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下扬子
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  lower yangtze
     Starting from Late Sinian Epoch to Middle Trassic Epoch, three sets of hydrocarbon source rock series of huge depth (Z 2-O 3,C-P,T 1) were deposited in Lower Yangtze Areas.
     从晚震旦世开始至中三叠世 ,下扬子地区沉积了三套巨厚的海相烃源岩系 (Z2 -O3 、C -P、T1)。
短句来源
     The features of neotectonism and earthquake activities in the Lower Yangtze area (118°—124°E, 29°—34°N) and their relationship have discussed. Based on these researches, the potential hypocentral areas are pointed out.
     本文探讨了下扬子地区(北纬29°—34°,东经118°—124°)的新构造运动、地震活动的特征及其两者的关系,并据此划分了区内的潜在震源区。
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     STUDY OF THE CARBONIFEROUS SEQUENCE STRATA AND EVOLUTION OF THE LOWER YANGTZE BASIN
     下扬子盆地石炭纪层序地层研究及盆地演化
短句来源
     The Carboniferous of Lower Yangtze Basin is divided into 3 evolution stages of depression,upwelling and extensional sinking ,corresponding to sequences A- B,C and D- F,respectively.
     石炭纪下扬子海盆的演化可以分为 3个阶段,即坳陷、隆起、扩展沉陷阶段,它们分别对应于层序 A- B、 C和 D- F。
短句来源
     Study on Anoxic Environments of Permian in the Middle and Lower Yangtze Region
     中下扬子地区二叠纪缺氧环境研究
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  lower yangtse
     And the sequence classification and regional correlation of Carboniferous in Lower Yangtse area are discussed. Results show that this area can be divided into 6 third,grade sequences (SQ1-SQ6),among which SQ1,SQ5,SQ6 belong to Type Ⅰ sequence; SQ2,SQ3,SQ4 to Type Ⅱ sequence.
     研究结果表明,苏皖下扬子地区石炭系可以分为6个三级层序,其中层序SQ1、SQ5、SQ6属于Ⅰ型层序,层序SQ2、SQ3、SQ4属于Ⅱ型层序。
短句来源
     In northeastern part of Lower Yangtse area,SQ1-SQ6 are completely developed; in southwestern part of it,SQ1-SQ4 are absent in different degrees;
     在苏皖下扬子的东北部地区SQ1—SQ6六个层序发育完整,而在西南部地区SQ1—SQ4四个层序存在不同程度的缺失;
短句来源
     Sequence Stratigraphy of Carboniferous in Lower Yangtse Area of Jiangsu and Anhui Provinces.
     苏皖下扬子地区石炭系层序地层学特征
短句来源
  lower yangtze valley
     New information of Caledonian tectonic features in the northern part of the southeastern margin of the Lower Yangtze valley
     下扬子东南缘北段加里东期构造形迹新资料
短句来源
     The source area of K-rich magmatic rocks in the Dabie area is closely related to the enriched mantle, while the rocks in the lower Yangtze Valley area are more affined to the lower crust.
     大别地区富K岩系的源区与富集地幔密切相关,下扬子地区的则与下地壳有更多亲缘关系。
短句来源
     The difference in magma source area is the fundamental cause for the appreciable difference in mineralization between the Dabie area and the lower Yangtze Valley area in the Yanshanian.
     岩浆源区的不同是造成大别地区和下扬子地区成矿作用重大差别的根本原因。
短句来源
     Based on an integrated analysis of the petroleum geological conditions of marine carbonate sequences in various areas of China, the paper also discusses the strategic petroleum exploration area selection in marine carbonate sequences and geological problems in need of immediate solution in the Sichuan basin, Middle and Lower Yangtze valley, Yunnan-Guizhou-Guangxi area, Tarim basin, Ordos basin, Bohai Bay basin and Qinghai-Tibet Plateau.
     在对不同地区海相碳酸盐岩层系油气地质条件进行分析解剖的基础上,分别对四川盆地、中下扬子及滇黔桂地区、塔里木盆地、鄂尔多斯盆地、渤海湾盆地和青藏地区的海相碳酸盐岩层系油气勘探战略选区急需解决的地质问题进行了讨论。
短句来源
  “下扬子”译为未确定词的双语例句
     The fifty-eight oriented specimens located at 29°30'-34°N and 115°30 - 119°15' E have been sampled on the ten sites.
     对在东经115°30′~119°15′、北纬29°30′~34°范围内的下扬子地区中生界,笔者分设10个采点采集定向标本58块。
短句来源
     COMPREHENSIVE GEOPHYSICAL SURVEY OF HQ-13 LINE IN THE LOWER YANGZI REACHES AND ITS GEOLOGICAL SIGNIFICANCE
     下扬子地区HQ-13线的综合地球物理调查及其地质意义
短句来源
     Geophysical discuss on extension to the east of boundary belt between Yangtze and Huanan Blocks
     对下扬子与华南边界结合带东延问题的地球物理探讨
短句来源
     The analysis of the electric parameters in the Northern Xiayangzi
     下扬子北部地区电性参数分析
短句来源
     The evolution of the foreland basin can be divided into 3 stages: 1)sprout and budding stage(P3-T1),during which the passive continental margin basin is formed,characterized by a set of typical deep-water to semideep-water flysch;
     下扬子北缘前陆盆地自萌芽至消亡可划分为3个演化阶段:1)萌芽阶段(P3—T1),形成被动大陆边缘盆地,发育深水—半深水复理石建造;
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  lower yangtze
Oil geologic anomaly in the north edge of the Middle and Lower Yangtze areas based on the evidence weight method
      
The decreasing trend of effective precipitation days for the middle-lower Yellow River valley and the increasing trend for the lower Yangtze River valley are most likely linked to anomalous monsoon circulation in East China.
      
