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红色盆地
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  red basin
     STRUCTURAL LITHOLOGICAL LITHOFACIES MAPPING METHOD—A New Method for 1∶50,000 Geological Mapping of the Terrestrial Red Basin
     陆相红色盆地1∶5万填图的一种新方法———构造—岩性—岩相填图法
短句来源
     Quantification Sedimentology Features and Evolution in East North segment of Chang Ping Continetal Deposit Red Basin
     长——平陆相红色盆地北东段量化沉积学特征及其演化
短句来源
     Mesozoic strata in the red basin of the Hainan Island
     海南岛中生代红色盆地地层
短句来源
     THE FUNDAMENTALPRINCIPLE AND METHOD FOR DEFININGTHE PROLUVIAL FANS IN ASMALL RED BASIN ACCORDING TO THE STATISTICS OF GRAVELS
     根据砾石统计确定红色盆地中洪积扇体的基本原理与方法
短句来源
     The placer diamond deposits in Yuanjiang River are found in the wide valley in the middle, lower reach of Yuanjiang River, where the river flows through the red basin of Mesozoic and Cenozoic era, 98% of the diamonds are found in individual crystal form with an average weight of 10.4mg, the maximal one reaches 8.46g.
     沅江的金刚石砂矿分布在沅江中、下游流经中新生代红色盆地的宽谷中,金刚石98%为单晶,平均重10.4mg,最大者达8.64g,晶形主要为十二面体,多数表面带黄色,而内部为无色透明,白度达85以上。
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  red basins
     The red beds in Guangdong are distributed in 108 Cretaceous-Tertiary red basins,covering a total area of 28283 km~(2),accounting for some 16% of the total land areas of the province. The distribution of those red beds is affected by the factors of geologic structure,lithology,climate,and time,etc. Danxia landform is widely distributed in Guangdong.
     在一定的地质构造、岩性特征和气候与时间等因素的作用下,广东的红层都分布在白垩-第三纪的红色盆地中,在全省108个红层盆地中,各盆地红层的总面积为28 283 km2,约占全省陆地面积的16%。
短句来源
     The Strata in Red Basins of the Eastern Part of Qinling Mountains
     秦岭东段红色盆地地层
短句来源
     Basin-margin types and basin-fill types of Cretaceous-Neogeneterrestrial red basins in Jiangxi
     江西白垩纪—新近纪陆相红色盆地的盆缘类型划分与盆地充填样式
短句来源
     Through1∶50000regional geological mapping of terrestrial red basins in Jiangxi ,a classification scheme of two types and eight sorts of terrestrial lithostratigraphic sequence boundaries has been worked out.
     根据江西境内陆相红色盆地1∶5万区调填图实践,拟定了陆相岩石地层序列界面2类8种的划分方案;
短句来源
     Neotectonic movement analysis can satisfactorily explain:the distribution pattern of red basins,different leaching degree of purple soil in the red basins,the formation of high peak of Wuliang mountain,influences of Kunnming Epsilon(∈)Type Structure on the soil development,distribution of lateritic soil and dry red soil etc.
     新构造运动观点可圆满解释:红色盆地的分布状况、红色盆地内紫色土的淋溶程度差异、无量山主峰的形成,昆明山字型构造对土壤发育的影响、砖红壤与燥红土等土壤的形成规律等等.
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  “红色盆地”译为未确定词的双语例句
     Study on sedimentary deposits in the red continental basin of Jian-Taihe, Jiangxi
     江西吉安—泰和陆相红色盆地沉积体研究
短句来源
     STRATIGRAPHICAL DIVISION AND CORRELATION OF THE RED BEDS IN SMALL BASINS DISPERSED ON THE GUIZHOU PLATEAU
     贵州高原分散小型红色盆地堆积物的划分与对比
短句来源
     A Study on XU Xiake's Investigation about Danxia Landform in Xinjiang Red-bed Basin,Jiangxi Province
     徐霞客江右信江红色盆地丹霞地貌考察研究
短句来源
     The distributi-on of the Paleozoic strata,the Meosozoic and Cenozoic red beds,as well as theYenshanian igneous rocks and modern morphologic landscape are resulted fromthe repeated faultings which also influenced the subsidence of some portions ofpearl River Delta and the occurrence of earthquake of Guangzhou area.
     由于断裂的反复作用,控制着本区古生代地层的分布,中、新生代红色盆地的沉积,燕山期岩浆的侵入与喷发,现代地貌景观的形成,并影响着珠江三角洲部分拗陷的沉降和广州地区地震的发生.
短句来源
     Whereas, the upper Cretaceous-Paleocene red down-faulted basin sediments is mainly distributed in the Anlu and Beiqiao fault depressions. It is continuous in section, rich in fossil and enormous in thickness.
     上白垩统—古新统为断陷红色盆地沉积,主要分布在安角断凹和北桥断凹,剖面连续,化石丰富,厚度巨大。
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  red basin
The ancient weathered crust studied occurs on the razed surfaces of various physiographic periods at different altitudes in the Sichuan red basin.
      
