1.
TECTONIC EVOLUTION OF THE LATE ARCHEAN WUTAISHAN COLLISION OROGEN
五台山晚太古代碰撞造山带构造演化
2.
THE FEATURES OF LATE ARCHEAN METAMORPHIC COMPLEX IN THE MOUNT LANGSHAN AREA,INNER MONGOLIA
内蒙古狼山地区晚太古代变质杂岩特征探讨
3.
The early Proterozoic atmosphere and hydrosphere are similar to those of Archaeozoic in being still absent in oxygen.
早元古代的大气圈、水圈与晚太古代相似,仍为缺氧性质。
4.
METAMORPHISM EVOLUTION OF THE LATE ARCHEAN COLLISION OROGENIC BELT IN WUTAISHAN
五台山晚太古代碰撞造山带的变质作用演化
5.
Geological Characteristics of Late Archean Metamorphic Rocks in the Qiuyuan Area of Pucheng County,Fujian Province
福建浦城丘源地区晚太古代变质岩地质特征
6.
Accordingly, the subduction of the North China plate possibly initialed during the late times of the late Achaean.
这一研究表明华北块的消减作用可能始于晚太古代晚期。
7.
This type of graphite deposits were formend in the Late Archaean to Early Proterozoic.
该类矿床的成矿时代多集中在晚太古代末至早元古代初期,并且具有全球性。
8.
Rb-Sr AGE DETERMINATION ON THE LATE ARCHEAN FERROSILICEOUS ROCK SERIES IN SIJIAYING,LUANXIAN,HEBEI
河北滦县司家营晚太古代铁硅质岩系的铷-锶同位素年龄测定
9.
DIVISION AND CORRELATION OF LATE ARCHAEOZOIC?BASEMENT METAMORPHIC ROCK SERIES IN XIAOSHAN?AND XIAOQINLING REGIONS
小秦岭崤山地区晚太古代基底变质岩系划分与对比
10.
GEOLOGICAL FEATURES AND REE GEOCHEMICAL EVOIUTION OF LATE ARCHEAN“FRAMEWORK INTRUSIVE ROCKS” IN THE MOUNT TAISHAN AREA
泰山地区晚太古代“框架侵入岩”的地质特征及稀土地球化学演化
11.
Unit two belongs to late Archaean middle-low grade metamorphic rocks with the characteristics of granite -greenstone belt.
组合(2)是具花岗—绿岩带特征的晚太古代中、低级变质岩系.
12.
Tectonic Division of High Grade Metamorphic Terrain and Late Archean Tectonc Evolution in North central part of North China Craton
华北中北部高级变质岩区的构造区划及其晚太古代构造演化
13.
GEOCHEMISTRY AND PETROGENESIS OF LATE ARCHAEAN GRANITOIDS IN E.HEBEI PROVINCE, NORTH CHINA
河北山海关地区晚太古代花岗岩类的地球化学和成因
14.
GEOLOGIC FEATURES AND METAMORPHISM OFTHE LATE ARCHEOZOIC HIGH-GRADE METAMOPHIC REGIONIN THE LIUHE AREA,JILIN PROVINCE
柳河地区晚太古代高级变质区地质特征及变质作用
15.
The supracrustal sequences in the Dabie complex in northeastern Hubei belongs to a late Archean stratified metamorphic sequences.
鄂东北大别杂岩中的表壳岩系属于晚太古代层状变质岩系。
16.
The chondrite normalized REE distribution patterns show no Eu anomalies in the late Archaean intrusive rocks but show negative Eu anomalies in the early Proterozoic ones.
鲁西晚太古代的侵入岩属无铕异常型,早元古代的侵入岩为负铕异常型;
17.
Late Archaean Mafic ultramafic Rocks from the Wutaishan, Shanxi Province: a Possible Ophiolite Melange
山西省五台山晚太古代镁铁质-超镁铁质岩: 一种可能的古蛇绿混杂岩
18.
ON THE TECTONIC ENVIRONMENTS AND METAMORPHIC BELTS OF THE LATE ARCHEAN DENGFENG GROUP AND TAIHUA GROUP FROM CENTRAL HENAN,CHINA
河南中部晚太古代登封群和太华群成岩构造环境和区域变质带的讨论