沉積巖組英文怎麼說

沉積巖組 的英文翻譯

沉積巖組 例句

1. The immediate host siliceous rocks of typical deposits ( jinya, gaolong ) are of hydrothermal sedimentary origin. gold ore bodies are layer - like and generally concordant with their host rocks. abundant relict synsedimentary fabrics are preserved in the ores
   典型礦床（金牙、高龍）中的含礦硅質 巖 屬熱水 沉 積 巖 ，礦體形態主要為與地層整合的層狀和似層狀，礦石具有大量同生 沉 積 的標型 組 構。
2. Dividing the sedimentary facies as a delta - lacustrine facies according to wudaoliang group sedimentary rock facies and its combination, regarding lacustrine facies as principle ; the northern qiangtang suonahu formation sedimentary facies was divided for fluvial facies and the lacustrine facies, regarding lacustrine facies as principle
   根據五道梁群 沉 積 巖 相特徵及其 組 合，將五道梁 沉 積 相劃分為扇三角洲- -湖泊相，以湖泊相為主。羌北盆地嗩吶湖 組 沉 積 相劃分為河流相和湖泊相，以湖泊相為主。
3. In the area of the left bank, rock body is mainly composed of permian period - triassic period granite and triassic period siltstones and mudstones ( t2m ). moreover, the rock body has been more faulted, such as f1 f3 f9 and so on. in addition, there also exist a lot of joints and form complex rock mass structure
   工程區主要出露二迭紀三迭紀花崗 巖 體（ _ 4 ~ 3 _ 5 ~ 1 ）和三迭系中統忙懷 組 下段 沉 積 巖 （ t _ （ 2m ） ~ 1 ） ，發育有工程區規模最大的f _ 1和f _ 3斷層，以及其它斷層和大量的各類斷續延伸的裂隙， 巖 體結構較為復雜。
4. Based on the variation of light / heavy mineral components of sedimentary rocks, the typomorphic characteristics of various debris, the cathodoluminescence color of quartzes, the direction of paleocurrent and the extension of sedimentary facies, two source direction of the studied area in carboniferous and permian can be recognized, one is in bayanwusu, wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos, another is alashan area in the northwest margin of ordos
   在深入研究本區 沉 積 巖 輕、重礦物 組 分的變化、各種 巖 屑的標型特徵、石英陰極發光顏色、古水流方向及 沉 積 相帶展布等基礎上，認為研究區石炭?二疊紀的物源方向主要有兩個，分別為：北緣杭錦旗以北的巴彥烏蘇、烏蘭格爾及河套陰山地區；以及研究區西北緣的阿拉善地區。
5. Depositional facies, a term of petroleum geology, is a combination of sedimentary rocks produced by a certain depositional environment
   沉 積 相是石油地質學中的一個術語，是指一定的 沉 積 環境所形成的 沉積巖組 合。

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