A Giant Palaeoslope Zone of Early Paleozoic Era in Southeastern Yangtze Landmass 扬子陆块东南缘早古生代的巨型斜坡带
The deformation myth of all nationalities is the product of life and thought in the Paleozoic era ( or primitive times). 变形神话是各民族在上古时代(或原始时代)的生活和思想的产物。
The extensive deposition of potash salts in North America in Paleozoic Era was associated closely with the position of paleoequator. 北美晚古生代钾盐大规模集中成矿作用,也与该时期北美大陆古赤道位置密切相关。
The age of emplacement is at Upper Paleozoic Era from the result of isotopic age determination. 依据同位素测年结果,确定其侵位时代为晚古生代晚期。
In Paleozoic Era stable marine sediments of platform type covered it. 古生代为稳定的海相地台类型沉积;
Transgression of Late Paleozoic Era in Ordos Area 鄂尔多斯地区晚古生代的海侵
Wave Structre in Paleozoic Era of Ordos Basin and Its Significance in Paleogeography 鄂尔多斯盆地早古生代波状构造及其古地理意义
The Caledonian movement took place in late Ordovician and may be divided into two phases, corresponding to arc-continent collision and continent-continent collision in the North Qinling orogenic belt during early Paleozoic Era respectively. 加里东运动形成于奥陶纪晚期,可再细分为两期,分别与北秦岭构造带早古生代的弧-陆碰撞与陆-陆碰撞作用有关。
In this paper, by researching the sandstone type, the distribution and change of lithic fragment types and the distribution and change of the heavy minerals assemblage type in the Ordos Basin during the Late Paleozoic era, the authors divide the basin into several districts. 通过对鄂尔多斯盆地晚古生代砂岩类型、岩屑类型和重矿物组合类型的分布及其变化研究,将整个盆地进行了分区。
The Biotic Groups and Stratigraphic Subdivision of Late Paleozoic Era in Tengxian Coalfield of Shandong-On Carboniferous-Permian Boundary 山东滕县煤田晚古生代生物群及地层划分兼论石炭二叠系界线
Characteristics of arc structure zones in the paleozoic era of Hainan island, and its geological implications 海南岛古生代弧状构造带的特征及其地质意义
The Sichuan Basin, a large Paleozoic and Meso-cenozoic era marine and continental basin, is situated between Tethys tectonic domain and marginal Pacific tectonic domain, which control its formation and development. 四川盆地是特提斯构造域巨型油气富集带中一个大型古生代中新生代海相陆相叠合盆地,其形成与演化受特提斯构造域与滨太平洋构造域控制。
The content and the distributing law of the microelements in lower paleozoic era stone coal in South Qinling have been systematically studied. 对南秦岭早古生代石煤的微量元素含量、分布规律等进行了详细系统的研究。
The discovery of hornfelsed basic rock veins discloses that strong geologic process with the activity of fault, magma and metamorphism were still taken placed in Paleozoic era within the metamorphic basement of the Xiangshan uranium ore field. 这一角岩化基性脉岩的发现,揭示在古生代相山铀矿田变质基底仍然遭受着断裂活动、岩浆活动和变质作用三者相伴随的较为强烈的地质构造作用。
On the Sedimentary Formation of Early Paleozoic Era and Sedimentary Facies-Paleogeographic Environment in West Fujian Province 论福建西部早古生代的沉积建造及岩相古地理环境
Difference in Coal Quality Between Seams of the Late Paleozoic Era in the Eastern Part of North China and Their Microscopic Characteristics 中国华北东部晚古生代煤层的煤质差别和显微特征
Since Paleozoic era, the plate movement resulted in the formation of five types of different sedimentary bases and even the formation of five types of different basin. 该区古生代以来的板块运动,使不同大地构造环境具有五种不同的沉积基底,伴之以形成五种类型的沉积盆地。
The exhalation-spout type deposits of the early Paleozoic era and the orogenic type deposits of the late Paleozoic to early Mesozoic era are the most important deposit groups. 早古生代时期的喷气喷流型矿床组合和晚古生代&早中生代时期的造山型矿床组合最为重要。
Double magmatic arcs, which were formed in Late Paleozoic Early Mesozoic era, were orogenic magmatic arcs at different stages in the same geodynamic mechanism. 晚古生代&早中生代发育的双岩浆弧是在同一动力学机制下不同阶段形成的造山岩浆弧:陆缘的钙碱性岩浆弧和陆内的高钾钙碱性岩浆弧。
Paleozoic era ophiolite of south west part in Western junggar, xinjiang, china 西准噶尔西南地区古生代蛇绿岩
Liming basin is a foreland basin developed on the passive continent margin of north margin of Yangtse platform during late Paleozoic Era. 礼岷盆地是晚古生代在扬子板块北缘被动陆缘之上发育起来的前陆盆地。
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
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;
The subsidence curves of Michigan Basin during Paleozoic era were modeled by using the layered thermo-elastic model in the paper. 用这种热弹性分层模型模拟计算了密执根(Michigan)盆地在古生代的沉降曲线。
The main geothermal reservoirs are reservoir of karst fissure of Cambrian-Ordovician, reservoir of pore and fracture of Cenozoic, and fracture reservoir of granite and metamorphic. The cap rocks are quaternary loose soil and deposition after Paleozoic Era. 热储层主要有寒武-奥陶系岩溶裂隙热储、新生界孔隙-裂隙热储以及花岗岩-变质岩裂隙热储,盖层主要有第四系松散沉积物和古生代以后沉积的地层。