斯洋宽度快速缩小，到第三纪晚期消亡，从而结束了特提斯构造域演化历史。
The sedimentary environment of the Early Feixianguan Age of Early Triassic in northeastern Sichuan Basin mainly inherited the pattern of the Late Changhsingian Age of Late Permian. 摘要四川盆地早三叠世飞仙关早期的环境基本上继承了晚二叠世长兴期末的格局。
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。
Early Triassic Daye Group and Middle-late Triassic Puqi Group are host rocks of Fe-Cu deposits in the eastern Hubai. 侵入接触带构造,捕虏体接触带构造,断裂叠加接触带构造,断裂构造是矿床的容矿构造。
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。
This paper divides4 plus successions of early triassic epoch Feijian tan group in Pingle sag west section. 在萍乐坳陷西段早三叠世飞剑潭组划分出4个正层序。
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;
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。
There exists an extended set of early Triassic intermediate-acid volcanics closely related to microdot gold ore in Southwestern Guangxi. 摘要桂西南广泛发育一套与微粒型金矿密切相关的早三叠世中酸性火山岩。
The Liufengguang flysch here refers to the early Triassic flysch formation of the Liufengguang group in the East Qinling miogeosyncline. 正>留凤关复理石,系指东秦岭冒地槽早三迭世留凤关群的复理石建造。它位于宝成铁路的凤县至聂家湾一带(图1),向西延至西秦岭。