斷層巖 的英文怎麼說

中文拼音 [duàncéngyán]
斷層巖 英文
fault rock
  • 斷 : Ⅰ動詞1 （分成段） break; snap 2 （斷絕;隔斷） break off; cut off; stop 3 （戒除） give up; abstai...
  • 層 : i 量詞1 （用於重疊、積累的東西 如樓層、階層、地層） storey; tier; stratum 2 （用於可以分項分步的...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 斷層 : fault; slip; slicle; fracture; dislocation
  1. 2. tazhong ancient uplift originated from normal fault in paleozoic, hydrocarbon formed in ordovician period, structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period, and it provided geologic background for the deposit of silurian - devonian stratum. tazhong uplift formed at the end devonian, ancient reservoir was destroyed and asphaltum sandstone formed, structure deformation more destroyed ancient reservoir in early permian, after then the major of structure deformation is regulation

    塔中隆起源於早古生代拉張背景下的正斷層，寒武-奧陶紀為其烴源巖形成的重要時期；早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期，同時也為志留系形成地層及復合圈閉提供了古地理背景；志留?泥盆紀塔里木盆地南北緣均轉為活動大陸邊緣，形成了大量的斷裂和不整合；泥盆紀末塔中鼻狀隆起基本定型，古油藏遭受破壞，形成了瀝青砂巖；早二疊世晚期的構造變形使古油藏遭受進一步的破壞；二疊紀后構造變動主要以調節為主。
  2. When the rock mass of dam abutment is enclosed by faults, joint fissures and bedding planes, it is necessary to carry out holistic anti - slide stability analysis in order to make the abutment withstand potential slide

    摘要當拱? ?肩巖體為斷層、節理裂隙、層面等結構面所圍成，有可能產生滑移時，就應進行整體抗滑穩定分析。
  3. You will enjoy these breathtaking sights : tunnel view, bridal veil fall, el captain, merced river, yosemite fall, half dome

    公園內著名景緻區如下新娘面紗瀑布，船長巨巖，昆仲斜巖石，金沙江，觀瀑橋，半球巨巖，斷層飛瀑，
  4. Arrive in yosemite national park after lunch. highlights include : tunnel view, bridal veil falls, el captain, merced river, yosemite falls, half dome. overnight stay in fresno

    公園內著名景緻區以次如下新娘面紗瀑布，船長巨巖，昆仲斜巖石，金沙江，觀瀑橋，半球巨巖，斷層飛瀑，南眺景等。
  5. You will enjoy these breathtaking sights : tunnel view, bridal veil fall, el captain, merced river, yosemite fall, half dome. the day ends with an overnight stay in central california s top city : fresno

    公園內著名景緻區以次如下新娘面紗瀑布，船長巨巖，昆仲斜巖石，金沙江，觀瀑橋，半球巨巖，斷層飛瀑，南眺景等。
  6. The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement

    其後的繼承性活動在斷裂帶內形成碎裂程度最強達到碎裂巖的碎裂巖系列構造巖，變形帶兩側發育兩組典型的共軛剪節理；第二次在晚白堊世?始新世，斷裂在北東?南西向近水平擠壓作用下右行張扭性活動，斷裂帶兩主斷裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶，而斷裂在巖體區也發育兩組典型的共軛剪節理，斷裂內形成初碎裂巖為主的構造巖；第三次是喜山期以西側抬升、東側下降的強烈升降為主的活動，在基巖中，主斷層兩側圍巖出現微破裂。
  7. In this case during paleozoic, nearly east west trending arc structures resulted from the interaction between china plate and siberian plate. in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault, diaoyudao fault, okinawa fault, uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate

    本文所涉及近東西向展布的弧形構造形成於古生代時期中國板塊與西伯利亞板塊的碰撞帶，而在中生代，中國板塊下的kula - pacific板塊向西俯沖導致了北北東向和北東向構造（如duimadao斷層、 diaoyudao斷層、 okinawa斷層、隆起帶和沉降帶）以及位於中國板塊東部的火山巖漿帶。
  8. The parefin 4 chromite claims near the northern end of the csardas thrust again indicate the eastward extension of the thinning ultrabasic sheet from railway block.

    靠近薩達斯沖斷層北端的帕勒芬4鉻礦區又表明從鐵路段向東超基性巖席減薄的情況。
  9. It may be gouge of finely comminuted rock material with perhaps large blocks of the harder rocks embedded in it.

    可能是磨碎的巖層物質組成的斷層流，並夾雜一些大塊堅硬巖石。
  10. Many ultrabasic bodies in the orogenic association occur along strike faults, which gives a simulated concordant relationship.

