灰屑巖 的英文怎麼說
中文拼音 [huīxièyán]
灰屑巖
英文
calcarenite-
The ash, cinders, and other fragments become a consolidated rock.
火山灰、火山渣和其它碎屑變成了固結的巖石。The mine zone is sandwiched between an overlying block of flows, pillow lavas and minor pyroclastics, and underlying agglomerates, tuffs, and more massive diabase bodies.
含礦帶夾在上覆的巖流、枕狀巖流和少量火山碎屑巖塊與下伏的集塊巖、凝灰巖和塊狀輝綠巖體之間。Typical sedimentary structures of tempestite, such as radiate and imbricate arrangements of strip dolomitic limestone gravels, grading beddings and ripple beddings are presented in the succession, indicating its accumulation in a shoreline environment
該風暴沉積的底面侵蝕構造清楚,長條形白雲質灰巖礫屑具放射狀構造或疊瓦狀構造,並發育渠鑄模、粒序層理和小型波狀層理等沉積構造,為典型的淺水風暴巖。The microfacies characteristic of carbonate rock of suonahu formation in cuoqinin basin constitutes with the marl lithofacies, the intraclast ash lithofacies, biological detritus ash lithofacies
措勤盆地嗩吶湖組碳酸鹽巖微相由內碎屑灰巖相、生物碎屑灰巖相和泥灰巖相組成。The thesis analysises the typical model profile and the special rock profile of wudaoliang group of miocene epoch in hoh xil basin. and be used the biocalcarenite with the marl rock take the marker bed of wudaoliang group
論文對可可西里盆地中新世五道梁群的典型剖面和特殊巖性剖面進行了分析,並以泥灰巖和生物碎屑灰巖作為五道梁群的標志層。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鹽巖微相類型主要為泥灰巖相、泥晶灰巖相、泥(亮)晶粒屑灰巖相、粒屑泥晶灰巖相、白雲巖相、疊層石灰巖相、核形石灰巖相等7種微相。The northern qiangtang basin suonahu formation microfacies of carbonate rock is divided for the intraclast ash lithofacies, biological detritus ash lithofacies, oncolite limestone lithofacies, contain the calcium and alga ash lithofacies, marl lithofacies and pure microlite limestone lithofacies
羌北盆地嗩吶湖組碳酸鹽巖微相為內碎屑灰巖相、生物碎屑灰巖相、核形石灰巖相、含膏藻灰巖相、泥灰巖相和純微晶灰巖相等6種微相。As the land above the magma chamber collapses, immense gray clouds called pyroclastic flows burst out horizontally all around the caldera
當巖漿庫上方的陸地崩陷,稱為火山碎屑流的巨大灰色雲霧,會突然由火山臼的周圍向外水平散開。This paper emphasizes the effect of the dissolution of aluminosilicate during diagenesis may provide more radiogenic strontium which would result in a high content of strontium in carbonate rocks. so we should avoid the vein of carbonate and select the samples with less terrigenous clastic, less grain content and lacking calcite cementation collected as analysis samples. the microcrystalline limestone and micro - to fine - crystalline dolomite are rather fairly whole rock samples
作者還強調了成巖過程中由長石等鋁硅酸鹽溶解提供殼源sr所造成的碳酸鹽礦物成巖蝕變可能表現為較高的sr含量;因此,在用全巖樣品進行旨在反映海水組成的各種分析時,應迴避碳酸鹽脈,選擇含陸源碎屑低、顆粒數量少、缺乏方解石膠結物的樣品,微晶灰巖或微?粉晶白雲巖是較為理想的全巖樣品。Through observation, description, slice identification of cores and chemical analysis of whole rock, it is determined that the central volcanic rocks of the eastern depression are classified as four major types, i. e. basalt, trachyte, tuff and cataclasite of sedimentary volcanic rocks, in which trachyte is of basic series and potassium rock type
通過巖心觀察、描述,巖心薄片鑒定,全巖化學分析等資料,確定東部凹陷中段火山巖巖石類型分為4大類:玄武巖、粗面巖、凝灰巖和沉火山碎屑巖類,其中粗面巖類屬于堿性系列、鉀巖類型。The reservoirs in permian is consist of carbonate rock, tuff, clastic rock and volcanic rock
二疊系儲集層主要由碳酸鹽巖、沉凝灰巖、碎屑巖和火山巖組成。Was made up of thick neutral and basic volcanics, volcanoclastic rocks and few normal sedimentary rocks. the sedimentary rocks of tiaohu fm. were mainly composed of terreverte or mauve mudstone, sandstone and glutenite
