暗色巖 的英文怎麼說

中文拼音 [ànshǎiyán]
暗色巖 英文
melanocrate
  • 暗 : Ⅰ形容詞1 （光線不足; 黑暗; 暗淡） dark; dim; dull 2 （不顯露的; 秘密的） hidden; secret 3 [書面語...
  • 色 : 色名詞[口語] （顏色） colour
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 暗色 : dark color
  1. The microscopical observation proves that the main types of granitoid rocks are granodiorite and quartz monzodiorite, and the enclave is mainly monzodiorite. the rock - forming minerals are mainly k - feldspar, plagioclase, amphiboie, biotite, quartz, magnetite, titanite, apatite, epidote, etc. the zonation of the feldspars is very popular. the dark - colored minerals, such as biotite and titanite, have been highly oxidized

    通過對本區花崗巖類樣品進行顯微觀察研究，知其主要的巖石類型為花崗閃長巖、石英二長閃長巖，其中的巖石包體主要為二長閃長巖，其造巖礦物為鉀長石、斜長石、角閃石、黑雲母、石英、磁鐵礦、榍石、磷灰石和綠簾石等，長石中環帶現象比較常見，黑雲母、榍石等暗色礦物顏色較深，表明其氧化程度較高。
  2. The dark green tints in the south of wales and the gloucestershire area reflect high strontium values associated with evaporites.

    位於南威爾士和格洛斯特郡地區的暗綠色反映了與蒸發巖有關的高鍶值。
  3. In low - lying area, dark - colored mudstones have been developed, the organic matter richness are increased, the kerogen type is better and in matural stage, so it has better oil source bases

    窪陷內暗色泥巖發育，有機質豐度較高，乾酪根類型較好，處于成熟演化階段，具有較好的生油物質基礎。
  4. Sedimentary environment of dark mudstone member of kongdian formation from well wang 46, dongying sag

    東營凹陷王46井孔二段暗色泥巖沉積環境
  5. The dark mudstone of neogene system in sikeshu sag of junggar basin is a potential source rock with vitrinite reflectance ( r ( subscript 。

    摘要準噶爾盆地四棵樹凹陷新近系暗色泥巖鏡質體反射率r （下標。
  6. There are a lot of capture crystals in the rock of basic end - member

    暗色微粒包體中多見寄主二長花崗巖中的捕擄晶。
  7. This formation is dominated by a set of sandstone - mudstone dark clastic rock series which belongs to marginal marine deposit at the end of the gondwana carboniferous - permian glacier period

    該組主要為一套砂巖泥巖的暗色碎屑巖系，屬岡瓦納石炭二疊紀冰川末期的邊緣海沉積。
  8. Terrestrial sediments consist mainly of fluvial and lacustrine facies have the following characteristics : lacustrine basins have undergone a long continuous and fast subsidence and contain many terrestrial source rock sequences ; sedimentary facies of terrestrial basins are deposited in a ring formation. the best source beds are the continental source beds which contain dark shale

    陸相沉積以河流湖泊相為主，其基本特徵有：長期快速沉降的湖相沉積盆地是陸相生油的發育區；陸相湖盆的沉積相帶大都是環狀分佈，暗色泥巖是最佳生油層。
  9. Some thin beds of layered sandstone and dark grey siltstone show slump structures.

    一些薄層砂巖和暗灰色粉砂巖顯示出滑動構造。
  10. The maria are circular depressions covered with dark, loosely packed material-not solid rock.

    「月海」是圓形窪地，覆蓋著暗色的鬆散物質，而不是堅硬的巖石。
  11. In situ deposits are dark shale with horizontal bedding

    原地沉積為水平層理發育的暗色泥板巖。
  12. The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic

    盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖；三疊系雜色砂礫巖、砂巖及灰色泥巖（下紅上灰） ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。
  13. Wenquan granite is composed of two end - member rocks, one is the host rock of the acid end - member, and the other is the microgranular mafic enclave

    摘要溫泉花崗巖體由酸性端元的寄主巖石和暗色微細粒鎂鐵質包體群及基性巖墻群組成。
  14. The rule represents the tectonic evolution feature ' s controling to the depositional infilling styles and facies " distribution. in dawan area, the top and the middle strata of the shahejie formation also developed a set of fan - delta sediment similar to the bottom of the shahejie formation, but the scale is significantly smaller

    本區主要發育了兩套烴源巖，即沙三中段的暗色泥巖和沙三上段的煤系地層，它們在工區的兩個主要生油窪陷?於家房子窪陷和黃沙坨窪陷都有分佈，且厚度巨大。
  15. Oil - source correlation analysis has shown that the oils were mostly from ed2 source rocks from the bozhong depression, and the oils occurred in the slope hidden hill belt were from es3 or / and es, source rocks in the bozhong depression

    油源對比結果表明東斜坡帶東營組原油來源於渤中凹陷ed _ 2暗色泥巖，斜坡潛山帶原油來源於渤中凹陷es _ 3或es _ 1生油巖。
  16. The main achievements are : i. the main gas source rock in xujiaweizi depression is deep color shale of k ^ ^

    論文主要成果及認識有： 1徐家圍子斷陷主要氣源巖為沙河子組營城組暗色泥巖。
  17. With the tectonic uplift of the source area and the climate turning dry, the coal forming period was over, the fluvial system and fluvial - delta system became to play a major role. based on the study of former researchers and the theory of deep basin gas reservoir forming, the deep basin gas trap in the ordos basin is analyzed and is supposed to form in the ramp of the basin. it is supposed that the hydrocarbon of the deep basin gas trap is mainly composed of coal, carbonate and carbonaceous shale and with the " upper water seal " in the north of the study area the g

    根據深盆氣成藏理論和前人的研究成果，分析了深盆氣藏的分佈類型，認為鄂爾多斯盆地深盆氣藏屬于盆地斜坡成藏類型；認為深盆氣的源巖以煤、炭質泥巖、暗色泥巖和碳酸鹽巖為主；北部氣水倒置、東部露頭區有天然氣逸出；氣藏具有多重壓力系統；成藏機理主要是氣體動態的運移與聚集，穩定的構造背景有利於氣藏的大面積保存。
  18. Were found in the margin around the basin. lucaogou fm. was mainly composed of thick dark mudstone, micritic limestone, argillaceous dolomite, which reflected a shallow to fairly deep - lake sedimentary formation

    蘆草溝組在盆地內部發育厚層暗色泥巖、泥晶灰巖、泥質白雲巖等，反映陸相淺一半深水沉積建造。
  19. The column of salt and gypsum rock that are interbeded with black mudstone are developed 3 ( superscript rd ) - 4 ( superscript th ) sub - member of shaheje formation of lower tertiary in dongpu depression

    摘要在求濮凹陷下第三系沙三段發育暗色泥巖與鹽巖和膏鹽巖的頻繁互層沉積，暗色泥巖為深水成因。
  20. Carboniferous strata, more than 1000m in thick in the area of hexi corridor to bayan haot basin, is the coal measures of transitional phase, in which there are three kinds of hydrocarbon source rocks including dark mudstone, limestone, coal and carbonaceous mudstone

    摘要河西走廊至巴彥浩特盆地地區石炭紀地層厚逾千米，是一套海陸交互相含煤巖系，發育暗色泥巖、灰巖、煤層及碳質泥巖等3大類烴源巖。
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