1.
Candidate for the Cambrian-Ordovician boundary stratotype of Newfoundland
关于纽芬兰寒武系-奥陶系界线层型候选剖面
2.
Study on Depositional Facies and Reservoir Characteristics of Cambrian and Ordovician in Eastern Tarim Basin
塔里木盆地塔东地区寒武系-奥陶系沉积相与储层特征研究
3.
GLAUCONITIZED SPONGE SPICULES FROM THE YELI FORMATION AT THE DAYANGCHA CAMBRIAN-ORDOVICIAN BOUNDARY SECTION,JILIN
吉林大阳岔寒武系-奥陶系界线剖面冶里组海绿石化海绵骨针化石
4.
Petroleum Geologic Features of Cambrian-Ordovician in Tarim Basin
塔里木盆地寒武──奥陶系石油地质特征
5.
Major hydrocarbon source rocks are in the Cambrian and Ordovician.
寒武-奥陶系烃源岩是该区主力烃源岩;
6.
STUDY ON THE CAMBRIAN-ORDOVICIAN CONODONTS FROM ZHUJI,ZHEJIANG
浙江诸暨地区寒武-奥陶系牙形石研究
7.
A New Data on Determination of the Boundary between Cambrian and Ordovician in Tongren, Guizhou
贵州铜仁寒武系与奥陶系界线划分新资料
8.
Sedimentary facies analysis of Cambrian-Ordovician in eastern Tarim Basin
塔里木盆地东部地区寒武系—奥陶系沉积相分析
9.
The Ordovician Conodonts and the Cambrian-Ordovician Boundary at the Platform Facies in the Tarim Basin, China
塔里木盆地奥陶纪台地相区牙形石及寒武—奥陶系界线
10.
THERMOLUMINESCENCE OF THE CAMBRIAN AND ORDOVICIAN LIMESTONES FROM EASTERN HEBEI AND WESTERN ZHEJIANG, CHINA
浙西、冀东寒武-奥陶系灰岩地层的热发光特征
11.
TYPES AND ORIGINS OF CAMBRIAN-ORDOVICIAN DOLOMITE IN SOUTHERN ANHUI
皖南寒武-奥陶系白云岩类型及成因探讨
12.
NEW DATA FROM THE CAMBRIAN AND ORDOVIAN IN THE SHIHUIGOU AREA, ULAN COUNTY, QINGHAI PROVINCE
青海乌兰石灰沟地区寒武、奥陶系新材料
13.
Research of Cambrian-Ordovician Sedimentary System and Its Petroleum Accumulation Conditions of Middle Tarim-basin;
塔中寒武—奥陶系沉积特征与成藏条件研究
14.
Evaluation on Efficient Source Rock of Cambrian-Ordovician in Tarim Basin, China;
塔里木盆地寒武—奥陶系有效烃源岩评价
15.
Study of Sedimentary Facies Characteristic of Cambrian-Ordovician in Awati Fault Depression and Its Surrounding Region
阿瓦提断陷及邻区寒武—奥陶系沉积相特征研究
16.
Study on the Carbonate Reservoir Characteristics in the Cambrian System to Lower Ordovician Series in the East of Tarim Basin
塔东地区寒武系—下奥陶统碳酸盐岩储层研究
17.
The Evolution of Structure and Sediment & Their Correlation of Cambrian-Ordovician in TaZhong Area, Tarim Basin;
塔里木盆地塔中寒武系—奥陶系构造与沉积演化及相互关系研究
18.
The average content of gold in the strata of Cambrian and Ordovician System inthe eastern sector of Tuolaishan ore belt is 8 to 14 times higher than that of crust.
托莱山矿带东段寒武系、奥陶系金平均含量高于地壳丰度的8～14倍。