鹽類巖屑 的英文怎麼說

中文拼音 [yánlèiyánxiè]
鹽類巖屑 英文
halolite
  • : 名詞1. (食鹽; 鹽類) salt 2. (姓氏) a surname
  • : Ⅰ名1 (許多相似或相同的事物的綜合; 種類) class; category; kind; type 2 (姓氏) a surname Ⅱ動詞...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : Ⅰ名詞(碎末) bits; scraps; crumbs Ⅱ形容詞(瑣碎) trifling Ⅲ動詞(認為值得) think sth. worth doing
  • 鹽類 : e. salt
  1. 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

    詳細的沉積相研究發現,紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖,以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陷陡坡背景下,上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系,下降半旋迴高水位期,扇三角洲相粗碎由北向南進積;在南部的凹陷緩坡背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和沉積。
  2. The microfacies of carbonate rock of the wudaoliang group in hoh xil basin is divided for marl lithofacies, micrite facies, micrite ( spar ) scraps ash lithofacies, grain scraps micrite facies, dolimite rock lithofacies, and the stromatolite ash lithofacies

    可可西里盆地五道梁群碳酸微相型主要為泥灰相、泥晶灰相、泥(亮)晶粒相、粒泥晶灰相、白雲相、疊層石灰相、核形石灰相等7種微相。
  3. This thesis emphasizes to proceed the study on the mechanism of formation of the reservoirs of lower palaeozoic burial hills in the regions of zhuangxi and chengdao from the angle of geochemistry. the research of petrology reveal rock types of the regions mainly include carbonate rock, claystone, siltstone, breccia and a few of evaporite rock

    石學研究表明,樁西、埕島地區下古生界古潛山儲層的型有碳酸、粘土、碎、以及少量蒸發,其中碳酸是該區下古生界古潛山儲層最主要的型,為一種穩定地臺型海相沉積環境的產物。
  4. Abstract : to the principle and project that tu guangazhi proposed in 1990, the gold ore deposits in qinling ( shaanxi ) may be classified into fouowing types : archean high - grade gneiss type, fine grained fragmental rock - carbonate rock - silicilith type, metamorphic fragmental rock type, volcanic rock type, explosive breccia type, intrusive rock exo - and endo - contact zone type. inthis paper, the geological characteristics, metallogenic geological setting, the source of ore - forming materials, digenic mechanism and metallogenetic epoch of gold ore deposits are also discussed

    文摘:參照塗光熾先生( 1990 )提出的礦床型劃分原則與金礦分方案,將陜西秦嶺地區原生金礦劃分為太古界綠建造型、細碎-碳酸-硅質建造型、變質碎型、火山建造型、隱爆角礫型和侵入內外接觸型金礦,並對各型金礦的地質特徵、成礦地質背景、成礦物質來源、礦床形成機制及形成時代等問題進行了論述和討論。
  5. The reservoir types in lucaogou formation is carbonate rock, clastic rock and tuff, while the reservoir types in tiaohu formation is mainly tuff and volcanic rock

    蘆草溝組儲層型主要有碳酸、碎及沉凝灰,而條湖組則主要為火山和沉凝灰
  6. Two kinds of ore have been identified. the first type is characterized by syngenetic sedimentation, which is called as hot - water sedimentary ore. the ore emerges in bedded orebodies which have stable thickness

    作為典型礦例的佛子沖礦田主要產于下志留統細碎夾碳酸地層中,作者首次在礦田內發現了兩種不同礦石型:一礦石具有典型的同生沉積特徵,稱之為熱水沉積型礦石,礦石產于層狀、似層狀礦體中。
  7. ( oxifordian - kimmeridgian ), xueshan fm. ( tithonian - berriasian ). according to field investigation, thin section identification and many other methods of sedimentary petrology, rock types of jurassic strata include carbonates, argillaceous rocks and clastic rocks

    結合野外觀察和室內鏡下鑒定等多種沉積石研究方法,研究區侏羅系型計有碳酸、泥質和碎三大
  8. Petroleum reserves in carbonate reservoir are only one - tenth of the total production. natural gas yields, however, only holding a small part in petroleum production, are nearly equal in both type reservoirs. such situation does not match the ratio that carbonate formation hold in the strata

    我國的石油主要產自碎儲層,而碳酸儲層中的石油儲量僅占我國石油儲量的十分之一,天然氣儲量雖在兩儲層中近似,但數量不多,這與我國碳酸地層所佔比例很不相稱。
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