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扬子型
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  yangtze type
     ON THE YANGTZE TYPE COPPER ORE DEPOSITS AND ITS ORIGIN
     论扬子型铜矿床及其成因
短句来源
     THE REE GEOCHEMISTRY OF MINERALS IN YANGTZE TYPE COPPER DEPOSITS,EASTERN CHINA
     扬子型铜矿床矿物稀土元素地球化学
短句来源
     2 ) the strata conformably underlying the flysch are all characterized by lithofacies and fossils of the Yangtze type;
     (2)岩相及古生物特征表明,与复理石整合接触的下伏地层为扬子型;
短句来源
     2.From north to south, the Carboniferous sea facies layers are gradually deve- loped, the rock association of Benxi Formation and Taiyuan Formation is more similar to that of Yangtze type and has the relationship of continuous transition with Yangtzetype Carboniferous in Binhai County, northern Jiangsu Province;
     2.石炭系海相层自北而南逐渐发育,本溪组、太原组的岩石组合特征逐渐接近扬子型,并与苏北滨海县扬子型石炭系呈现连续过渡;
短句来源
     The discovery of the Yangtze type Neoarchean metamorphic basement to the west side of the fault zone and the coincidence of the Yenshanian intermediate acid intrusive isotope geochemical characteristics for both sides of it suggested that the Huanglishu-Miaoji Fault Zone is not the boundary between the Dabie orogen and the Yangtze landmass.
     断裂带西侧“扬子型”新太古代变质基底的发现及断裂带两侧燕山期中酸性岩体同位素地球化学特征的一致性,证明它不是大别造山带与扬子地块的界线。
短句来源
  “扬子型”译为未确定词的双语例句
     Jiangsu lower Yangtze area is in the southeast of Huaiyin-Xiangshui and Tanlu fracture, and the area have sea facies aggradation distributing in middle and south of Jiangsu Province.
     江苏下扬子区位于淮阴—响水断裂、郯庐断裂东南,指具有扬子型海相沉积分布的江苏省中南部地区。
短句来源
     Based on the observations of the Cambrian at three locations and abundant fossils collected, this paper proposes a biogeographical division of the Middle and the Late Cambrian in western Guangxi, the similarity between the trilobite assemblage at the Poben section in Napo county and that from Dayangcha, Henjiang, Jilin Province, the similarity between the fauna of the Poben and Shechang areas and those of the North China - Yangzi type, and proposes that the fauna from Goluo is a transitional type.
     本文根据观察桂西三处寒武系分布区并采到较多的三叶虫化石资料,提出该地区中、晚寒武世生物地理分区,那坡县坡笨剖面三叶虫组合与吉林浑江大阳岔区非常相似,坡笨和蛇场地区的动物群可与华北—扬子型动物群对比,果乐地区为过渡型动物群。
短句来源
     From north to south in the eastern NCP, the Carboniferous clastic ratio decreases, layer numbers and thickness of sea-facies limestone increase, and the sedimentary facies is more similar to Yangtze-tyPe one.
     在华北地块东部,碎屑岩比自北而南递减,海相灰岩层数和厚度递增,越向南越呈现扬子型沉积特点。
短句来源
     A linear Lower Paleozoic omission zone is exposed to the Jiangnan uplift which extends along the strike of the uplift,separates the Yangtz-type strata in north from southern Jiangnan-type strata, and is overlaped by Late Paleozoic shallow marine carbonates.
     江南隆起核部存在一下古生界缺失带,它平行隆起走向线状分布,空间上分开了西北的扬子型地层和东南的江南型地层区,晚古生代浅海碳酸盐平缓超覆其上。
短句来源
     The Yangtze Permian coal - bearing rock series (the Longtan coal series) distribute in South Anhui broadly , and can bedivided into the Chaoxian and the Susong two depositional subtypes based on the depositional features in the district.
     安徽南部广泛分布着扬子型二叠纪合媒岩系(龙潭煤系),根据该区沉积特征可划分两种沉积亚型印象即巢县亚型和宿松亚型。
短句来源
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     The author considers that there arethree subspecies of Neophocaena phocaenoides existing in the Chinese waters, thatis, N.
     亚种N.
短句来源
     ON THE YANGTZE TYPE COPPER ORE DEPOSITS AND ITS ORIGIN
     论铜矿床及其成因
短句来源
     THE REE GEOCHEMISTRY OF MINERALS IN YANGTZE TYPE COPPER DEPOSITS,EASTERN CHINA
     铜矿床矿物稀土元素地球化学
短句来源
     (2)C shape;
     C ;
短句来源
     The Subshift of Infinite Type
     无限移位
短句来源
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A flysch belt of E-W trend sedimented from late Paleozoic to early Mesozoic, outcrops in the Qinling Mountains. The following evidences support that the flysch deposited on active margin north of the Yangtze Plate; 1 ) the flysch belt is now located south to the suture zone of Yangtze and North China Plates; 2 ) the strata conformably underlying the flysch are all characterized by lithofacies and fossils of the Yangtze type; 3 ) paleocurrent data ( from N to S ) show that there was an ancient source area for...

