1.
Flow and Deformation Mechanisms of Hornblende Rocks from the Paleoproterozoic Fold Belt in Liaodong Peninsula;
辽东古元古宙褶皱带变质角闪质岩石的流动与变形机制
2.
STRUCTURAL STYLE AND DEFORMATIONAL HISTORY OF THE FUPING ARCHEAN DOMAL COMPOSITE FOLD GROUP
阜平太古宙穹状复合褶皱群的构造样式及变形史
3.
PROTEROZOIC TECTONIC SLICES ALONG THE NORTHERN MARGIN OF NORTH CHINA PLATE
华北板块北缘活动带元古宙构造岩片
4.
The Shengong Movement in late Middle Proterozoic Era was strong and the superimposed fold of Junning Movement in late Qingbaikou Period was clear.
中元古代末的神功运动表现强烈，青白口纪末的晋宁运动叠加褶皱明显。
5.
5)Cale-donian fault-fold belt (Hercynian deformation) in the southeast of it ;
5）塔东南中、新元古基底的加里东断褶带（海西改建）；
6.
The early Precambrian in Jilin province includes the Archaeozoic granite-greenstone belt,early Proterozoic Ji’an Group and mid Proterozoic Laoling Group .
吉林省早前寒武纪地质包括太古宙花岗—绿岩带、早元古代集安群和中元古代老岭群。
7.
accumulation zone of thrust fold
逆掩断裂褶皱聚集带
8.
GEOLOGICAL SIGNIFICANCE OF THE NEOARCHEAN GLOBAL CRATONIZATION EVENT AND THE BOUNDARY BETWEEN ARCHEAN AND PROTEROZOIC
新太古代全球克拉通事件与太古宙-元古宙分界的地质涵义
9.
<title>DISCUSSION ON PLATE TECTONICS AND?MINERALIZING PROCESS IN MIDDLE?LATE?PROTEROZOIC EON IN QINLING OROGENIC BELT?AND ITS ADJACENT AREA
秦岭造山带及邻区中晚元古宙板块构造与成矿作用初析
10.
Archean Era Greenstone Bel Gold Deposit of Ore-Hunting Evidence in Middle Part Inner Mongolia
内蒙古中部地区太古宙绿岩带金矿找矿标志
11.
THE GEOLOGICAL FEATURES OF THE LATE ACHAEAN-EARLY PROTEROZOIC IN THE EAST SECTION OF THE NORTHERN EDGE OF THE NORTH CHINA PLATFORM
华北地台北缘东段晚太古——早元古宙地质特征
12.
The Proterozoic climate was still warm and wet, but compared with that of the Archaeozoic Eon, the temperature fell a little.
元古宙的气候仍是温暖而潮湿的,但较太古宙温度有所降低。
13.
TECTONIC UNITS OF THE ARCHEAN CRYSTALLINE BASEMENT IN EASTERN HEBEI
冀东太古宙结晶基底区构造单元划分
14.
TECTONIC INVIRONMENT AND LITHOSPHERE STRUCTURE IN THE EARLY PROTEROZOIC IN EAST LIAONING
辽东早元古宙构造环境及岩石圈结构
15.
Geochemical constraints on the tectonic setting of the Proterozoic turbidites in the Xuefeng Uplift region of the Jiangnan orogenic belt
江南造山带雪峰隆起区元古宙浊积岩沉积构造背景的地球化学制约
16.
These folds are characteristic of a-type fold which are commonly found in ductile shear zones.
这些褶皱的特征表明它们属于a型褶皱，而a型褶皱通常发育在韧性剪切带中。
17.
LOWER PALEOZOIC OMISSION ZONE IN JIANGNAN UPLIFT──A SIGN OF CALEDONIAN FORELAND FOLD THRUST BELT
江南隆起上的下古生界缺失带──华南加里东前陆褶冲带的标志
18.
orthotectonic Caledonides
标准构造型加里东褶皱带