生物地層標志 的英文怎麼說

中文拼音 [shēngdecéngbiāozhì]
生物地層標志 英文
biostratigraphic index
  • : Ⅰ動詞1 (生育; 生殖) give birth to; bear 2 (出生) be born 3 (生長) grow 4 (生存; 活) live;...
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • : 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...
  • : Ⅰ名詞1 [書面語] (樹梢) treetop; the tip of a tree2 (枝節或表面) symptom; outside appearance; ...
  • : Ⅰ名詞1 (志向; 志願) aspiration; ambition; ideal; will 2 (文字記錄) records; annals 3 (記號)...
  • 生物 : living things; living beings; organisms; bios (pl bioi bioses); biont; thing; life生物材料 biol...
  • 標志 : signmarksymbolhallmarkblipemblemdenotationtagensignflagattributemarkerbrandstypeindex
  1. This study is a post - cruise study of this leg, calcareous nannofossil samples from sites 1146, 1147 and 1148 of leg 184 were analyzed to provide a high - resolution biostratigraphy for this leg and to investigate morphological variation of coccolith genus gephyrocapsa. the main results of this study are : 1. 12 late pliocene to pleistocene bio - events were recognized and 6 zones of martini ( 1971 ) were determined for the upper sediment sequences of sites 1146 and 1148

    本文作為大洋鉆探項目船下后續研究的一部分,對184航次中的1146站位和1147 、 1148站位的樣品進行了分析和研究,在船上科學家已經建立起的框架的基礎上進一步加密采樣,對事件化石類別進行數量統計,進一步確定了12個事件在鉆孔中的深度,建立起了兩個站位的高解析度的鈣質超微化石框架。
  2. The thesis analysises the typical model profile and the special rock profile of wudaoliang group of miocene epoch in hoh xil basin. and be used the biocalcarenite with the marl rock take the marker bed of wudaoliang group

    論文對可可西里盆中新世五道梁群的典型剖面和特殊巖性剖面進行了分析,並以泥灰巖和碎屑灰巖作為五道梁群的
  3. The paper adopts some methods such as gas composition, carbon isotope, systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas, illustrates that natural gas from the section of jialingjiang formation is mainly attributed to sapropel type organic matter gas of permian, comes from carbonatite hydrocarbon rocks permian which most of them are overmature, its main gas source has nothing to do with carbonatite hydrocarbon rocks of jialingjiang formation themselves, presents in geochemistry characteristics of oil type cracked gas

    摘要通過對川中川南過渡帶西部的磨溪潼南區嘉二段天然氣組成、碳同位素組成、高演化天然氣儲瀝青化合的系統分析測試和混合成因氣的定量估算,闡明了該區嘉二段天然氣主要屬於二疊系腐泥型有機質成因氣,來源於二疊系過成熟為主的碳酸鹽巖烴源,主力氣源與嘉陵江組自身的碳酸鹽巖烴源無關,並具有油型裂解氣的球化學特徵。
  4. Biostratigraphic zonation and mark - fossil erection should be based on restoring evolutionary pedigrees or occurrence sequences, and the boundary should be confirmed at the horizon of their " first appearance "

    學研究一定要以恢復演化譜系或發序列為基礎,界線化石應該選在其「首現」位。
  5. Their distribution of deposition control lithology subtle trap, die - out around paleo - uplift the distribution of subtle traps in the slope, subtle trap forms along faults and above and beneath unconformity boundary. through exploring and studying in huanghua depression many years, we gradually summarize a series of methods and technologies for subtle trap exploration, they are precise stratigraphy correlation on the basis of sequence stratigraphy, including micromarker correlation, element logging, high frequent cycle stratigraphy and precise sequence stratigraphy, besides conventional biography stratigraphy, logging correlation. through using facies analysis method, the type and distribution of reservoir are determined

    在黃驊坳陷通過多年的摸索和引用,逐漸形成了一套系統的隱蔽油氣藏的研究方法和技術,它們是以學為代表的精細劃分方法,用來解決劃分及歸屬問題,除常規的學、巖電特徵對比方法外,創新性的運用了包括微劃分方法、元素測井方法、高頻旋迴對比方法及精細劃分方法等四種精細劃分方法。
  6. The results are shown as the followings : on the basis of studies of depositional environment of source rock and its petroleum potential assessment, the biomarker compositions of the five source beds ( hq, j2k, jiy, tjt, tsh ) in kuche basin are analyzed in detail and the effects of depositional environment and maturity on the biomarker compositions are also discussed. the results show that there is not clear correlation between the distribution of biomarker composition and the ages of triassic and jurassic. it is proposed for the first time in the kuche basin that the changes of biomarker composition in the coal can be classified into three stages with the maturity, and the regular changes of different biomarker parameters in the coal are revealed

    以烴源巖沉積環境為背景,詳細剖析了庫車前陸盆五套烴源( j _ 2q 、 j _ 2k 、 j _ 1y 、 t _ 3t 、 t _ 3h )中煤、炭質泥巖、湖相泥巖、煤系泥巖的組成特徵,分析了沉積環境、成熟度對組成的影響,指出同一烴源在盆不同組成的差異,並認為組成特徵與三疊系和侏羅系的時代對應關系不明顯。
  7. It appears that biodegradation, oxidation and water washing near the surface are not responsible for the high density and high viscosity of these deep viscous heavy oils, in addition, biomarker parameters demonstrate maturities of these viscous oils are relatively low to that of the normal oils derived from the es3 source rocks in this area

    這表明這兩個區深稠油屬原稠油,不是由於降解、表氧化、水洗等次作用形成的。成熟度指顯示稠油具有中低成熟度,相對低於來源於沙三段源巖稀油成熟度。
  8. This paper reviews current development in researches of the field of microbial diversity in polluted soils at home and abroad based on the methods of isolating culture and biomarkers, and the knowledge of microbial diversity from the angles of different ecological levels, and explores advanced approaches, new ideas and issues in the research on soil microbial ecological processes aiming at new problems in soil pollution the world is faced with

    本文基於分離培養以及分子方法,從不同次上認識微多樣性,較全面、系統綜合評述國內外污染土壤環境的微群落功能、結構及分子遺傳多樣性的研究進展,並針對新形勢下土壤污染所面臨的新問題,探討了近期土壤微態學過程研究的重要手段與科學問題。
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