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锡矿山组
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  “锡矿山组”译为未确定词的双语例句
     SOME OSTRACODS OF THE UPPER MEMBER OF XIKUANGSHAN GROUP OF UPPER DEVONIAN IN CENTRAL HUNAN
     湘中上泥盆统锡矿山组上段介形类化石
短句来源
     The Xihuangshan formation of the late Devonian includes four stages of small cycles of regressive type.
     泥盆纪晚期锡矿山组包括四期海退式小旋回。
短句来源
     The Oujiachong Member of the Xikuangshan Group, which consists of conti-nental sediments intercalating with marine beds, is overlain by the Tournaician Sh-aodong Group and underlain by Famennian Magunao limestone bed of the Xikuang-shan Group.
     锡矿山组上段(欧家冲段),由陆相沉积和海相夹层所组成,上覆地层为杜内阶邵东段,下伏地层为法门阶锡矿山组下段(马牯脑灰岩段)。
短句来源
     The writer has obtained a lot of ostracoda fossils from the Oujiachon Member of the Xikuangshan Group in the Shaodong region of central Hunan andg carried out a detailed study on them.
     笔者在邵东县锡矿山组上段采到大量的介形类化石并进行了详细研究。
短句来源
     In eastern Hunan, the Chaling type iron deposits, located in Xikuangshan Formation of Devonian, assuming stratiform and bedded shape, with mediumto strong magnetism, can give rise to small amplitude low gradient magnetic anomalies of obvious regularity, showing banded distribution.
     在湘东地区,赋存于泥盆系锡矿山组中的茶陵式铁矿,呈层状,似层状,受层位控制,具中等至强磁性,能引起规律性明显的低缓磁异常,并呈带状分布。
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     Group B: SD to Wistar rat heart tarnsplantation;
     B
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     The SV and CO of the treatment group B increased in 5 minutes, which wa
     B
短句来源
     SOME OSTRACODS OF THE UPPER MEMBER OF XIKUANGSHAN GROUP OF UPPER DEVONIAN IN CENTRAL HUNAN
     湘中上泥盆统锡矿山上段介形类化石
短句来源
     The Xihuangshan formation of the late Devonian includes four stages of small cycles of regressive type.
     泥盆纪晚期锡矿山包括四期海退式小旋回。
短句来源
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The Devonian system is completely developed in the southern Hunan, the sed-imentation is continuous and shows the subaerial sea sedimentation characteristics. In the Simaqiao Devonian system studied by the author also occurs the famous reef controlled Houjianqiao lead-zinc-siderite-manganese ore deoosits. The sedimentation facies of the Tiaomajian formation of the early and middle Devonian stage of the western flank of syncline is the continental-littoral fa-cies, The Qiziqiao formation of the middle Devonian...

The Devonian system is completely developed in the southern Hunan, the sed-imentation is continuous and shows the subaerial sea sedimentation characteristics. In the Simaqiao Devonian system studied by the author also occurs the famous reef controlled Houjianqiao lead-zinc-siderite-manganese ore deoosits. The sedimentation facies of the Tiaomajian formation of the early and middle Devonian stage of the western flank of syncline is the continental-littoral fa-cies, The Qiziqiao formation of the middle Devonian is the beach-shoreside mar- ine basin subfacies of littoral facies. The lower part of the Shetianqiao formation of the late Devonian is a relatively large transgression stage, the type of faceis of which is the same as the Qiziquao formation, but the depth of the sea water gradually increased and with the occurrence of oxygen deficient condition. There-after, there, again, occurred the biohermal microfacies of platform limited neritic subfacies. The central part, being the slow regression stage, is characterized by the occurrence of the biotic beach microfacies and lagoon microfacies of platform limited neritic subfacies; the ore-bearing horizon occurs in the lower section of the part. The upper part is a relatively large continuous regression stage with the occurrence of oolite and oncoids beachs. The Xihuangshan formation of the late Devonian includes four stages of small cycles of regressive type.

湘南地区泥盆系发育齐全,沉积连续,并具陆表海的沉积特征。本文研究的四马桥向斜上泥盆统中,还产有著名的后江桥铅锌菱铁锰礁控矿床。向斜西翼泥盆纪早期及中期跳马涧组沉积相为陆相一滨海相。中期棋梓桥组为滨海相海滩一滨岸海盆亚相。泥盆纪晚期佘田桥组下部为较大的海侵阶段,属相虽与棋梓桥组相同,但海水逐渐加深,并形成缺氧环境,随后又出现台地局限浅海亚相生物礁微相;中部为缓慢海退阶段,出现台地局限浅海亚相生物滩微相、泻湖微相,含矿层位于下段;上部为较大的持续海退阶段,出现鲕粒滩及核形石滩。泥盆纪晚期锡矿山组包括四期海退式小旋回。

The Oujiachong Member of the Xikuangshan Group, which consists of conti-nental sediments intercalating with marine beds, is overlain by the Tournaician Sh-aodong Group and underlain by Famennian Magunao limestone bed of the Xikuang-shan Group. The writer has obtained a lot of ostracoda fossils from the Oujiachon Member of the Xikuangshan Group in the Shaodong region of central Hunan andg carried out a detailed study on them. The ostracods of the Oujiachong Member include 6 genus; 7 species and 3 sp. indet.(6...

