1.
The iron bearing formations mainly occur in the Middle and ,especially,Upper Devonian strata.
含矿建造主要赋存于中上泥盆统 ,而以上泥盆统为主。
2.
Sequence Stratigraphy of upper Devonian-Carboniferous in Tarim Basin
塔里木盆地上泥盆统—石炭系层序地层学研究
3.
RESEARCH ON THE MIDDLE/UPPER DEVONIAN BOUNDARY AT DALE, GUANGXI
广西大乐中、上泥盆统界线的再研究
4.
STUDY ON THE UPPER DEVONIAN CYCLIC SEQUENCES OF SHANGNAN SHAANXI
陕西商南地区上泥盆统旋回层序研究
5.
THE UPPER DEVONIAN "SHITI FORMATION" SHOULD BE RENAMED
上泥盆统“石梯组”与侏罗系石梯组重名
6.
A DISCUSSION OF THE DEVONIAN TETRACORAL FOSSIL ASSEMBLAGE ZONES AND THE DETERMINATION OF THE BOUNDARY BETWEEN THE MIDDLE AND UPPER DEVONIAN
湖南泥盆纪四射珊瑚化石组合带及中、上泥盆统界线划分
7.
SOME OSTRACODS OF THE UPPER MEMBER OF XIKUANGSHAN GROUP OF UPPER DEVONIAN IN CENTRAL HUNAN
湘中上泥盆统锡矿山组上段介形类化石
8.
The foreland basin of Late Paleozoic is accumulated by the Upper Devonian and Lower Carboniferous.
晚古生代在前陆盆地率先接受了上泥盆统、下石炭统沉积;
9.
ROBUST ELEMENT ABUNDANCE ANALYSIS AND ELEMENT ABUNDANCE OF THE UPPER DEVONIAN STRATA IN NANDAN-HECHI BASIN, GUANGXI PROVINCE
稳健丰度分析及丹池盆地上泥盆统元素丰度的意义
10.
Reservoir Characteristics and Evaluation of Donghe Sandstone of the Upper Devonian in Tarim Basin
塔里木盆地上泥盆统东河砂岩段储层特征及评价
11.
FEATURES AND PROSPECT MEANING OF THE REEFS OF MIDDLE-UPPER DEVONIAN, SOUTHWESTERN HUNAN, CHINA
湘西南中、上泥盆统礁特征及其找矿意义
12.
GRAVITY-FLOW DEPOSITS IN THE UPPER DEVONIAN TONGYUSI FORMATION,SHANYANG,SHANXI.
陕西山阳地区上泥盆统桐峪寺组重力流沉积
13.
CONCHOSTRACANS AND SPORES OF UPPER DEVONIAN HUANGJIADENG FORMATION IN HUBEI PROVINCE
湖北长阳上泥盆统黄家磴组叶肢介和孢子
14.
ANALYSIS OF SEDIMENTARY ENVIRONMENT IN THE CHAKOUHE FORMATION OF UPPER DEVONIAN,TEWO,GANSU
甘肃迭部上泥盆统擦括合组沉积环境分析
15.
Study on Outcrop Sequence Stratigraphy of the Upper Devonian Xihu Formation in Hangzhou
杭州上泥盆统西湖组露头层序地层研究
16.
Paleoxygenation facies and oxygen-deficient environmental model of the Devonian source rocks from southern South China Sea:An example from the Middle and Upper Devonian of Guangxi
南华海泥盆纪烃源岩的古氧相和缺氧环境模式——以广西中、上泥盆统为例
17.
The Late Devonian (?) Bakken is believed to have been at least 150 my old when it released much of its oil.
上泥盆统Bakken组据信已释放出了其大部分石油至少150百万年。
18.
FIRST DISCOVERY OF A STEM WITH INTERNAL STRUCTURE REFERABLE TO LEPTOPHLOEUM RHOMBICUM FROM THE UPPER DEVONIAN, XINJIANG
斜方薄皮木茎干内部构造在新疆上泥盆统的首次发现