Unlike the loess area in the Red Basin, there is only a thin layer of soil which can be regenerated only over a long period of time.
      
Within the zone of alpine meadows and the uppermost region of natural forest as well as in the Red Basin evidence of pasture and agriculture goes back by at least 2,000 years.
      
So for instance, all river reaches that start with 09020305 are in the Clearwater Watershed in the Red Basin.
      
These rocks form a large, composite, red basin characterized by five sedimentary cycles.
      
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A tank experiment to study the rainfall characteristics,degree of slope and kinds of crops in relation to erosion of the Szechuan purple brown soil was carried out on the experimental farm of the University of Nanking in Chengtu during the period from 1941 to 1945 inclusive.The text consists of the results,of four years only,that of the first year being used for reference.

本试验就成都南郊金陵大学农场利用箱具装置以求降雨,坡度及作物种类对于四川紫棕土冲蚀之关系,试验自1941年须始至1945年年底为止,本报告包括1942至1945年四年记录;最初一年记录仅供参考未列入计算。试验中之箱具係木制,长1.8公尺,宽0.35公尺,深0.33公尺,共四具,分别置于5%,10%,20%及30%之四种坡度上,内盛四川红色盆地中之一种紫棕色粘土。降雨之时,每廿小时测定雨量,逕流及土壤冲矢量各一次,试验中192及1943两年行播芝蔴代表茎葉稀疏之作物,1944及1945年密播大豆代表茎菜密茂之作物。四年结果中之要点如下:(i)本试验四年中成都年降水量总平均为959.9公厘,最少年为689.9公厘而最多年为489.8公厘,本试验芝蔴年度平均降水量为734.0公厘,而大豆年度平均降水量为1185.8公厘。(ii)成都降雨烈度可暂按廿四小时内雨量,分为0—3.9m.m.,4—7.9m.m.,8—11.9m.m.,12—23.9m.m.,24—17.9m.m.,4(?)—95.6m.m.,96—191.9m.m.,等七级,四年中廿四小时内最多雨量可自84.2公厘至183.2公厘不等,此项烈雨...

本试验就成都南郊金陵大学农场利用箱具装置以求降雨,坡度及作物种类对于四川紫棕土冲蚀之关系,试验自1941年须始至1945年年底为止,本报告包括1942至1945年四年记录;最初一年记录仅供参考未列入计算。试验中之箱具係木制,长1.8公尺,宽0.35公尺,深0.33公尺,共四具,分别置于5%,10%,20%及30%之四种坡度上,内盛四川红色盆地中之一种紫棕色粘土。降雨之时,每廿小时测定雨量,逕流及土壤冲矢量各一次,试验中192及1943两年行播芝蔴代表茎葉稀疏之作物,1944及1945年密播大豆代表茎菜密茂之作物。四年结果中之要点如下:(i)本试验四年中成都年降水量总平均为959.9公厘,最少年为689.9公厘而最多年为489.8公厘,本试验芝蔴年度平均降水量为734.0公厘,而大豆年度平均降水量为1185.8公厘。(ii)成都降雨烈度可暂按廿四小时内雨量,分为0—3.9m.m.,4—7.9m.m.,8—11.9m.m.,12—23.9m.m.,24—17.9m.m.,4(?)—95.6m.m.,96—191.9m.m.,等七级,四年中廿四小时内最多雨量可自84.2公厘至183.2公厘不等,此项烈雨可降于六月初至八月底之间,廿四小时内大于24公厘之雨日可自七日至十七日不等。(iii)芝蔴年度年降水量虽较大豆年度为低,但逕流占年雨量百分数,依坡度顺序,则前者各为16.95%,19.23%,25.71%及27.66%而后者各为3.96%,9.06%,9.63%及10.62%。(iv)四年中逕流量之实际数值,依坡度顺序,芝蔴年度各为129.11公厘,143.79公厘,193.54公厘及216.64公厘,而后者各为53.37公厘,120.59公厘,121.60公厘及135.07公厘。逕流逐月分布隨雨量分佈而变异,惟大豆作物有使逕流分佈百分数,向各月分散之趋势。又芝蔴年度七月份或八月份之逕流量可占年逕流量70%以上。(v)逕流之大部由于廿四小时内大于24公厘之雨量所发生,各坡度上大于24公厘之烈度等级中,在芝蔴年度,其分佈百分数之和幾全人於80%,而在大豆年度,其分佈百分数之和,自约38%至90%以上不等。芝蔴年度逕流量之实际数值较大豆年度为大,但逕流量隨坡度增加之比率则芝蔴年度较大豆年度为小。(vi)土壤冲失量之实际数值,依坡度顺序,芝蔴年度各为每市亩773.91市斤,832.5市斤,2004.93市斤及2822.62市斤,而大豆年度各为每市亩270.02市斤,370.50市斤,666.53市斤及762.95市斤,大豆年度中雨量特別丰沛之年,大豆护土力在大坡度上(坡度30%)更为显盖。(vii)芝蔴年度月雨量对于土壤冲矢量之影响大于对于逕流量之影响,月雨量增多,使同月土壤冲失量增加之百分数较使同月逕流量增加之百分数为大,大豆年度则反是。芝蔴年度土壤冲失量之实际数值较大豆年度为大,目土壤冲失量隨坡度增加之比率,芝蔴年度亦较大豆年度为大。(viii)据本试验情形,某一日之前五日内如降落巨雨,则该日急雨可发生甚大量之逕流及土壤冲失,芝蔴年度此种情形甚显,但大豆年度则不显。(ix)大豆作物之护土力,由于宽阔平向之叶面及密茂之莖叶可遮蔽地面以防雨滴之打击,而落叶护土亦可使地面流水澄清而维持土壤之渗漏速率,又麦稈覆盖地面之护土效力甚宏,如于大豆莖叶向未郁閉之前用之,可防初夏急雨之冲蚀。(X)自成都向南至仁寿县一带之紫棕土斤陵地,可行玉米与大豆等高行栽之间作制,惟大豆宜密植以收护土之效,若能于生长前期,地面覆盖麦稈,则土壤冲蚀之害可大减。

