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Unpublished Ph.D thesis of Peking University.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