A flysch belt of E-W trend sedimented from late Paleozoic to early Mesozoic, outcrops in the Qinling Mountains. The following evidences support that the flysch deposited on active margin north of the Yangtze Plate; 1 ) the flysch belt is now located south to the suture zone of Yangtze and North China Plates; 2 ) the strata conformably underlying the flysch are all characterized by lithofacies and fossils of the Yangtze type; 3 ) paleocurrent data ( from N to S ) show that there was an ancient source area for detritus in the north of the flysch belt, which is represented now by remnent blocks of mobilized basement; 4) pyroclastics in the flysch mean that the source area might be a series of islands related to southward plate subduc-tion. It should be noted that north inclined structures now in Qinling resulted from southward overthrust. A reasonable explanation for the phenomenon is plate flip: before T2, oceanic crust of the paleotethys north to the Yangtze Plate subducted southward, resulting in an active continental margin; after T2, while the paleotethys was entirely consumed, the North China Plate behind the oceanic crust overthrust onto the Yangtze Plate, resulting in the building up of nowadays Qinling.

秦岭发育一条近东西走向的复理石带,其沉积时限约为古生代末至中生代初。下述证据表明,这些复理石是扬子板块北侧活动大陆边缘的产物:(1)该复理石带位于华北板块与扬子板块的缝合线以南;(2)岩相及古生物特征表明,与复理石整合接触的下伏地层为扬子型;(3)由北向南的古水流资料表明,复理石带北侧曾存在提供碎屑的物源区,那里现存的一系列活化基底块体可能即为古老岛陆的残余;(4)复理石中夹有若干层火山碎屑岩,暗示了那些岛陆与向南的板块俯冲有关。需要强调的是,秦岭现今构造倒向是向南逆冲及推覆的结果。这一现象可用板块俯冲方向倒转(Plate flip)解释,即,中三叠世以前,扬子板块以北的古特提洋壳向南俯冲,形成活动大陆边缘,中三叠世以后,洋壳消减殆尽,大洋彼岸的华北板块与扬子板块对撞,并逆冲至后者之上,形成秦岭。

Taoyuan and Cili are situated on the margin of Jiangnan stratigraphical province and adjoin Yangzi stratigraphical province. The Cambrian-Ordovician boundary sequence is endowed with contineous in contact relation, wellexposed, rich in fossils. Noticeably, this graplolite fauna contains the both members of Jiangnan and Yangzi province. It is one of the best Cambrian-Ordovician boundary sections in China. The Cambrian-Ordovician boundary sequence is described and three graptolite zones are established as follows:...

Taoyuan and Cili are situated on the margin of Jiangnan stratigraphical province and adjoin Yangzi stratigraphical province. The Cambrian-Ordovician boundary sequence is endowed with contineous in contact relation, wellexposed, rich in fossils. Noticeably, this graplolite fauna contains the both members of Jiangnan and Yangzi province. It is one of the best Cambrian-Ordovician boundary sections in China. The Cambrian-Ordovician boundary sequence is described and three graptolite zones are established as follows: 1). Dictyograptus wutingshanensis zone, 2). D. flabellijormis zone, 3), Anisograptus zone. The Cambrian-Ordovician boundary sot between D. wutingshanensis zone and D. flabellifarmis zone. The nature of graptolite fauna, the correlation of the graptolite-bearing strata with that in other area and the Cambrian-Ordovician boundary arc also discussed.

桃源、慈利一带位于江南地层区边缘,与扬子地区相邻,寒武系与奥陶系界线附近的地层发育良好,沉积连续,化石丰富,生物具有扬子型和江南型之间的过渡性特征,是我国研究寒武系与奥陶系的理想地区之一。本文描记了界线附近的地层,建立了三个笔石带,自下而上为:1).Dictyograptus wutingshanensis带,2).D.flabelliformis带 ,3) .Anisograptus带。寒武系与奥陶系界线位于D.woutingshanensis带与D.flabelliformis带之间。本文还对笔石动物群的性质进行了分析,与邻区和国外相当地层进行了对比,并讨论了本区寒武系与奥陶系界线。

Taoyuan and Cili are situated on the margin of Jiangnan stratigraphical province and adjoin Yangzi stratigraphical province. The Cambrian-Ordovician boundary sequence is endowed with contineous in contact relation, wellexposed, rich in fossils. Noticeably, this graptolite fauna contains the both members of Jiangnan and Yangzi province. It is one of the best Cambrian-Ordovician boundary sections in China. The Cambrian-Ordovician boundary sequence is described and three graptolite zones are established as follows:...

Taoyuan and Cili are situated on the margin of Jiangnan stratigraphical province and adjoin Yangzi stratigraphical province. The Cambrian-Ordovician boundary sequence is endowed with contineous in contact relation, wellexposed, rich in fossils. Noticeably, this graptolite fauna contains the both members of Jiangnan and Yangzi province. It is one of the best Cambrian-Ordovician boundary sections in China. The Cambrian-Ordovician boundary sequence is described and three graptolite zones are established as follows: 1).Dictyograplus wutingshanensis zone, 2). D. flabelliformis zone, 3). Anisograptus zone. The Cambrian-Ordovician boundary set between D. wutingshanensis zone and D. flabelliformis zone. The nature of graptolite fauna, the correlation of the graptolite-bearing strata with that in other area and the Cambrian-Ordovician boundary are also discussed.

桃源、慈利一带位于江南地层区边缘,与扬子地区相邻,寒武系与奥陶系界线附近的地层发育良好,沉积连续,化石丰富,生物具有扬子型和江南型之间的过渡性特征,是我国研究寒武系与奥陶系的理想地区之一。本文描记了界线附近的地层,建立了三个笔石带,自下而上为:(1).Dictyograptus wutingshanensis带,(2).D.flabelliformis带,3).Anisograptus带。寒武系与奥陶系界线位于D.wutingshanensis带与D.flabelliformis带之间。本文还对笔石动物群的性质进行了分析,与邻区和国外相当地层进行了对比,并讨论了本区寒武系与奥陶系界线。

 
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