1)Late Paleozoic晚古生代
1.Late Paleozoic sedimentary systems and gas potential in the south Ordos Basin;鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力
2.Geochemistry of Rare Earth Elements in Late Paleozoic Coals in the North China;华北晚古生代煤的稀土元素地球化学特征
3.Geochemistry of Late Paleozoic epimetamorphic rocks in Jixi of Heilongjiang and its structural setting;黑龙江鸡西地区晚古生代浅变质岩地球化学特征及构造环境
英文短句/例句
1.LATE PALAEOZOIC ERA COAL FORMING ENVIRONMENTS′ EVOLUTION IN THE ZIBO AREA,SHANDONG PROVINCE山东淄博地区晚古生代成煤环境演替
2.EVOLUTION OF THE SEDIMENTATION AND TECTONICS OF LATE PALEOZOIC DANCHI BASIN丹池晚古生代盆地的沉积和构造演化
3.After later Palaeozoic, this area was transformed into a paraplatform from" southeast Caledonian miogeo- syncline" by later Caledonian movement.晚古生代始,转化为后加里东准地台。
4.The Study of Tectonic Evolution of Late Paleozoic Strata in the East of Inner Mongolia;内蒙古东部地区晚古生代地层构造演化研究
5.Study of the Transgressive Event Deposition and Paleogeography Characteristics of Noepaleozoic in North China Area华北晚古生代海侵事件沉积及古地理特征研究
6.Paleomagnetic Results of Late Paleozoic Rocks from QT Basin in Qinghai-Tibet Plateau青藏高原羌塘地块晚古生代古地磁研究
7.GEOLOGICAL CHARACTERISTICS OF EAST KUNLUN AND TECTONIC EVOLUTION IN LATE PALAEZOIC-MESOZOIC ERA东昆仑地质特征及晚古生代——中生代构造演化
8.The Late Paleozoic-early Mesozoic Tectonic Frame in the Western Kunlun-Karakorum Area;西昆仑—喀喇昆仑晚古生代—早中生代构造格局
9.Orggenic Processes of the Inner Mongolia-Yanshan Area in Eastern China during the Late Late Paleozoic-Mesozoic;中国东部内蒙—燕山地区晚古生代晚期—中生代的造山作用过程
10.The Late Palaeozoic and Early Triassic Depositional System and Lithofacies Paleogeographic Recovery in Luoyang-Yichuan in the West of Henan Province;豫西洛阳—伊川地区晚古生代、早中生代沉积体系与岩相古地理恢复
11.On Ore-controlling of Contemporaneou fault of the Late Paleozoic Rifts in Xinjiang新疆晚古生代裂谷中同生断裂的控矿问题
12.South Tianshan: a Late Paleozoic or a Triassic orogen?南天山:晚古生代还是三叠纪碰撞造山带?
13.heavy-bodied reptile with a dorsal sail or crest; of the late Paleozoic.有背鳍和头冠、体重的爬行动物；产于晚古生代。
14.DEFORMATION OF OPHIOLITIC MELANGE OF LATE PALAEOZOIC IN NORTH TIANSHAN OF XINJIANG新疆北天山晚古生代蛇绿混杂岩带的变形研究
15.Sedimentary Tectonic Evolution from Late Palaeozoic to Triassic in the South of North China Block华北地块南部晚古生代至三叠纪沉积构造演化
16.TYPES OF LATE PALEOZOIC SEDIMENTARY BASINS AND THEIR SEDIMENTARY CHARACTERISTICS IN NORTHERN XINJIANG新疆北部晚古生代沉积盆地类型及其沉积特征
17.THE LATITUDE 38 N.TECTONIC BELT AND ITS CONTROLLING FUNCTION TO THE LATE PALAEOZOIC COAL MEASURES38°构造带及其对晚古生代煤系的控制作用
18.Sedimentation and Metallization of the Late Paleozoic Fore-arc Basin in the Western Qinling Orogenic Belt;西秦岭晚古生代弧前盆地沉积与成矿作用
相关短句/例句
Late Palaeozoic晚古生代
1.The palaeokarstification in the Late Palaeozoic Youjiang Basin, southwestern China;晚古生代右江盆地古岩溶作用研究
2.The discovery and implications of the Nalong Late Palaeozoic rift basin in Damxung, Xizang;西藏当雄纳龙晚古生代裂谷盆地的识别及其意义
3.Sedimentary Tectonic Evolution from Late Palaeozoic to Triassic in the South of North China Block;华北地块南部晚古生代至三叠纪沉积构造演化
3)Late Palaeozoic Era晚古生代
4)Neopaleozoic[,ni:?u,peili?'z?uik]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。
5)late Paleozoic Era晚古生代
1.The paper has summarized systematically evolutionary law in time and space on petrofacies and paleogeography of Late Paleozoic era in Northern China and distributive law of depositional systems.根据华北晚古生代沉积岩系的环境标志,识别出29个相,归并为冲积扇、河流、三角洲、潮汐砂滩、碳酸盐台地等6个沉积体系。
6)the end of late Paleozoic晚古生代晚期
延伸阅读
晚古生代晚古生代（距今约4.09亿年～距今2.5亿年）LatePaleozoicEra古生代两个分期的晚期。这一时期形成的地层称上古生界。晚古生代分为泥盆纪、石炭纪和二叠纪。晚古生代随着陆地面积的扩大，地理环境的变迁，给生物发展带来了新的变化。植物和脊椎动物迅速由水生向陆生发展，形成晚古生代陆生动、植物大发展的新局面。陆地出现了裸蕨植物群。孢子植物繁盛，并在二叠纪晚期出现了裸子植物。晚古生代是陆生脊椎动物发展的时期。在地史上曾将晚古生代称为鱼类和两栖类时代。海生无脊椎动物中出现了菊石、有孔虫和竹节石。曾发生过两次生物集群灭绝：①晚泥盆世弗拉斯阶和法门阶之间的生物量的突然变化以及生态系的更替。②二叠纪末期的、四射珊瑚、床板珊瑚、三叶虫以及腕足动物的大部分科属绝灭，成为划分古生代与中生代的标志。晚古生代，全球岩石圈各板块继续运动，由于北半球各板块间的碰撞、拼合，并与冈瓦纳大陆相接，到二叠纪末形成了联合古陆。晚古生代中、后期在南半球冰川广布。著名矿产有与生物礁伴生的石油、天然气，与蒸发岩伴生的钾盐。陆生植物的繁盛，造成地史上大规模煤和油页岩的堆积。
