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sedimentary strata中文是什么意思

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  • Simple disconformities between adjacent sedimentary strata (4) record time breaks in the succession .
    相鄰沿積間的簡單的假整合(4)記錄著時(shí)間序列上的間斷。
  • Simple disconformities between adjacent sedimentary strata ( 4 ) record time breaks in the succession
    相鄰沿積間的簡單的假整合( 4 )記錄著時(shí)間序列上的間斷。
  • Distribution characters and exploration potential of mesozoic sea facies sedimentary strata in the south china sea basin
    南海盆地中生代海相沉積地層分布特征及勘探潛力分析
  • The qiangtang basin , having the most complete and extensive marine sedimentary strata during jurassic , is the second larger mesozoic marine sedimentary basin
    藏北羌塘盆地地處青藏高原腹部,是我國中生代第二大海相沉積盆地,侏羅系是羌塘盆地發(fā)育最全、分布最廣泛的海相沉積層系。
  • Thirdly , by comparing with holocene strata of the coastal plain of shandong peninsula , sedimentary strata of this area are divided into four layers , and sedimentary environments are comfirmed
    再次,通過與山東半島濱海平原全新統(tǒng)地層進(jìn)行對比,對本沉積區(qū)地層進(jìn)行劃分并確定各層沉積環(huán)境。
  • According to the characteristic of sedimentary stratum and the study of geochemistry in binbei area , source rocks of each layer become thicker from north to south . source rocks of south depressed center heiyupao , south wuyuer sunkeness and other area on the binzhou railway are best development
    根據(jù)濱北地區(qū)地層的沉積特點(diǎn)和地球化學(xué)研究,各層源巖表現(xiàn)為從北向南逐漸增厚,其中黑魚泡凹陷中部以南、烏裕兒凹陷南部、臨近濱州線的其它地區(qū)源巖發(fā)育最好。
  • The qiantang basin , having the most complete and extensive marine sedimentary strata during jurassic , is the second larger mesozoic marine sedimentary basin . although many achievements are obtained in recent years , the research are still only involved in second - or third - order of mesozoic sequence . on the base of sedimentation facies analysis of matuo formation , high frequency sequence are studied
    藏北羌塘盆地地處青藏高原腹部,是我國中生代第二大海相沉積盆地,侏羅紀(jì)是羌塘盆地發(fā)育最全、分布最廣泛的海相沉積層系近年來,羌塘盆地在層序地層方面的研究已取得不少成果,但其層序地層研究多涉及中生代二級或三級層序,至于高頻層序,尚未進(jìn)行詳細(xì)的研究。
  • By studying the lithologjcal and mineral parameters ( pebbled elastics percent ratio , clastic maturation index , heavy crop stability factor ) of mesozoic sedimentary strata , the result shows that the northern boundary of present basin is near to the boundary of original basin and the moving distance of elastics is short , but the southern boundary of present basin is far from the boundary of original basin and the moving distance of elastics is long . the fades of northern basin are mainly delta fades and the fades of middle and southern basin are lacustrine fades
    通過對盆地中生代沉積地層中各種巖礦參數(shù)(碎屑巖含礫百分比、碎屑成熟度指數(shù)和重礦物穩(wěn)定系數(shù))分析和綜合研究認(rèn)為,今盆地北部距離原始盆地沉積邊界較近,碎屑物搬運(yùn)距離較短;南部距離盆地古沉積邊界較遠(yuǎn),沉積物搬運(yùn)距離較遠(yuǎn);中生代盆地北部主要為三角洲沉積相,中南部為湖泊相沉積。
  • The lower paleozoic continent marginal sedimentary strata in the north kunlun massif are sinian - cambrian alajiaoyi group and ordovician pishigaisayi formation . the former is composed of high maturity flysch deposit , the later consist of continental shelf deposit such as carbonate and slate and sandstone . these rocks implies that they might form at passive continental margin
    與其曼于特蛇綠巖相關(guān)的早古生代邊緣沉積巖在昆北地塊上為震旦?寒武系阿拉叫依巖群、奧陶系皮什蓋薩依巖組,前者為一套成熟度較高的陸源碎屑復(fù)理石沉積,后者為碳酸鹽巖和含碳板巖砂巖等陸棚沉積,顯示其具被動(dòng)陸緣性質(zhì)。
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