1.
The Sea-level Changes during the Latest Ordovician to the Earliest Silurian in the Yangtze Basin and the Subdivision of the Ordovician-Silurian Boundary;
扬子海盆晚奥陶世晚期至志留纪初期海平面升降与奥陶/志留系界线的划分与对比
2.
SOME SILURIAN AND DEVONIAN OSTRACODES FROM JIANGYOU, SICHUAN
四川江油一些志留纪及泥盆纪介形类
3.
An overview of Ordovician and Silurian K-bentonites
奥陶纪和志留纪钾质斑脱岩研究评述
4.
TWO NEW SPECIES OF BRYOZOA FROM THE MIDDLE SILURIAN OF KUANGYUAN, SZECHUAN
四川广元中志留纪苔藓?之二新?(英文)
5.
PRELIMINARY INVESTIGATION ON THE SEDIMENTARY FACIES OF THE MIDDLE SILURIAN URANIFEROUS ROCK FORMATIONS IN WESTERN QINLING
西秦岭中志留统含铀岩组沉积相初析
6.
On the Birth of English Voluntary Hospitals in the Eighteenth and Nineteenth Centuries;
18～19世纪英国志愿医院兴起初探
7.
Comparison of Chinese Students Studying in Japan and U.S. in the Early 20~(th) Century;
二十世纪初中国留日留美学生群体的比较
8.
The Study on the Jewish Women Salon from the Late 18~(th) Century to the Early 19~(th) Century
18世纪末至19世纪初德意志犹太女性沙龙研究
9.
The Characteristics of the Returned Students Index Activities in the Early Twenty Century;
20世纪初期留学生索引活动特点探析
10.
The original survived for eight centuries but collapsed at the beginning of the twentieth century.
其原物存留了8个世纪，于20世纪初倒坍。
11.
On the Progressive Publications by Chinese Students Studying abroad in Japan in the End of the 19~(th) Century and the Beginning of the 20~(th) Century;
19世纪末20世纪初中国留日学生进步刊物浅谈
12.
ORDOVICIAN AND SILURIAN TETRACORAIS FROM THE SOUTHERN PART OF TARBAGATAI MOUNTAIN IN XINJIANG
新疆塔尔巴哈台山南坡奥陶—志留纪四射珊瑚
13.
SILURIAN TUVAELLA GIGANTEA FAUNULE (BRACHIOPODA) OF THE BARKOL AREA, NORTHEASTERN XINJIANG
新疆巴里坤地区志留纪的大型图瓦贝组合
14.
SILURIAN AND DEVONIAN TABULATE CORAL ASSEMBLAGES IN THE BEISHAN AREA, GANSU PROVINCE
甘肃北山地区志留—泥盆纪床板珊瑚的组合序列
15.
GRAPTOLITE ZONE OF THE ORDOVICIAN AND EARLY SILURIAN IN KALPIN REGION, XINJIANG
新疆柯坪地区奥陶纪和早志留世的化石带
16.
ON THE AGE OF SILURIAN AND DEVONIAN FISH-BEARING STRATA FROM EASTERN CHINA
关于华东志留、泥盆纪含鱼层时代的商榷
17.
NEW MATERIAL OF THE PROETID TRILOBITE LATIPROETUS LU,1962 FROM AERONIAN (LLANDOVERY,SILURIAN) OF WESTERN HUBEI,CHINA
鄂西志留纪早期三叶虫Latiproetus Lu,1962的新材料
18.
A rift trough along Mianxian -Lueyang ophiolitic melange belt was formed from Ordovician to Silurian.
奥陶纪—志留纪大致沿勉略构造带形成南秦岭裂陷槽。