该词条未找到_海词词典

您要查找的是不是：

The increasing volcanism implies that the regional tectonism became progressively severe from the early stage to late stage of the Late Carboniferous. 自晚石炭世早期到晚期，火山活动期逐渐增长，休眠期逐渐缩短，反映出盆地性质自稳定向活动的转化过程。
Late Carboniferous and Early Permian flora is composed of 104 species in 37 genera in Zibo area . 山东淄博地区晚石炭世和早二叠世植物群由37属104种组成。
There are two types of Late Carboniferous rocks in Yanbian stratigraphical province. 本文提出延边地层区的晚石炭世地层有两种类型：一是原地系统的天宝山组；
The Late Carboniferous (Namurian B_C, westphalian, and stephanian) and Permian floras of China represent the Cathaysia flora. 中国的晚石炭世（纳缪尔B_C期、维斯发期和斯蒂芬期）和二叠纪植物群为华夏植物群。
The magnetic declination of palaeomagnetic mean directions of the Bohemian Massif and that of Inner Sudetie Basin of Late Carboniferous Epoc differed 17 degrees. 波希米亚地块与内苏台德盆地地区晚石炭纪古地磁平均方向的磁偏角相差17度。
The emplacement mechanism of late Carboniferous granite are dominated by strong and rotary balloon swelling, and subordinated by tectonic extension. 晚石炭世花岗岩是以强力旋转上升定位的气球膨胀作用机制为主，构造扩展机制为辅。
The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks. 变形带由下石炭统干墩组组成，为一套糜棱岩化火山岩、火山碎屑沉积岩。
The main coal-bearing strata in the Qinshui Basin are late Carboniferous Epoch Taiyuan Formation and Early Permin Epoch Shanxi Formation. 摘要沁水盆地晚古生代含煤地层主要为晚石炭世太原组和早二叠世山西组，可采煤层有太原组第15号煤层和山西组第3号煤层，两者均为高煤阶无烟煤。
The foreland thrust belt in northwestern margin of Junggar basin is a large-scale imbricated thrust system developed since Late Carboniferous. 准噶尔盆地西北缘前陆冲断带是自石炭纪晚期发育起来的大型叠瓦冲断系统,哈拉阿拉特山冲断带为其冲断前锋构造带的东段。
Wu-Xia fault belt is a large-scale overthrust belt developed from Late Carboniferous to Triassic and faults mostly develop below the Triassic. 乌尔禾-夏子街断裂带是一个晚石炭世至三叠纪发育起来的大型逆掩断裂带,断层主要发育在三叠系以下层位,侏罗系以上近于单斜形态。
Study and analysis of brachipod fossils reveal that brachipod distribution was mainly controled by tempreture during the early period of late Carboniferous. 通过晚石炭世早期腕足动物化石资料分析研究,发现该期腕足动物分布主要受温度控制,温度在控制该期全球腕足动物大区一级分布十分明显。
The characteristics mentioned above are controlled by the development and evolution of the northern Xinjiang Hercynian geosyncline region of Late Carboniferous age. 上述特点的产生受新疆北部晚石炭世古海西地槽区发展演化的控制。
By the Late Carboniferous the continents that make up modern North America and Europe had collided with the southern continents of Gondwana to form the western half of Pangea. 三亿六百万年前：晚石炭纪，地质历史上强烈的成煤时期地球演化到晚石炭纪，构成今天北美和欧洲的陆块和冈瓦那南部的陆块碰撞后形成了泛大陆的西部。
Late Carboniferous allochthonous coal is characterized by silty grains and shows similar turbidity sequence, without strike_lenticular structure commonly shown in in_situ coal. 河南宜洛煤田晚石炭世太原组中的异地煤，不存在通常在煤层中见到的那种条带状-透镜状结构，而呈现出是一种粉粒状的、具有浊积层序特征的煤层。
The sedimentary hiatus in Xiaohaizi Formation and late age of late carboniferous in Tarim basin are found and demonstrated by the authors for the first time. 首次发现和论证了巴楚小海子地区小海子组内和塔里木盆地内部晚石炭世晚期的沉积间断；
In the late Carboniferous, rift bay deposit occurred in Helanshan, while widespread epicontinental sea deposit developed in the area east of paleo-mid-ridge. 中二叠世早期，研究区由北向南依次为冲积扇、辫状河、辫状河三角洲平原、辫状河三角洲前缘和滨浅湖所占据。
Recently some Brachiopoda, coral, gastropoda, phytolite is identified by Nanjing Institute of Geology and Palaeontology China Academy of Sciences.The age belongs to Late Carboniferous epoch. 在该地层中发现了一些腕足类、珊瑚、腹足类、植物化石，经中国科学院南京地质古生物研究所鉴定，时代属晚石炭世晚期。
As one of the typical cool water brachiopod, Anidanthus had a main time range between Sakmarian of the early Permian and Wordian of the middle Permian. Several pioneers appeared in Bashkirian of the late Carboniferous. Anidanthus是凉水型腕足动物的代表之一 ,主要出现在早二叠世Sakmarian期至中二叠世Wordian期 ,先驱分子在晚石炭世的巴什基尔期已出现 ,部分种延至晚二叠世。
Abundant late Carboniferous fusulinids are found in this section including Eostaffella,Pseudoendothyra,Milleralla,Ozawainella,Pseudostaffella,Profusulinella,Fusulina,Fusulinella,Triticites,and Protricites. The base of the section is not exposed . 碳酸盐岩中含丰富的Eostaffella、Pseudoendothyra、Milleralla、Ozawainella、Pseudostaffella、Profusulinella、Fusulina、Fusulinella、Triticites、Protricites等,属于典型的石炭纪分子。
From the Late Carboniferous to the end of Permian, the spores of the Shishuyuan trough were from the North China Province, and the marine sediments were absent in the southern part of EQM. 晚石炭世至二叠纪末，柿树园海槽的孢子见于华北生物省，东秦岭南部缺乏海相沉积。

今日热词