The Oujiachong Member of the Xikuangshan Group, which consists of conti-nental sediments intercalating with marine beds, is overlain by the Tournaician Sh-aodong Group and underlain by Famennian Magunao limestone bed of the Xikuang-shan Group. The writer has obtained a lot of ostracoda fossils from the Oujiachon Member of the Xikuangshan Group in the Shaodong region of central Hunan andg carried out a detailed study on them. The ostracods of the Oujiachong Member include 6 genus; 7 species and 3 sp. indet.(6 new species). Among them, the Cavellina is very abundant and the size of the shell of Baschkirina opima is small. They lived in the lagoon of fresh water. The collection described in the pre-sent paper includes the following species: Cavellina sublatiovata sp. nov., C. sticta sp. nov., C. postcosta sp. nov., Baschkirina opima sp. nov., B. brevis sp. nov., Kloedenia pulchra sp. nov. The species of Cavellina subla-tiovata, C. sticta, C. postcosta may correspond to Cavellina latiovata of Xie-jingsi Group of the upper Devonian from the western Hubei Province, Most of the ostracods belong to Devonian and a few of them belong to the Shaodong Group of Tournaician. The writer suggests that the Ostracods of the Oujiachong Member indicate an age of late Famennian of late Devonian.

锡矿山组上段(欧家冲段),由陆相沉积和海相夹层所组成,上覆地层为杜内阶邵东段,下伏地层为法门阶锡矿山组下段(马牯脑灰岩段)。笔者在邵东县锡矿山组上段采到大量的介形类化石并进行了详细研究。这些介形类包括6属、7种(6新种)和3个未定种,其中卡咪尔介十分丰富和壳体较小的丰满巴什基利亚介,它们生活在淡化泻湖里。本文描述的标本包括下列六个新种:近宽卵形卡咪尔介、斑点卡咪尔阶、后脊卡咪尔介、丰满巴什基利亚介、短巴什基利亚介、美丽克罗登介。前三种和中国湖北西部上泥盆统写经寺组宽卵形卡咪尔介对比,多数介形类属于泥盆系,少数属于杜内阶邵东段。笔者认为锡矿山组上段介形类属晚泥盆世法门期晚时。

This paper introduces a large quantity of solitary rugose corals and a small quantity of brachiopods collected from the strata assigned originally to the Fanxia Mumber of the late Late Devonian Xikuangshan Formation at the secti- on of Wusheshan,Yougxin County,Jiangxi.It has been confirmed that there exists the early F arly Carboniferous Ceriphyllum elegantum assemblage zone. Besides,Cystophrentis,brachiopods and fossil plants were discovered in Shang- shuling,Pingxaing.This indicates that the Mengkongao Formation...

This paper introduces a large quantity of solitary rugose corals and a small quantity of brachiopods collected from the strata assigned originally to the Fanxia Mumber of the late Late Devonian Xikuangshan Formation at the secti- on of Wusheshan,Yougxin County,Jiangxi.It has been confirmed that there exists the early F arly Carboniferous Ceriphyllum elegantum assemblage zone. Besides,Cystophrentis,brachiopods and fossil plants were discovered in Shang- shuling,Pingxaing.This indicates that the Mengkongao Formation is laso not absent.Therefore,the contact between the Devonian and the Carboniferous should be conformable in western Jiangxi and the Liugiang movement did not- exist.The age of the Ningxiang-type iron deposit occurring in the Fanxia Formation should be early Early Carboniferous.Its stratigraphichorizon rjses gradually from west to east.

作者在江西省永新县乌石山剖面中,原划归晚泥盆世的锡矿山组“翻下段”内,采获大量单体四射珊瑚化石,证明有相当早石炭世早期邵东组 Ceriphyllumelegantum 组合带的存在。此外,在萍乡上株岭还发现了 Cystophretis 及腕足类、植物等化石,这表明孟公坳组也未缺失。因此,可以肯定赣西地区泥盆—石炭系应为整合过渡关系,柳江运动并不存在。同时,产于翻下组的“宁乡式铁矿”亦应属于早石炭世早期,其层位有自西向东逐渐升高的变化特点。

 
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