晚二疊紀 的英文怎麼說

中文拼音 [wǎnèrdiě]
晚二疊紀 英文
grauliegendes
  • : 名詞1 (晚上) evening; night 2 (姓氏) a surname Ⅱ形容詞1 (時間靠後的; 遲) far on in time; la...
  • : Ⅰ數詞(一加一后所得) two Ⅱ形容詞(兩樣) different
  • : 紀名詞(姓氏) a surname
  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-奧陶為其烴源巖形成的重要時期;早奧陶世末-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;早期的構造變形使古油藏遭受進一步的破壞;后構造變動主要以調節為主。
  2. Evolution of junggar late carboniferous - permian foreland basin

    準噶爾石炭世一前陸盆地的演化
  3. This basin had undergone three phases, the rifting phase in permian, the depression phase from mesozoic to early neozoic and the phase which formed the intermountain basin by thrusting reformation latter neozoic

    盆地演化經歷了裂谷盆地、中生界至新生界代早期的陸內坳陷盆地和新生代期的逆沖改造山間盆地三個階段。
  4. ( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian, late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic. structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave. most traps in the area formed or typed at last in the himalayan episode, dispersed on the north and south belts

    ( 4 )研究區構造與地層不整合圈閉的形成和發育受志留-泥盆世-第三、漸新世-第四三個擠壓階段的控制;早古生代主要發育非構造圈閉和復合圈閉,古生代和新生代則主要發育構造圈閉:構造圈閉主要發育在南北兩帶上,其次為中帶;非構造圈閉主要發育在和田凹陷以北的地區;研究區內大多數圈閉是喜山期形成或最終定型的,在南北兩帶都有分佈,而海西期圈閉主要分佈於研究區中帶瑪南構造帶處。
  5. Through research, the organic matter of source rocks in carboniferous - permian coal measure strata began first hydrocarbon - generating in mesozoic, and the first hydrocarbon - filling took place. but, because of yanshan movement later, the carboniferous - permian strata rose, as a result, the first hydrocarbon - generating and reservoir - forming paused ; in early tertiary period, because carboniferous - permian strata dipping forward east originally turned into dipping forward west, the prototype of faulted block began to form gradually ; by the end of sha - 3 period of early tertiary, the paleogeotherm of carboniferous - permian strata exceed the mesozoic ' s temperature again, and accordingly, abundant hydrocarbon was generated and expulsed secondly. the trap continued to develop ; from the end of late tertiary to quaternary, the second hydrocarbon - generating and expulsing got to its peak, and the second reservoir - forming was over

    研究表明,本區石炭?烴源巖在中生代發生一次生烴和排烴,並有油氣充注,后因燕山運動導致地層抬升,一次生烴和成藏過程中止;在早第三,原來東傾的地層變為西傾,斷塊圈閉開始具雛形;至早第三末期,石炭?系的大部分地層古地溫再次超過中生代一次生烴的溫度,開始次生烴和排烴,圈閉持續發育;第三末?第四次生烴、排烴達到高峰,次成藏完成。
  6. According to the analysis of the structure deformation variant direction the structure superposition during late period, and the tectonic stress field and deformation variant field, the cover extended nearly sn direction in early stage ( d - c ), maybe changed the direction in pernian ( especial the late permian ), and developed some new half - graben along sn direction except the succession activity at great fault zone. the direction of compression deformation variant, however, was nearly sn direction in indo - chinese epoch, ne - sw direction in early yanshan movement epoch, nne - ssw direction in late yanshan movement epoch, and transformed from ew to sn direction in himalayan movement epoch

    根據不同構造層中變形方向及後期構造加的分析,對本區的構造應力場及變形場進行了探討,本區蓋層早期階段( d - c )為近南北向的伸展拉張,(特別是世)的伸展方向可能發生了改變,除在各斷裂帶繼承性活動外,沿南北方向又新生了一些半地塹。而在擠壓變形時,印支期主要為近南北向擠壓,燕山早期為nw - se向擠壓,燕山期為nne - ssw向擠壓,而喜山運動可能經歷了從ew向向sn向方向擠壓的轉變。
  7. From the late carboniferous to the end of permian, the spores of the shishuyuan trough were from the north china province, and the marine sediments were absent in the southern part of eqm

    石炭世至末,柿樹園海槽的孢子見于華北生物省,東秦嶺南部缺乏海相沉積。
  8. In the late permian and triassic, the basin underwent once again a large - scale transgression, and the depositional environment was shelf sea with delta locally

    世三盆地又經歷了一次大的海侵, ?淺海陸棚環境,局部?海陸過渡三角洲相。
  9. The large - scale composite ductile shear zone around laerdun daban is analyzed into three stages including horizontal dispatch, uplift by compression and magrnatic intrusion, and dextral strike - slip ductile shearing, respectively of late early paleozoic to early late paleozoic, late devonian, and permian - triassic ages

    摘要拉爾敦達坂一帶發育的大型復合式韌性剪切帶,經解析分為水平拆離、擠壓和巖漿侵入隆升、左行走滑韌性剪切三個不同階段,變形時限分別限定在早古生代期至古生代早期、泥盆世和
  10. By studying deposit ' s geochemical features, it is believed that mineralizing metals came from d3 and c1 stratums ; ore - forming fluid is atmosphere water ; mineralizing era is later permian ; sulphur came from seawater sulfate ; and it is a low - middle temperature deposit. emeishan basalt provided heat impetus without providing mineralizing metals

    通過對礦床地球化學特徵的探討,認為上泥盆統及中下石炭統地層提供了成礦物質;成礦溶液為大氣降水;成礦時期為期;礦床的硫主要來自海水硫酸鹽;礦床的成礦溫度為低-中溫。
  11. The source rocks of carboniferous and early periman generated oil in middle triassic. the source rocks in middle periman reached the oil threshold in mid - late jurassic. the source rocks in jurassic hav n ' t reached the oil threshold

    石炭系、下統烴源巖於三中期成熟,中統烴源巖于侏羅中?期成熟,侏羅系煤系烴源巖未進入生油門限。
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