碎巖屑 的英文怎麼說
中文拼音 [suìyánxiè]
碎巖屑
英文
fragmental debris-
The study shows that cretaceous volcanics mainly consist of medium acidic volcanic lava and volcanoclastic rocks, with locally developed basic lava ; medium acidic volcanics mainly consists of calc - alkalic series, was formed in compressive orogenic environment, and has good reservoir property, while cretaceous basis lava mainly consists of alkalic series, was formed in rift environment, and has poor reservoir property
結果認為,白堊紀火山巖以中酸性火山熔巖和火山碎屑巖為主,局部發育基性熔巖;中酸性火山巖以鈣堿性系列為主,形成於擠壓造山環境,儲集性能較好,而白堊紀基性熔巖以堿性系列為主,形成於裂谷環境,儲集性能較差。In places, hill - slope debris forms a mantle over the bedrock and alluvium fills some of the valleys
在部分地方,基巖表面由巖石碎屑堆積形成覆蓋層,而部分河谷則有沖積層。The wall rock of the mine is the third member of aqishan formation, which it is formed by the neutral - acidic volcanic rock and volcanic arenite of calcium - alkala series. the rock is mainly of andesite, quartz andesite, volcanic breccia agglomerate and volcanic breccia
礦床賦礦圍巖為阿奇山組第三巖性段鈣堿系列的中酸性火山巖-火山碎屑巖,主要巖性為安山巖、英安巖、火山角礫熔巖、火山角礫巖等。Existence of charcoal fragments in sedimentary basaltic volcanoclastic rock and its implication in geology, in longtan formation of southwesten guizhou
黔西南地區龍潭組玄武質火山碎屑巖中木炭碎屑的存在及地質意義Through the search of bourn of intraclast congeries silica rock, its earth and west side all grow consortium robble
經對內碎屑堆積硅質巖的邊界研究發現,其東西兩側均發育有同生斷裂。Based on the authigenic and clay mineral assemblage, two types of diagenetic ambient have been recognized in the meso - cainozoic detrital rocks in tarim basin
根據自生礦物與粘土礦物組合,在塔里木中新生界碎屑巖中可以識別出兩種成巖環境。Thin layers of sandy shale, and carbonaceous fragments are locally present.
局部出現砂質頁巖薄層和碳質碎屑。Carbonate rocks are predominantly composed of intra - clastic dolostone, chert dolostone and sand - bearing dolostone
碳酸鹽巖以內碎屑白雲巖、燧石白雲兒和含砂白雲巖為主。The lower part formed in a littoral - epeiric environment, is a series of elastic rocks, partly contains carbonate rock and metamorphic basic volcanic rocks and the upper part formed in a bathypelagic environment is a series of sediments with chert, partly contains metamorphic basic volcanic rocks
其下部為一套濱淺相碎屑巖,局部夾碳酸鹽巖、變質基性火山巖;上部為一套深水沉積巖系夾硅質巖,局部夾變質基性火山巖。Clastic facies pattern recognition is somewhat systematic.
碎屑巖相模式的識別是帶有一定系統性的。Fine description method of clastic reservoir
碎屑巖油氣儲層精細描述方法The division of diagenetic stages in clastic rocks
碎屑巖成巖階段劃分Method of grain - size analysis of clastic rocks
碎屑巖粒度分析方法Rock resistivity displacement experiment of core on clastic reservoir
碎屑巖儲層巖石電性水驅實驗Characters of deep - buried clastic reservoir rocks in hexiwu structural belt of langgu depression
廊固凹陷河西務構造帶深部碎屑巖儲層特徵Prediction for igneous intrusive mass of clastic reservoir in the pericline area around central tarim basin
塔中圍斜區碎屑巖儲層火成巖侵入體預測Ore area locate on, silver factory ditch - ancient tomb ditch in west branch river set lower bench, stratigraphic succession, rock assemblage are different with circumference. most is a set of intraclast congeries silica rock. in search of it, its distribution range in the silver factory ditch - ancient tomb ditch
礦區所在部位銀廠溝?古墓溝一帶,西岔河組下段地層中,地層層序、巖石組合特徵與周邊地區存在明顯的差異。主要為一套內碎屑堆積的硅質巖。Rock fragments, including volcanics, are common, and the matrix consists largely of kaolin and illite.
常見有巖石碎塊,包括火山巖屑,基質大部分為高齡土和伊利石。The cardium sandstone is lithic, being composed of grains of chert, quartz, quartzite, silicified argillite, and other rock fragments.
卡迪砂巖是巖屑砂巖,由燧石,石英、石英巖、硅化泥板巖和其它巖石碎屑顆粒所組成。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。分享友人