1、K/Rb RATIOS IN ARCHAEAN GRANULITES IN THE EASTERN PART OF HEBEI PROVINCE
冀東太古代麻粒巖相變質(zhì)巖中的K/Rb比值

2、Archaean cell walls lack murein, and their lipids have ether links rather than ester links.
古細(xì)菌的細(xì)胞壁缺乏胞壁質(zhì)，其連接是醚連接而不是酯連接。

3、This type of graphite deposits were formend in the Late Archaean to Early Proterozoic.
魯西晚太古代的侵入巖屬無(wú)銪異常型，早元古代的侵入巖為負(fù)銪異常型；

4、ON THE MECHANISM OF MINERALIZATION IN ARCHAEAN GOLD-BEARING SHEAR ZONE
論太古宙含金剪切帶的成礦機(jī)制

5、GEOCHRONOLOGICAL STUDY OF ARCHAEAN ROCKS IN ANSHAN, LIAONING PROVINCE
鞍山地區(qū)太古代巖石同位素地質(zhì)年代學(xué)研究

6、Archaean granulite belts are just the product of plate-tectonic movement of rigid Archaean crust.
太古宙麻粒巖帶就是太古畝地殼發(fā)生剛性板塊運(yùn)動(dòng)的直接產(chǎn)物。

7、Sanukite of late Archaean and early Earth evolution.
晚太古代Sanukite(贊岐巖)與地球早期演化

8、ARCHAEAN GRANULITE AND SUBDIVISION OF LOWER CRUST IN EASTERN HEBEI, CHINA
冀東太古宙麻粒巖及下地殼分層的討論

9、ON THE ORIGIN AND DEVELOPMENT OF EARTH FROM THE ARCHAEAN GNEISSES
從太古代片麻巖系推測(cè)地球的成因和發(fā)展

10、ARCHAEAN GREENSTONE BELT ON THE ALASHAN BLOCK
阿拉善斷塊的太古代綠巖帶

11、The Jiapigou gold deposit lies in the lower part of the late Archaean greenstone belt.
夾皮溝金礦產(chǎn)于晚太古宙綠巖帶的下部層位。

12、pH-EVOLUTlON OF ARCHAEAN SEAWATER AND ITS RELATIONS TO ORE DEPOSITION
太古代海水pH值的演化及其和成礦作用的關(guān)系