2) the Middle Paleozoic
中古生代的
3) ancient mode of production
古代的生产方式
4) Early Paleozoic
早古生代
1.
Early Paleozoic palaeogeomorphology—characteristics of slope break zones and their control on stratigraphic-lithologic traps in Tarim Basin;
塔里木盆地早古生代古地貌——坡折带特征及对地层岩性圈闭的控制
2.
Chemical mobility of selenium in early paleozoic rock and stone coal in Daba Mountain, South Qinling;
大巴山区早古生代地层和石煤中硒的化学活动性的初步研究
3.
Discovery of Early Paleozoic granites in the eastern Xiao Hinggan Mountains, northeastern China and their tectonic significance;
小兴安岭东部早古生代花岗岩的发现及其构造意义
5) Paleozoic
[英][,peiliə'zəuik] [美][,pelɪə'zoɪk]
古生代
1.
Review and revelation of oil/gas discoveries in the Paleozoic marine strata of China;
中国古生代海相油气田发现的回顾与启示
2.
Re-discussion on exploration potential of Paleozoic in Tarim basin: 20 thanniversary of significant discovery in Shacan 2 well;
再论塔里木盆地古生代油气勘探潜力——纪念沙参2井油气重大突破20周年
3.
Metallogenic regularity of Qinling-Qilian-Kunlun metallogenic domain in Paleozoic;
秦祁昆成矿域古生代区域成矿规律
6) Neopaleozoic
[,ni:əu,peiliə'zəuik]
晚古生代
1.
Remote Sensing Interpretation and Characteristics of Basin-controlling Faults of Neopaleozoic Oil and Gas-bearing Basin in Middle Part of Guangxi;
桂中晚古生代含油气盆地控盆断裂特征及遥感解译
2.
The source rock, flow-conducting system and trap of the Eopaleozoic and Neopaleozoic petroleum accumulation systems are isolated in Tazhong area, in which the petroleum of Eopaleozoic comes from single source, whereas that of Neopaleozoic from multiple sources, shaping three-body systems, respec.
塔中早古生代和晚古生代成藏体系的烃源岩、输导体系和圈闭均为分离状,都属于三位成藏体系,但前者的油气来源单一(单源),后者的油气来源多样(多源),故两者分别被称之为塔中早古生代单源三位成藏体系和塔中晚古生代多源三位成藏体系。
3.
Kalamaili suture zone is an important plate boundary in north Xinjiang,and there are plenty of Neopaleozoic volcanic rocks around it.
卡拉麦里缝合带是北疆的一条重要界线,沿该带广泛发育晚古生代火山岩。
补充资料：古生代
| 古生代(距今5.70亿年～距今2.50亿年） Palaeozoic Era 显生宙第一个代。显生宙包括古生代、中生代和新生代。古生代分为早古生代和晚古生代，早古生代包括寒武纪、奥陶纪和志留纪；晚古生代包括泥盆纪、石炭纪和二叠纪。也有将古生代三分为早、中、晚古生代。古生代时形成的地层称古生界，位于前寒武系之上、中生界之下。 古生代意为古老生物的时代。生物界从原始生命的形成，经历了前寒武纪漫长时期的演化，古生代时已发展到一个新阶段。从寒武纪开始发生了广泛的海侵，是海生无脊椎动物为主的时代。志留纪时陆生植物开始发展。晚古生代孢子植物大量繁盛。晚二叠世时，裸子植物代替孢子植物占居重要地位。原始脊椎动物的无颚类出现于寒武纪晚期。鱼类在泥盆纪达到全盛。石炭纪、二叠纪两栖类大量繁盛。 |
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参考词条