The authors discussed the metallogenic conditions of gold-bearing skarn deposits along the middle-lower Yangtze River reaches.
      
Analysis of the deep tectonics and cover tectonic deformations shows that tectonic layering motion is a typical lithospheric characteristic in the Tongling area and the metallogenic belt of the middle-lower Yangtze.
      
Carbon isotope composition of the Lower Triassic marine carbonates, Lower Yangtze Region, South China
      
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  lower yangtze valley
Hydrothermal mobilization and enrichment of iron in the iron deposits of the Middle-Lower Yangtze Valley district
      
There are two main types of iron deposits in the Middle-Lower Yangtze Valley district.
      
Copper mineralization in the lower Yangtze Valley can be divided into three major types: skarn type, porphyry type and volcanic type.
      
From them, two resistant cultivars with high-yielding potential were developed and commercialized in the Lower Yangtze Valley.
      


~~

本文在綜合研究宁鎮山脈象山羣岩层縐构造形态基本特征、分布規律和形成机理的基础上,专門論述了海西印支裡縐构造的基底断裂如何控制燕山盖层褶縐形成的具体表現方式,論証了燕山运动以块断运动为主的构造性貭,为进一步研究下揚子地区岩漿活动和成矿作用的空間分布規律提供了构造方面的依据。

The Hsuehfeng cycle of the region under discussion is taken as a stage of eugeosynclinal development. The eugeosytnclinal formational sequences are rich in volcanic rocks which have been folded into tight linear folds by the Hsuehfeng movement. The Hsuehfeng folded belt is responsible for the formation of the Kiangnan geanticline of the Caledonian cycle. The South Anhui geosyncline extends along the northern side of the Kiangnan geanticline and is filled with the miogeosynclinal formational sequences which have...

The Hsuehfeng cycle of the region under discussion is taken as a stage of eugeosynclinal development. The eugeosytnclinal formational sequences are rich in volcanic rocks which have been folded into tight linear folds by the Hsuehfeng movement. The Hsuehfeng folded belt is responsible for the formation of the Kiangnan geanticline of the Caledonian cycle. The South Anhui geosyncline extends along the northern side of the Kiangnan geanticline and is filled with the miogeosynclinal formational sequences which have vast thickness of more than ten thousand meters and consist of typical geosynclinal formations (flysch formation, graywacke formation, siliceous shale formation, etc.) with zonal arrangement. The geometric styles of folding in the South Anhui geosyncline are of linear complex folds the individual fold of which is either tight or open in form, which indicates the varied origin of the folded structure. On the basis of the above mentioned structural characteristics it is to be compared with the West Chekiang Caledonian geosyncline, Through comparative research and analysis of the South Anhui, Northwest Kiangsi and West Hunan Caledonian geosynclines bondering the northern side of the Kiangnan geanticline, the present writer has found that their similarities are rather obvious. Thus they form as a whole the belt of the marginal geosynclinal depressions. The South Anhui Caledonian geosyncline could be distinguished from the South Kiangsi Caledonian inner geosyncline by the following diagnostic features: (1) it has more abundant carbonate rocks in the sedimentary sequences; (2) it possesses comparatively open style of folding; (3) the trough of sedimentation migrates from the Kiangnan geanticline towards the platform throughout the early palaeozoic period; and (4) it displays weak regional metamorphism and igneous activity. Judging from the above-stated reasons, it is less mobile and displays the character of a residual geosyncline. The Shitai-Guogongtzang deep fault marks the boundary between the South Anhui Caledonian geosyncline in the south and the Lower Yangtze Pericratonic Subsidence zone, having the carbonate formation of platform type, in the north. During the Caledonian cycle the Nantian trough is superimposed upon the eastern part of the Kiangnan geanticline and distinguished from the South Anhui geosyncline by the incompleteuess of the sedimentary cycle, its paramolasse formation and the basin-shaped syncline. The Kiangnan geanticline broadly controls the formational and structural development of the South Anhui geosyncline and the West Chekiang geosyncline on both sides. Thus the South Anhui geosyncline together with the West Chekiang geosyncline and the Kiangnan geanticline constitutes a geosynclinal system which forms the northeastern section of the South China Caledonian geosynclinal region.

皖南南部构造性质及构造单元的归属的争论,在最近一次全国性编图会议,意见仍未统一。作者在实际调查材料的基础上,运用构造——建造分析和比较大地构造的方法研究了本区前寒武纪及早期古生代各时代建造成分,确定了各建造的名称、性质和空间分布特征,进一步划分出几个不同性质的建造序列;描述了不同时代地层和不同空间的构造形态,划分了构造层及构造形态的级别,並分析了构造形态形成的原因;论证了本区加里东运动的存在及其性质。在上述资料基础上,阐明了本区是华南加里东地槽区皖南浙西加里东地槽系的重要组成部分,並对皖南加里东地槽与其北隣的下扬子台缘沉陷带的界限予以确定,进一步说明了本区在加里东旋迴是冒地槽,具有残余地槽和边缘地槽拗陷的特性。

The profile of the Qing-Long Group(Middle-Lower Triassic) at the Shanjuan caverns, Yixing, Jiangsu, in which the features of petrography and the marks of lithofacies in every member are clear and obvious. is an ideal one in the eastern Lower Yangtze region. These limestones principally appear to be the facies of banks, tidal flats and tidal channels. It suggests that this region is located at the northeastern Jiangnan Rise that submerged in water at that time.

江苏省宜兴县善卷洞附近的青龙灰岩(中、下三迭统)出露完整,其中各岩性段岩性特征明显,是下扬子东部地区的较好剖面。本剖面的岩层主要反映潮坪、浅滩和通道相。当时,这一地区处于江南隆起的北东水下延伸带上。

 
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