鹽類巖 的英文怎麼說

中文拼音 [yánlèiyán]
鹽類巖 英文
salinastone
  • 鹽 : 名詞1. （食鹽; 鹽類） salt 2. （姓氏） a surname
  • 類 : 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...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 鹽類 : e. salt
  1. The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems

    五道梁群湖相碳酸鹽巖分為生物粘結灰巖（疊層石） 、泥晶灰巖、顆粒灰巖與泥晶白雲巖四大類，反映出沉積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。
  2. The fossils of algae, ostracoda, foraminifera, gastropod and polychaeta were found in the tertiary carbonate beds in the west of chaidamu basin

    摘要柴達木盆地西部第三系的碳酸鹽巖層中發現有藻類、介形蟲、有孔蟲、腹足類、多毛類等化石。
  3. Dongpu sag is of the superior geological conditions for forming deep gas pools, including two sets f premium source rocks, variety of sand bodies, sell developed porosity and thick halite and mudstone as cap rocks

    摘要東濮凹陷具有形成深層氣的優越基礎地質條件：兩套優質烴源巖、多種類型的儲集砂體和高異常孔隙發育、厚的巖鹽和泥巖作為良好蓋層。
  4. In middle and late periods of the early permian, the pre - caspian areas rose successively, the climate became dry, and the environment turned to be supratidal zone ( evaporitic environment ), resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite

    早二疊世中後期由於持續構造抬升，盆地氣候變得乾旱，海水變淺，潮上帶蒸發環境發育，以致這一時期廣泛發育鹽類沉積，形成含鹽層系，主要由鹽巖和硬石膏層構成，並形成許多大小不等的鹽丘構造。
  5. 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種主要沉積相類型，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，扇三角洲相粗碎屑巖由北向南進積;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鹽類沉積。
  6. The high content and the high water temperature favour the solution of salt and metals from the underground formations.

    高含量和高水溫促進了地下巖層里鹽類和金屬的溶解。
  7. The determinative characteristics of common rock forming minerals containing quartz group, feldspar group, mica group, hornblende group, pyroxene group, olivine group and carbonatite minerals will be discussed in greater detail

    對常見造巖礦物，如石英類、長石類、雲母類、角閃石類、輝石類、橄欖石類、碳酸鹽類礦物的鑒定特徵將予以詳細的說明。
  8. From studies of these characteristics of structures, palaeontology, drilling, well logging, seismic profile, salt chemistry and lacustrine sedimentary system, it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag, and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area

    通過該區構造、古生物、鉆井、測井、地震、鹽巖化學及湖盆內沉積體系等特徵的研究，認為淮陰凹陷浦口組二段和三段的沉積構造有其特殊性，巨厚的鹽巖層是殼深部鹽類物質沿深大斷裂上涌以熱鹵水形式進入湖盆的結果。
  9. The gangue minerals are mostly carbonating minerals, fluorite, barite, celestite and so on ; the rock alteration is slightly silicified, carbonated, baritizated, celestited, which is low - temperature alteration. because of continual downgoing extrusion from india plate to euro - asian plate, there are some thrusting nappe structures in lanping basin related to the orogens on the two sides

    礦床中礦石礦物發育典型的中低溫熱液成因的礦物組合，如黝銅礦系列、方鉛礦、黃銅礦等，脈石礦物主要為碳酸鹽類礦物、螢石、重晶石、天青石等；圍巖蝕變主要發育弱硅化、碳酸鹽化、重晶石化、天青石化等低溫蝕變組合。
  10. The bareness area of carbonate rock of southwest china is 41. 05 + 1004km2, it is the biggest karst continuum strip

    我國西南地區碳酸鹽類巖石出露面積達41 . 05萬km ~ 2 ，是世界上最大的巖溶連續帶。
  11. The greatest dependence upon temperature is shown by rocks with high conductivities at room temperature e. g. salt.

    在室溫下，高熱導率巖類（如鹽類）的熱導率對溫度的反應最大。
  12. As is known that the water in the rock contains a mount of salt, and the kind and content in turn make the water freezing temperature variable. on the ot her hand, rock material will shrink when frozen, and expand when warmed

    主要是由於巖石中的水融有一定量的鹽類物質，鹽類物質的存在及其含量的差異使的水分的冰點具有一定的可變性，而巖石材料本身具有熱脹冷縮的性質。
  13. The deposit is contained in the predominantly calc-silicate upper part of the corella formation.

    礦床位於科雷拉巖繫上部主要為鈣質-硅酸鹽類的巖層中。
  14. The hydrological condition of danjiang reservoir is very complex, where carbonate rock distribute in the canyon areas, and a series of funnels are formed

    丹庫區水文地質條件復雜，在峽谷庫段，碳酸鹽類巖石裸露，巖溶裂隙水活動形成一系列落水洞、漏斗和溶洞。
  15. New estimates of carbonate and silicate weathering fluxes and associated with co _ ( 2 ) consumption budget were given in the major drainage basins of china where previous information was indeed limited. an attempt was also made to calculate chemical weathering rates of silicates and carbonates per unit area

    中國主要流域盆地巖石化學風化的年均大氣co :消耗量1375 . 91x109mol （佔世界巖石風化年均消耗co :總量的6 . 55 % ） 、轉移的碳量為1 . 65又107t碳，其中碳酸鹽和硅酸鹽類化學風化消耗的大氣co :量分別佔85 %和15 % 。
  16. The paper focused on consumption of atmospheric co _ ( 2 ) through rock weathering and weathering reactions what were attributable for dissolved loads in the major basins of china. generally, dissolved loads were preferentially considered to evaluate chemical weathering relative to river - borne particulate / sediment because they are directly from source rock weathering

    中國主要流域盆地巖石化學風化的大氣co :消耗率通常較高，而且中國主要流域盆地整體上碳酸鹽類的風化溶解對河水化學的影響程度明顯強于硅酸鹽類，這是中國主要流域盆地較為突出的特徵。
  17. Test of carbonate rock sample ' s dissolution reveals that lithology ' s effects on dissolution mainly lie on their different start - up dissolution velocities

    摘要對碳酸鹽巖類巖石樣品的溶蝕試驗表明，巖性對溶蝕的影響主要表現為各類巖石在啟動溶蝕速率上的差異。
  18. At the same time watertight rock surround the carbonate rock, which is helpful to water percolate deeply and trigger earthquake

    同時，峽谷區碳酸鹽類巖石周圍又有弱透水和微透水的巖層包圍著，有利於庫水向深部滲透，誘發地震。
  19. Therefore the salt crystals mined from the deep of the mountains are pure and untouched by pollution

    同類巖鹽水晶只有在波蘭及喜馬拉雅山被發現。
  20. Carbonate area gets to 41. 05x 104 km2 in southwest china. it is the maximal continuum of karst mountain in the world. the dimensionality area is about 82. 4 thousands km2 in chongqing region

    我國西南地區碳酸鹽類巖石出露面積達41 . 05x10 ~ 4km ~ 2 ，是世界上最大的巖溶連續帶。
分享友人
分享到 Line

分享到臉書