粗碎屑的英文

• coarse fragment
• grus
• macrofragment
• megaclast

• "粗"英文翻译    wide; thick
• "碎屑"英文翻译    fragment; bits; shard; scrap ...
• "粗碎" 英文翻译 :    breaking;cracking; coarse breaking; coarse crushing; granulation; kibble; primary crushing
• "粗碎冰" 英文翻译 :    crushed ice
• "粗碎的" 英文翻译 :    coarse ground; kibbled
• "粗碎机" 英文翻译 :    boulder crusher; coarse breaker; coarse crusher; coarse-crush machine; first cracker; preliminary crusher; primary crusher
• "粗碎料" 英文翻译 :    coarse particles
• "粗碎片" 英文翻译 :    coarse fragments
• "碎屑" 英文翻译 :    fragment; bits; shard; scrap; refuse; chippings; offal
• "初碎机 粗碎机" 英文翻译 :    primarycrusher
• "粗碎玻璃" 英文翻译 :    crushed glass
• "粗碎豆粒" 英文翻译 :    kibbled beans
• "粗碎谷粒" 英文翻译 :    break chop; groats
• "粗碎谷物" 英文翻译 :    cracked corn; cracked grain
• "粗碎谷物, 碎米" 英文翻译 :    cracked grain
• "粗碎油饼" 英文翻译 :    kibbled cake
• "粗碎玉米" 英文翻译 :    corn grits
• "粗碎圆锥" 英文翻译 :    coarse cone
• "碎屑；碎屑的" 英文翻译 :    clastic
• "骨碎屑" 英文翻译 :    bone scraps
• "角碎屑" 英文翻译 :    anguclast
• "内碎屑" 英文翻译 :    intraclast
• "切屑；碎屑" 英文翻译 :    chip
• "室碎屑" 英文翻译 :    chamber detritus
• "碎片,碎屑" 英文翻译 :    chip

