lake facies中文是什么意思

• 湖相

• lake    vi. 血球溶解。 vt. 使(血液)发生血球溶解。
• facies    n. 〔pl.〕 〔单复同〕 1.颜面，外观；外表。 2 ...
• lacustrine facies;lake acies    湖相
• facies    n. 〔pl.〕 〔单复同〕 1.颜面，外观；外表。 2.【生态】演替系列混优种社会，演替系列变群丛。 3.【地质学；地理学】相。 4.【医学】面色；表面。
• deesea facies(abyssal facies)    深海相
• lacustrine facies; limnetic facies    湖相
• mitrotricuspid facies mitral facies    二尖瓣病面容,二尖瓣三尖瓣病面容
• by the lake    在湖边
• lake    n. 莱克〔姓氏〕。 n. 1. 湖(公园等中的)池塘，小湖。 2.(贮油等的)池。 The Great L- 大西洋。 The Great L-s 北美洲五大湖。 the L-s (英国北部的)湖泊地区。 Go jump in the lake ! 〔美俚〕别来麻烦! 滚开!不要吵 lake2 n. 1. 【化学】色淀；沉淀染料。 2.胭脂红。 vi. 血球溶解。 vt. 使(血液)发生血球溶解。
• lake no    诺湖
• of the lake    湖泊
• on the lake    在湖面上; 在湖上
• the lake    湖心骇客
• a ociated facies    共生相
• abnormal facies    异常面容
• abysmal facies    深海相
• abyssal facies    深海相
• acromegaly facies    肢端肥大症面容
• actinolitegreenschist facies    阳起石绿片岩相
• adenoid facies    增殖腺面容
• aeolian facies    风积相
• ahydrous facies    无水相
• albiteepidotehornfels facies    钠长石绿帘石角岩相
• aldan facies    紫苏花岗岩相
• algal facies    藻相

• It was developed mostly deep lake facies on the south of basin and coastal - shallow lake facies on the north of basin
  此时期盆地南缘主要发育半深湖亚相，盆地北缘则发育滨浅湖亚相。
• From northern and western to southern and eastern , the sedimentary facies transited from fan delta , braided delta to lake facies
  由北、西向南、东，沉积相由扇三角洲、辫状河三角洲向湖泊过渡。
• Discovery and study of the early pleistocene river and lake facies stratum in bukedaban area of the western segment in the eastern kunlun mt
  东昆仑西段布喀达坂峰地区早更新世河湖相地层的发现及初步研究
• Flat bedding , wavy bedding and vermiglyph were often found in the shallow lake facies , and the log was usually straight or slight dentation
  滨浅湖相常发育水平层理、波状层理及虫迹，测井曲线形态较平直，常呈微齿状。
• 3 ) the pingdiquan formation mainly are the deposition of lake and fan - delta , fan - delta developing in the background of the lake facies sedimentary
  平地泉组以湖，扇三角洲相沉积为主，扇三角洲的生长是在湖相的背景下进行的。
• The types of sedimentary facies were mainly fan - shaped delta , delta , binshore subaqueous fans , slump turbid fan , lake facies , fluvial facies
  该研究区主要发育扇三角洲、三角洲、近岸水下扇、滑塌浊积扇、湖相和河流相沉积。
• Early permian was initial stages of expanding of the lake basin . inside the region of interest , there developed fan delta , braided delta and lake facies
  早二叠世是湖盆扩张初期，区内发育扇三角洲相、辫状河三角洲相和湖泊相。
• In the fairly deep lake facies there found abundant bivalve fossils , such as the standard foss il of permian in north xingjiang - tarfaniasp . ,
  半深湖相中发现丰富的瓣鳃类动物化石，如北疆地区二叠系标准化石?吐鲁番鳕鱼及介形类等。
• Ostracoda , and so on . in the deep lake facies of niujuanhu and mazhong structural belts , there were also discovered gravity - flow microfacies , which was mainly composed of turbidite in which the slump structure and convolute bedding were often found
  马朗凹陷牛圈湖构造带、马中构造带的半深湖相中，发育湖泊重力流微相，典型的表现为浊积岩的发育，其中可见到重力滑塌构造及包卷层理等。
• At the beginning of tiaohu period , the lake basin shrank , and the water became shallow . braided river facies and braided delta facies were found on both side of the basin , and deep lake facies disappeared , and shallow lake facies was only found in the southern of tiaohu seg and central part of malang seg
  从中二叠世条湖期开始，湖盆发生萎缩，水体变浅，盆地南北两侧出现辫状河及辫状河三角洲相沉积，半深湖相消失，仅在条湖凹陷南缘及马朗凹陷中部残余滨浅湖相沉积。