條湖組的分佈范圍與蘆草溝組大致相當,但巖性卻差異很大,為厚層中?基性火山巖、火山碎屑巖,是火山活動頻繁的證據,條湖組沉積巖夾在火山巖中間,主要為灰綠、紫紅色泥巖、砂巖及砂礫巖。Synthesizely contrasted the suonahu formation profile of the northern qiangtang basin and cuoqin basin of miocene epoch, used the intraclast ash rock as the marker bed of the suonahu formation
對羌北盆地和措勤盆地中新世的嗩吶湖組剖面作了綜合對比,將內碎屑灰巖作為嗩吶湖組的標志層。The main characters of the thermal fluid activity are recognized as follow : many types and stages of veins are widely developed ; vitrinite reflectivity of different areas varies apparently with the depth ; there was a high temperature field during the formation of the thermal fluid, meanwhile, the volcaniclastic rocks were modificated by the thermal fluid activity, for example, sericitization of plagioclase, chloritization of volcanic detritus in andesitic detris tuff ; in the tufaceous mud, the thermal fluid activity accelerates " maturating " of the organic carbon by heating ; and the trace elements show an anomaly in the wall rocks
同時,受熱流體活動的影響,熱流體對火山碎屑巖具有一定改造作用,如在安山質巖屑凝灰巖中,斜長石絹雲母化、火山巖巖屑綠泥石化明顯;在凝灰質泥巖中,熱流體對圍巖中有機碳具有明顯的「催熟」加熱作用,微量元素則出現異常現象。On the point favorable reservoir zones are predicted. it is suggested that donghe sandstone and bioclastic limestone members should be main targets of oil - gas exploration in the region
據此作出有利勘探區帶預測,建議將東河砂巖段和生屑灰巖段作為本區油氣勘探的重要目標。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
蘆草溝組儲層巖石類型主要有碳酸鹽巖、碎屑巖及沉凝灰巖,而條湖組則主要為火山巖和沉凝灰巖。1. the framework of mesozoic strata in the north margin of the dabie orogenic belt was reestablished according to the discovery of the tuff beds and volcanic debris in zhougongshan and fenghaungtai formations, along with their isotope ages and the correlations of sedimentary facies and heavy minerals
在周公山組中在鳳凰臺組中發現了火山凝灰巖層利火山巖碎屑,結合同位素年代學研究以及沉積相和重礦物對比,重新釐定了大別造山帶北緣中生代地層的格架。The open platform limestones are arranged in the risum - ge ' gyai tarico stratigraphie subprovince, while the restricted platform limestones and terrigenous progradational clastic rocks are observed in the coqen - xainza stratigraphic subprovince in the south and muggar kangri stratigraphic subprovince in the north
早白堊世晚期,盆地以臺地相碳酸鹽巖沉積為主,裂谷帶附近以發育臺地邊緣礁灘相沉積;裂谷帶兩側的日松革吉它日錯分區主要由開闊臺地相灰巖組成;盆地南北部的措勤申扎分區和木嘎崗日分區由局限臺地相灰巖和陸源進積碎屑巖組成。Light gray, light yellow gray carbonate rock, clastic rock, a little amount mudstone with the gypsum rock in suonahu formation, regarding carbonate rock as principle
嗩吶湖組主要發育淺灰色、淺黃灰色碳酸鹽巖、碎屑巖,少量泥巖和石膏巖沉積,以碳酸鹽巖為主。The lower paleozoic strata in the south kunlun massif are kulafuhe group of cambbrian - ordovician. they consists of metamorphic detrital rocks, limestone, magnetite - bearing basalt, quartzite ( meta - silicalite ), which suggests that they might form at active continent margin. the geochemical characteristics of volcanic and detrital rocks do indicate that they might form at an active marginal environment such as island arc etc. associated with the qimanyuter ophiolite suit, there are lots of early paleozoic granitic plutons
在昆南地塊上的早古生代地層為寒武?奧陶系庫拉甫河巖群,由變碎屑巖、灰巖、含磁鐵礦玄武巖、石英巖(變硅質巖)等組成,顯示其比昆北地塊有較大的活動性,火山巖和碎屑巖的巖石地球化學特徵也反映為島弧及活動邊緣環境。分享友人