• The discriminant analysis on inorganic element abundance shows that the palaeosedimentary environment of jurassic in the yanqi basin is close to that of dongying sag
  萨胡判别分析证明，与煤共生的粗碎屑岩不是形成于河流环境，而是形成于深水浊积沉积环境。
• Railway jacking bridge engineering passing through sand pebble ( gravel ) layer , because it is a complex loose coarse fragment accumulation layer , the roadbed must be reinforced
  摘要铁路顶桥工程中遇到砂卵（砾）石层时，因砂卵（砾）石层是一种复杂松散粗碎屑堆积层，因此必须对铁路路基进行加固。
• The upper cretaceous jingzhushan formation in the biru basin , xizang consists of a succession of coarse - grained elastic rocks in the alluvial fan - fan delta depositional system , intercalated with intermediate - acidic volcanic rocks including dacite , andesite , quartz trachyandesite and rhyolite
  摘要上白垩统竞柱山组为一套冲积扇扇三角洲沉积体系的粗碎屑岩，间夹由英安岩、安山岩、石英粗安岩和流纹岩组成的中酸性火山岩。
• Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous , is featured by simple sedimentary feature , depositional cycle , small lacustrine transgressive , dry climate , salinization lacustrine water and multi - and - near sources
  摘要二连盆地是在海西期地槽褶皱基底上发育起来的早白垩世断陷湖泊群，具有湖盆湖浸规模较小、气候条件干燥、湖水咸化、沉积旋回单一，多物源、近物源和粗碎屑等沉积特征，以及发育岩性地层油气藏为主的油气分布特点。
• 2 ) analyses and researches systematicly the lithofacies , sedimentary facies and depositional environment of the dayi conglomerate in the cenozoic longmenshan foreland basin . this paper analyzes detailed six coarse elastics lithofacies , five mid - elastics lithofacies and three fine elastics lithofacies . establishes the association of three depositional environment types including alluvial fan and river
  2 )对新生代龙门山前陆盆地大邑砾岩岩相、沉积相和沉积环境进行了系统分析和研究，划分出6种粗碎屑岩相、 5种中碎屑岩相、 3种细碎屑岩相，确定了大邑砾岩为冲积扇相、河流相沉积环境的组合。
• Besides , the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration . the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings . the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north , the coarse lithology of fan - delta prograded from north to south in fall - hemicycles , and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south , braided stream facies prograded from sorth to north in the fall - hemicycles , but the lacustrine facies and salt lake facies developed in the middle part of the area
  详细的沉积相研究发现，红狮地区第三系发育有冲积扇、水下冲积扇、河流、三角洲、扇三角洲、湖泊和湖底扇7种主要沉积相类型，并对作为区内主要勘探目的层系的下干柴沟组和上干柴沟组进行了以超层序为单位的沉积相平面编图，以较高的时间分辨率揭示了区内沉积相带的平面展布及其在不同构造背景中的分布规律，比如在北部的凹陷陡坡背景下，上升半旋回低水位期通常发育有水下扇、湖底扇等陡岸近源特征的沉积体系，下降半旋回高水位期，扇三角洲相粗碎屑岩由北向南进积;在南部的凹陷缓坡背景下，上升半旋回主要发育辫状河流相，下降半旋回辫状河三角洲相由南向北进积;而中部红柳泉一狮子沟一带则为湖泊相沉积和盐类沉积。
• The basin - formed mechanism , evolution model and petroliferous geological features of compresso - shear basins in the world are analyzed , by which six aspects of the features are summarized as follows : 1 ) in the compresso - shear process , the sedimentary speed of basin is high , forming thicker coarse - grained clastic rocks which normally shape good petroleum reservoir ; 2 ) the source rocks of basin tend to coming from the organic matter - enriched rocks formed in pre - compresso - shear stages , except that in intense compresso - shear process , deep water - semi deep water source rocks are possibly developed in pre - compresso - shear stages , e4xcept that in intense compresso - shear process , deep water - semi deep water source rocks are possibly developed in frontal of deep depression ( fore deep ) of thrust belt ; 3 ) the en echelon folds ( including anticline and fault - nose structure ) are generally as good oil traps ; 4 ) the compresso - shear process is helpful to hydrocarbon accumulation ; 5 ) it may promote the maturity and hydrocarbon - generating process of organic matte , and 6 ) the thrust belts in the surrounding areas of compresso - shear basin are favorable are favorable domains for petroleum concentration
  摘要通过对世界上压扭性盆地的成盆机制、演化模式和油气地质特点分析，总结压扭性盆地具有6个方面的石油地质特征：压扭作用期间盆地的沉积速率较高，一般形成较厚的粗碎屑沉积，它们常构成很好的油气储集层：盆地的烃源岩往住来自于前压扭期砂成的富含有机质的岩石，但在强烈的压扭作用期间，在冲断带的前缘深坳陷（前渊）中有可能发育深水半深水相的烃源岩；压扭（张扭）作用期间形成的雁行式褶皱（包括背斜和断鼻等）往住是很好的油气圈闭；压扭作用易于成藏；压扭作用可以促进有机质的成熟生烃作用；压扭性盆地的周边冲断带是油气赋存的有利部位。
• During my master " degree investigation , i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts , the eastern yanshan , and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution , volcanism and tectonism . then i summarized the mesozoic basin development and the coupling characters of basin and mountain . the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic , the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous
  在野外典型路线调查的基础上，对燕山地区东段承德、平泉地区的中生代盆地中发育的粗碎屑沉积层，进行了系统的物源分析与古流测定，并在此基础上重点剖析了盆地的发育、火山活动、构造变动三者之间的关系，总结了本区中生代盆地发育规律及盆山耦合特征，并将盆山演化划分为：三叠纪?早侏罗纪的构造挤压隆升与挠曲盆地发育阶段阶段，中晚侏罗纪的构造挤压?火山活动与类前陆盆地发育阶段，早白垩世的拉张断陷盆地发育阶段。
• In the chronstratigraphic framework , the facies , the depositional system and the principle and range of reservoirs distribution are studied . the main depositional system is braided delta ? ub - lake fan . the coarse lithofacies which form braided delta depositional system is sub - water channel deposits ; the coarse lithofacies which form the sub - lake fan depositional system include turbidity channel deposits and bedded turbidity deposits
  在等时地层格架内，总结了各个中期旋回的沉积相类型、沉积体系和展布规律及范围，认为研究区在该时期以辫状三角洲?湖底扇沉积为主；构成辫状三角洲的粗碎屑相为水下分支河道；构成湖底扇的粗碎屑相包括：浊流水道相、层状浊积岩相。
• Many research such as clay minerals , suspend in the sea , the grain size trend analysis of surface sediment , poc 6 cu and 8 c13 in bottom sediments etc . showed that : the yellow sea warm current divided the south yellow sea into two , the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current , and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period , sedimentation stratum , and oxygen isotope record
  粘土矿物、碳酸盐、粗碎屑、海域悬浮体、表层沉积物粒度趋势分析、 poc c ~ ( 13 )及底质沉积物的c ~ ( 13 )等多方面研究表明：以黄海暖流为主导，南黄海堆积陆架平原西侧现代沉积物陆源物质主要源于黄海沿岸流携带的现代黄河悬移物质，黄海槽东西两侧的沉积差异主要表现在冰消期以来沉积厚度、沉积层序、氧同位素记录上。