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   三缝孢子 的翻译结果: 查询用时:0.148秒
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三缝孢子
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  “三缝孢子”译为未确定词的双语例句
     In the 8th Team of Bangqi Farm,the sporopollen assemblage dominated by triletes was first analysed from the sericite—phyllite which was originally thought to be the Bed 2 of the Lower Carboniferous Junying Group.
     在邦溪农场八队绢云母千枚岩中,第一次分析出以三缝孢子占优势的孢粉组合。
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     The late Early Carboniferous miospore assemblage is dominated by trilete spores, with abundant lepidophyte microspores of the genus Lycospora.
     早石炭世晚期孢粉组合中三缝孢子占优势,并以鳞木植物的小孢子Lycospora含量很高为特征。
短句来源
     The Late Carboniferous assemblage is principally predominated by trilete spores, with Lycospora accounting for up to 33.4% of the abundance.
     晚石炭世孢粉组合中三缝孢子占有绝对的优势,鳞木植物的小孢子Lycospora的含量最高(占总含量的33.4%)。
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     EXPLANATION OF"JIAO ZI
     “交”释义
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     Fuzzy Submatroids
     模糊拟阵
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     In the 8th Team of Bangqi Farm,the sporopollen assemblage dominated by triletes was first analysed from the sericite—phyllite which was originally thought to be the Bed 2 of the Lower Carboniferous Junying Group.
     在邦溪农场八队绢云母千枚岩中,第一次分析出以三缝孢占优势的孢粉组合。
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The Late Palaeozoic Erathem of the Daling area of Hainan Island was regarded to be the Lower Carboniferous Junying Group by the 4th Branch of the Hainan Geolgical Team in 1978.The authors found first Agathiceras cf. vulgatum Ruzhancev, Altudoceras sp., in the phyllite that lies on the 3rd member of the Yangguang Stage in the Daling Farm section from the 14th team to 12th team. Altudoceras is common in the Early Permian in South China. Neogondolella? sp.ranging in age from Permian to Triassic,was...

The Late Palaeozoic Erathem of the Daling area of Hainan Island was regarded to be the Lower Carboniferous Junying Group by the 4th Branch of the Hainan Geolgical Team in 1978.The authors found first Agathiceras cf. vulgatum Ruzhancev, Altudoceras sp., in the phyllite that lies on the 3rd member of the Yangguang Stage in the Daling Farm section from the 14th team to 12th team. Altudoceras is common in the Early Permian in South China. Neogondolella? sp.ranging in age from Permian to Triassic,was found from the Hechaling section that was originally considered to be the limestone of the Bed 4 in the upper part of the Predevonian.In the 8th Team of Bangqi Farm,the sporopollen assemblage dominated by triletes was first analysed from the sericite—phyllite which was originally thought to be the Bed 2 of the Lower Carboniferous Junying Group.The main members of the assemblage have been found in the coal measures of Early Permian age in Shaodong,Shaoshan of Hunan, Changxing of Zhejiang,Pingdingshan of Henan and other places especially, Densosporites sp.which was only found in the Early Permian Qianyang coal measures in Qingfeng of Hunan.The authors think that the Permian System was the first discovery,in addition to Lower Carboniferous Yangguang Stage,in the Late Palaeozoic of the Daling area.Ammonitides,conodonts and sporopollen assemblage are all common in Permian rocks in South Chian.The Permian of the Daling area is divided into Echa,Eding and Nanlong Formations,which have a correlation with the Permian of the Western Hainan Island.The dicovery of ammonoides in the Permian rocks over the Yangguang Stage proved that the Permian in this area lies on the Yangguang Stage.

测制大岭农场14—12队剖面时,在覆于相当昌江鸡实含Pseudouralinia带岩关阶地层之上的千枚岩中,首次发现菊石Altudocerassp.、Agathicerascf.vulgatum;河叉岭剖面首次发现牙形刺Neogondolela?sp.;在邦溪农场八队绢云母千枚岩中,第一次分析出以三缝孢子占优势的孢粉组合。据此,笔者认为大岭地区的晚古生代地层,除有下石炭统岩关阶地层外,还有二叠纪地层,并可与邻区二叠纪地层对比,并探讨了该区二叠纪岩相古地理。

Based on the analysis of 123 palynological samples from 11 test wells in the Awati-Bachu area of the Tarim Basin, three miospore assemblages of the Carboniferous age have been recognized, providing important palaeontological data for the biostratigraphical subdivision and correlation in this area. The early Early Carboniferous miospore assemblage is composed entirely of spores, dominated by those of Lycopsida dominated (up to 80%) with subordinate archaeopteridophyte and calamophyte spores. The late Early Carboniferous...

Based on the analysis of 123 palynological samples from 11 test wells in the Awati-Bachu area of the Tarim Basin, three miospore assemblages of the Carboniferous age have been recognized, providing important palaeontological data for the biostratigraphical subdivision and correlation in this area. The early Early Carboniferous miospore assemblage is composed entirely of spores, dominated by those of Lycopsida dominated (up to 80%) with subordinate archaeopteridophyte and calamophyte spores. The late Early Carboniferous miospore assemblage is dominated by trilete spores, with abundant lepidophyte microspores of the genus Lycospora. The Late Carboniferous assemblage is principally predominated by trilete spores, with Lycospora accounting for up to 33.4% of the abundance.

通过对新疆塔里木盆地阿瓦提—巴楚地区11口探井123块石炭系孢粉样品的鉴定结果系统分析,建立了该区Rugosporaminuta-Verrucosisporitessimilis、Lycosporapusilla-Verrucosisporitesmicrotubercosus和Calamosporaliquida-Schopfipollenitesellipsoids孢粉组合3个,从而为该区石炭纪地层的划分对比提供了依据。该区早石炭世早期孢粉组合中石松植物的孢子占优势(约占总含量的80%),古蕨类植物和芦木植物的孢子含量次之,在个别样品中出现少量疑源类和虫颚化石。早石炭世晚期孢粉组合中三缝孢子占优势,并以鳞木植物的小孢子Lycospora含量很高为特征。晚石炭世孢粉组合中三缝孢子占有绝对的优势,鳞木植物的小孢子Lycospora的含量最高(占总含量的33.4%)。

 
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