晚寒武世,late Cambrian
1)late Cambrian晚寒武世
1.Sequence stratigraphy of the Late Cambrian strata on the North China platform and the correlation of the sea-level changes with the North America platform;华北地台晚寒武世层序地层及其与北美地台海平面变化的对比
2.Primitive euconodonts are extrmely abundant and varied in the Late Cambrian in western Shandong Province.鲁西地区晚寒武世地层发育 ,产有数量丰富、分异度大的原始真牙形石分子 ,经笔者研究 ,建立了 2新属、2新种及 2未定种 Camconodontus rotundatus gen et sp。
3.Based on a detailed petrologic and sedimentological study, five 3 rd-order sedimentary cycles have been distinguished in the Late Cambrian strata in the study area, and the basic characteristics of the sedimentary cycles have been analysed and the main factors which control the cycles have been assessed.华北北部晚寒武世沉积一套多旋回碳酸盐岩建造,在稳定的构造背景和无陆源物质大量供给条件下,这些旋回主要受海平面变化和气候影响控制。
英文短句/例句

1.Fengshanian stage凤山阶-晚寒武世晚期
2.LATE MIDDLE AND EARLY LATE CAMBRIAN AGNOSTIDS IN HUAYUAN, HUNAN湖南花垣中寒武世晚期至晚寒武世早期球接子类
3.LATE MIDDLE AND EARLY LATE CAMBRIAN CONODONTS FROM HUAYUAN,HUNAN湖南花垣中寒武世晚期至晚寒武世早期牙形石动物群(英文)
4.DISCOVERY OF GRAPTOLITE FROM FENGSHAN FORMATION OF UPPER CAMBRIAN IN SOUTHERN LIAODONG PENINSULA AND DISCUSSION ABOUT THE TOP OF CAMBRIAN辽东半岛南部晚寒武世凤山组笔石的发现兼论寒武系顶界
5.SEQUENCE STRATIGRAPHIC STUDY OF MIDDLE-UPPER CAMBRIAN DOLOMITE FACIES, IN BORDER OF GUIZHOU AND HUNAN湘黔交境中晚寒武世白云岩相区层序地层研究
6.THE DISCOVERY OF THE LATE CAMBRIAN GUSHAN-AGED STRATA IN WESTERN YUNNAN AND THEIR SIGNIFICANCE滇西晚寒武世崮山期地层的发现及其意义
7.The Stratigrphic Significance of the Astronomical Period and the Storm Founction of Late Cambrian in North China华北晚寒武世风暴作用与天文周期的地层意义
8.Depositional Environments and Sequence Stratigraphy of the Late Cambrian, Luxi Block, China;鲁西晚寒武世沉积环境与层序地层研究
9.MEI Shi-long,1991.Middle and Late Cambrian conodont and trilobite biostratigraphy in Wanxian,Hebei.Unpublished Ph.D thesis of Peking University.武桂春,2003.鲁西地区晚寒武世牙形石.北京大学博士研究生学位论文.
10.Late Cambrian Conodonts Composition and the Determination of Cambrian and Ordovician Boundary in Huangyangshan of Laiwu City in Shandong Province山东莱芜黄羊山晚寒武世牙形石组合及寒武系与奥陶系界线的确定
11.Study on the Bioherm Structure of Middle-Late Cambrian Sedimentary Sequences in the North China Platform华北地台中晚寒武世沉积层序中生物丘构造研究
12.MIDDLE AND EARLY UPPER CAMBRIAN TRILOBITES FROM KUNSHAN, JIANGSU WITH REFERENCE TO THEIR DISTRIBUTION IN THE LOWER YANGTZE REGION从江苏昆山中、晚寒武世三叶虫的发现,试论长江下游的生物分区
13.LATE CAMBRIAN FENGSHANIAN TRIOBITE COMMUNITY AND ENVIRONMENTAL ANALYSIS IN SOUTHERN JILIN吉林南部晚寒武世凤山期三叶虫化石群落与沉积环境分析
14.Stud on Carbonate Petro;ogy, Sedimentology and Sedimentational Synchrony of Late Cambrian in the North Part of North China Platform;华北北部晚寒武世碳酸盐岩岩石学沉积学及沉积作用等时性研究
15.This paper is a continuation of the papers on lithofacies palaeogeography of the Early, Middle and Late Cambrian and the Early and Middle Ordovician.本文是笔者等的中国早、中、晚寒武世和早、中奥陶世岩相古地理诸文的继续。
16.The material source of the Carboniferous karst type bauxite in North China mainly came from the underlying Late Cambrian-Middle Ordovician carbonate rock.华北石炭纪岩溶型铝土矿的主要物质来源为下伏的晚寒武世—中奥陶世碳酸盐岩。
17.The discovery of the tempestites is of great significance to restructure the palaeogeography of Middle-Late Cambrian in Huangshi, eastern Hubei Province.该风暴岩的发现对重建鄂东黄石地区中晚寒武世古地理及区域地层对比具有重要意义。
18.Chancelloriids from Late Middle Cambrian of Huayuan,Hunan,South China湖南花垣中寒武世晚期开腔骨类化石
相关短句/例句

Middle and Late Cambrian中-晚寒武世
3)Middle-Upper Cambrian中晚寒武世
1.Many newly_discovered paleo_karst unconformity interfaces and exposure zones and some para_sequences and their superimposed patterns can both be employed to divide the Middle-Upper Cambrian dolomite facies in border of Guizhou and Hunan into seven third_order sequences.根据新发现的许多古岩溶不整合面和暴露带 ,以及副层序和副层序叠置规律 ,将湘黔交境台地中晚寒武世娄山关组 (白云岩相 )划分为 7个三级层序 ,每一层序都由海进体系域和高水位体系域组成 ,缺少低水位体系域沉积 。
4)Late Cambrian and Early Ordovicain晚寒武世至早奥陶世
5)Neoproterozoic-Lower Cambrain晚震旦世-早寒武世地层
6)Late Sinian-Early Cambrian晚震旦世-早寒武世
延伸阅读

晚寒【诗文】:急景流如箭,凄风利似刀。暝催鸡翅敛,寒束树枝高。缩水浓和酒,加绵厚絮袍。可怜冬计毕,暖卧醉陶陶。【注释】:【出处】:全唐诗