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- ZHU Tongxing, HUANG Zhiying , HUI Lan. The Geology of Late Permian Period Biohermal Facies in Upper Yangtze Tableland[M]. Beijing: Geological Publishing House, 1999(in Chinese). 朱同兴;黄志英;惠兰.;上扬子台地晚二叠世生物礁相地质[M]
- Late Permian period Wu Jia Ping magnesium limestone reef in the Western European Commission, represented the basin reefs, these types of simple reef, or from stromatolites bryozoans composition. 晚二叠世吴家坪期的礁以西欧镁灰岩统盆地的礁为代表,这些礁的类型简单,由叠层石或苔藓虫组成。
- Analysis on peat's reserves in later permian period of Guizhou 贵州省晚二叠世泥炭储量分析
- late Permian Period 晚二叠世
- Keywords Panji mine in Huainan;the Later Permian Period;INAA;trace elements in coal;affinity of element; 淮南潘集;晚二叠世;中子活化分析;煤中微量元素;元素亲和性;
- Late Permian a the cycads, conifers and other the show began state. 晚二叠世出现了银杏、苏铁、本内苏铁、松柏类等裸子植物,开始呈现中生代的面貌。
- Analysis of coal-accumulating regulation the longtan formation coal series of later permian period in Liyuanba Minefield, Songzao Mining area, Qianyu 黔渝地区松藻矿区梨园坝井田晚二叠世龙潭组煤系聚煤规律分析
- The intrusion of Angara plants into Tarim block took place at late permian. 晚二叠世发生了准噶尔区安加拉植物入侵塔里木区事件。 在我国北方这是一次普遍的植物事件。
- later permian period 晚二叠世
- The basin was fromed during Late Permian Epoch, its period of full bloom of expanding and depression being Early and Middle Jurassic System when incoalation envorinment was most favorable. 吐鲁番-哈密盆地形成于晚二叠世,早、中侏罗世是盆地扩张坳陷全盛时期,此期盆地成煤条件最好。
- The genesis of deposits is analyzd that "deposits were formed in peneplain lake condition in semi-humid continental climate during late period of early Permian and early period of late Permian". 简要的分析了矿床的成因,认为该矿床沈积形成于早二叠世晚期到晚二处世早期半潮湿大陆气候的准平原化湖泊环境。
- The genesis of deposits is analyzd that deposits were formed in peneplain lake condition in semi-humid continental climate during late period of early Permian and early period of late Permian. 简要的分析了矿床的成因,认为该矿床沉积形成于早二叠世晚期到晚二叠世早期半潮湿大陆气候的准平原化湖泊环境。
- At the end of the Permian period 225m years ago, between 80 % and 96 % of all living marine species were extinguished. 2.;25亿年前的二叠纪末期,当时80%25到96%25的海洋物种灭绝;
- Extinct terrestrial reptiles having teeth set in sockets,of the late Permian to Triassic. 有牙,且牙齿长于牙槽的已灭绝的陆地爬虫动物,生活于二垩纪晚期到三垩纪。
- Any of various large, segmented aquatic arthropods of the order Eurypterida that existed from the Ordovician Period to the Permian Period. (古生)板足鲎目的一种巨大的、有节的,属于板足鲎目的水生节肢动物,生存于奥陶纪到二叠纪时期
- Studying late Permian biotic events in this area will further the understanding of those events. 对此区域内二叠纪晚期生物灭绝事件的研究,有助于更全面的把握二叠纪末期生物灭绝事件在扬子区内的表现。
- At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa. 二叠纪末期,地球上的陆地合并成一块超级大洲,叫作盘古大陆,以及一个超级大海,叫作原始大洋。
- Ore deposits which have economical value mainly are depositional type and volcanegenic type produced in the permian period and tertiary period. 具经济价值的主要为产于二叠纪及第三纪沉积类及火山沉积类矿床。
- Late Permian to Triassic rifting and subsidence resulted in the deposition of as much as 9 kilometers of Triassic strata, locally injected with sills. 二叠纪晚期到三叠纪断裂和下沉作用形成了大约9千米厚的第三纪沉积地层,在其中有岩床的切入。
- The hydrothermal fluid and the spaces of ore-bodies in the deposit are provided by the granite magmas and the Permian period. 指出印支期白岗质花岗岩岩浆提供部分成矿物质,二叠系地层和花岗岩浸位提供热源和导矿、容矿空间。