    與造山運動共生的許多超基性巖體沿著走向斷層出露，表現出假的整合關系。
  11. This paper puts forward the showing ways and the modeling algorithms for the familiar geologic bodies such as terrane, fold and faultage

    本文主要對常見的地質對象，如巖層面、褶曲、斷層面等，提出了它們的表示方法和建立它們的三維模型的演算法。
  12. On the east terrace - fault slope of the depression, the sedimentary mode of fan - shaped delta - slump turbid fan - deep lake facies are developed. on the long axial direction of fula depression, the southeastern groove was filled with a large scale delta which was the main sources, the other little delta limited by the 3 syndepositional fault was distributed down the slope edge of the northern sub - depression. this stage developed a favorable oil sources, reservoir and regional seal which formed the good matching relations of generation, reservoir and seal in the time - space zone

    Abugarbra組的sc和sd層序發育在邊界斷層和同沉積斷層活動劇烈、湖盆擴張期，凹陷中心發育半深湖-深湖相沉積，在凹陷陡坡發育近岸水下扇，斷階緩坡帶發育扇三角洲?滑塌濁積扇?深湖相組合，長軸凹槽和北部次凹的北部緩坡帶發育三角洲體系，此層位是有利生油層和巖性圈閉發育層段。
  13. It is the regional structure stress field formed in the processes of formation of the major faults of buried hills action on the graben that controlled the development of the fractures of sandstone of mesozoic of baigezhuang region

    正是壘塊上古潛山內幕主要斷層形成過程中的局部構造應力場，控制形成了柏各莊地區潛山中生界砂泥巖中裂縫的發育。
  14. The study area is composed of sandstone & conglomerate reservoir of alluvial fan & fan delta, which belong to sha3 lower member and sha4 upper member of lower tertiary of yong " an town oilfield in dongying depression. the target stataum develops in the hanging wall of the synsedimentary fault in the scarp zone of dongying depression. the frequently intense movements result in the variation of sandstone and conglomerate reservoir and the evolution of the time and space of sha3 lower member and sha4 upper member in yong " an town oilfield

    研究區是東營凹陷永安鎮油田沙三下段、沙四上段的沖積扇和扇三角洲砂礫巖體，目的層發育在東營凹陷陡坡帶同生斷層的下降盤，因斷層多期強烈活動，導致永安鎮油田沙三下段、沙四上段的砂礫巖體成因類型多，時空演化變化大，在扇根一帶小層對比難度大，給油田開發帶來很大的難題，在這種背景下進行流動單元研究難度更大。
  15. Based on the regional structure dynamics analysis of the lithosphere imbricate structure in lanping - weixi area, the middle section of three - rivers area ( n26 - 28 ), the bouguer gravity anomaly of deep structures was completed and the fractal of these faults was calculated. the geology structure model and the elasticoplastic three - dimension finite - element mathematic are described, made and calculated ; and physical simulation was accomplished

    針對三江中段n26 - 28蘭坪-維西地區的巖石圈正交疊加構造的區域構造動力學分析，進行了深部構造的布格重力異常延拓處理和淺部的斷層分維計算，描述、製作計算了地質結構模型、彈塑性三維有限元數學模型和物理模擬。
  16. Two oil layers are mainly fault and lithologic deposit

    兩套油層主要為斷層巖性油藏。
  17. Near the faulty step - break, low stand system developed, and some sediment system distribute broad, such as alluvial fan, low stand wedge, low stand fan, and so on. the sand body can form not only the trap of dying out upward and sand lens, but also fault - iithology trap. the study shows that fault - lithology trap is most important trap style in study area especially sha - 3 formation

    斷階坡折附近是低水位體系域發育的重要場所，常發育沖積扇、沖蝕作用的下切河道以及低水位楔狀體、低水位扇體等沉積體系，這些砂體不僅具有形成上傾尖滅或砂巖透鏡體圈閉的條件，而且可形成斷層?巖性圈閉。
  18. To understand the control action of bedding faults during the formation of hydrocarbon accumulations, an experimental analysis on sealing capacity of bedding fault rocks was performed

    摘要為了解順層斷層對油氣成藏的控製作用，實驗研究了順層斷層巖的封閉能力。
  19. According to paleo - geomorphology and depositional systems analysis, three kinds of forming models of subtle traps were built. they are fan - delta front - slope - sliding turbidity subtle traps n sub - fan near fault - stepping faults - turbidity subtle traps and fan - delta - furrow - sub - fan - sliding turbidity subtle traps

    綜合分析表明，臨南窪陷具有有利的油氣成藏條件，發育有上傾尖滅型隱蔽油氣藏、透鏡體隱蔽油氣藏、斷層-巖性隱蔽油氣藏等隱蔽油氣藏。
  20. Based on these, this paper studied deeply the main factors controlling accumulation and distribution of oil or gas and accumution models through studying types of oil or gas reservoirs and oil or gas distribution laws of f, y oil layers in the north of songliao basin. this paper pointed out sourcerocks, caprocks, faults and hydrodynamics power to be the main factors controlling oil or gas accumulation and distribution. there are - two models of oil or gas accumulating in fault - lithology or fault block traps through migrating downward under the regional caprock and oil or gas from sourcerock downward accumulating in fault - lithology or fault block traps in reservoirs upward by migrating through fau lts

    在此基礎上，通過對松遼盆地北部扶、楊油層油氣藏類型及分佈規律分析，深入研究了扶、楊油層油氣成藏與分佈的主控因素和成藏模式，指出源巖、蓋層、斷裂和水動力是松遼盆地北部扶、楊油層油氣成藏與分佈的主控因素，具有被下油氣倒灌運移于斷層?巖性或斷塊圈閉成藏和下生上儲天然氣沿斷裂運移斷層?巖性或斷塊圈閉成藏二種模式。
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