The fault-tectonic belts of Guangzhou-Luofushan are the largest E-W trend fau-lt belts in the central part of Guangzhou area.It has a long developing history,and underwent polyepisode and polystage activites.The repeated tension andcompression(or compressional shear)of nearly N-S direction formed a series oftectonic rocks with different mechanical features and apparent zonation of thetectonic rocks which are superimposed and composed each other.The distributi-on of the Paleozoic strata,the Meosozoic and Cenozoic...

The fault-tectonic belts of Guangzhou-Luofushan are the largest E-W trend fau-lt belts in the central part of Guangzhou area.It has a long developing history,and underwent polyepisode and polystage activites.The repeated tension andcompression(or compressional shear)of nearly N-S direction formed a series oftectonic rocks with different mechanical features and apparent zonation of thetectonic rocks which are superimposed and composed each other.The distributi-on of the Paleozoic strata,the Meosozoic and Cenozoic red beds,as well as theYenshanian igneous rocks and modern morphologic landscape are resulted fromthe repeated faultings which also influenced the subsidence of some portions ofpearl River Delta and the occurrence of earthquake of Guangzhou area.The int-ensity of faulting activity changed from strong to weak since Mesozoic to recenttime,and the intensity progressively decreased.

广州——罗浮山断裂构造带是横亘广州地区中部规模最大的东西向断裂带.发育历史悠久,经历过多期、多阶段的活动,近南北向的拉张与挤压(或压剪)反复交替进行,形成了一系列不同力学性质的构造岩互相迭置、复合和构造岩的明显分带性.由于断裂的反复作用,控制着本区古生代地层的分布,中、新生代红色盆地的沉积,燕山期岩浆的侵入与喷发,现代地貌景观的形成,并影响着珠江三角洲部分拗陷的沉降和广州地区地震的发生.断裂活动强度的发展趋势,在中、新生代以来,由强到弱,挽近时期活动强度趋低.

In the Shanghai area, the upper Jurassic intermediate/acid volcanic, volcaniclastic and sedimentary rock series is widely developed. Its spacial distribution is closely related to the regional Jaulting and volcanic structures. Its lithological features correspond to those of the upper Jurassic both in the western and easten Zejiang province. Whereas, the upper Cretaceous-Paleocene red down-faulted basin sediments is mainly distributed in the Anlu and Beiqiao fault depressions. It is continuous in section, rich...

In the Shanghai area, the upper Jurassic intermediate/acid volcanic, volcaniclastic and sedimentary rock series is widely developed. Its spacial distribution is closely related to the regional Jaulting and volcanic structures. Its lithological features correspond to those of the upper Jurassic both in the western and easten Zejiang province. Whereas, the upper Cretaceous-Paleocene red down-faulted basin sediments is mainly distributed in the Anlu and Beiqiao fault depressions. It is continuous in section, rich in fossil and enormous in thickness.

上海地区上侏罗统中—酸性火山岩、火山碎屑—沉积岩系广泛发育,其空间分布与区域性断裂构造、火山构造有着密切的联系,岩性特征与浙西的上侏罗统颇为一致,同时又兼有浙东的特点;上白垩统—古新统为断陷红色盆地沉积,主要分布在安角断凹和北桥断凹,剖面连续,化石丰富,厚度巨大。

 
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