晚二疊世 的英文怎麼說

中文拼音 [wǎnèrdiěshì]
晚二疊世 英文
late permian epoch
  • 晚 : 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...
  • 二 : Ⅰ數詞（一加一后所得） two Ⅱ形容詞（兩樣） different
  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. Conodont fauna of late permian to early triassic in leping area, jiangxi province conodont fauna of late permian to early triassic in leping area, jiangxi province

    江西樂平地區晚二疊世-早三疊世的牙形石動物群
  3. According to the fossils, we found one graptolite zone : mongraptus yukonensis - neomongraptus himalayensis zone ; two radiolarian combinations : entactinia - entactinosphaera, entqctinia itsukaichiensis combination, and three radiolarian zones : albaillella paradoxa zone, albaillella indensis zone and albaillella cartalla zone. 2. the new cognition about the sedimentary environment of the original nanpihe formation

    放射蟲可建立兩個組合和三個化石帶：晚泥盆世entactinia - entactinosphaera組合；早石炭世杜內期中期albaillellaparadoxa帶，杜內期晚期?維憲期早期albaillellaindensis帶，維憲期中期albaillellacartalla帶；晚二疊世entactiniaitsukaichiensis組合。
  4. The copper, iron, nickel and silver deposits might be assigned to four metallogenic series : i. the metallogenic subseries of copper, molybdenum, gold, silver deposit related to late devonian - early carboniferous basic - intermediate - acid hypabyssal intrusive - eruptive rocks ; ii. the metallogenic subseriesof iron, copper, zinc deposits related to early carboniferous basic - intermediate - acid volcanic - intrusive rocks ; iii. the metallogenic subseries of copper, silver, iron deposits related to middle - late carboniferous basic - intermediate - acid volcanic - intrusive rocks ; iv. the metallogenic subseries of copper, nickel and platinum group deposits related to late carboniferous - early permian basic - ultrabasic rocks ; 3, division of regional major metallogenic belts on the basis of the previous work conducted and by following the principles, grounds and methods of the division of metallogenic belts, areas and fields, . in light of this, metallogenic belts of grade iv were divided

    1 、按照成礦系列理論的學術指導思想，將研究區華里西期銅礦床成礦系列劃分為四個成礦系列亞系列： 、晚泥盆?早石炭世延東?土屋?三岔口與中酸性巖漿侵入活動有關的cu 、 mo 、 au礦床成礦亞系列、早石炭世與巖漿作用有關的鐵、銅、金、銀礦床成礦亞系列、中石炭世與巖漿作用有關的cu 、 fe 、 ag 、 au礦床成礦亞系列、晚石炭世-早二疊世與幔源基性?超基性巖有關的銅、鎳、鉑族礦床成礦亞系列並從地層、巖漿巖、控礦構造、地球化學、成礦特徵等方面對各成礦亞系列進行了詳細論述。
  5. After late of early permian period, deposits of deltas and lacus took shape extensively along with up - lifting of yimeng area in the north and marine regression of this area

    早二疊世晚期以後，隨著北部伊盟地區不斷隆升，海水退出本區，研究區形成廣泛的三角洲和湖泊沉積。
  6. ( 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-泥盆紀、晚二疊世-第三紀、漸新世-第四紀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，晚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。
  7. Reefs are well developed in western hubei and eastern chongqing. through sedulous research, the whole acquaintance on types of reef builders, types of reef carbonatite, development and evolution of reef organisms, division of reef facies, distributing regularities of reefs and diagenesis has been concluded. according to the comprehensive studies, the following results and conclusions have been obtained

    通過對鄂西渝東區上二疊統長興組生物礁造礁生物、沉積相、成巖作用的研究，認清了礁體的主要造礁生物類型、主要巖石類型、生長演化、相帶劃分、分佈規律以及成巖作用，可以得出以下結論和認識： 1生物礁主要分佈於晚二疊世碳酸鹽臺地內部和臺地邊緣，可分為三種類型。
  8. 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疊加的分析，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，二疊紀（特別是晚二疊世）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，燕山晚期為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。
  9. 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

    晚二疊世三疊紀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。
  10. The stratum, deposited in nongba which in eastern part of gengma area and composed by sandstone, mudstone and silicate and tuff interlayers, was named by former man as nanpihe formation and papai formation, and their age were later permian and early triassic respectively

    耿馬弄巴地區出露一套以砂泥質巖為主體夾硅質巖、凝灰巖的地層，前人將它命名為南皮河組和怕拍組，並分別定名為晚二疊世和早三疊世。
  11. Substance sources of rare - earth elements in late permian coal seams on coal mines in bijie

    畢節煤礦區晚二疊世煤層稀土元素的物質來源
  12. Pa elements, this article described two important pa elements of

    鑒于在晚二疊世至早三疊世，
  13. Thermoevolutional characteristics of hydrocarbon generation from barkinite, late permian coals in shuicheng, guizhou province

    貴州水城晚二疊世樹皮體成烴的演化特徵
  14. The post - salt sediment group formed ( upper permian to quaternary ) is composed mainly of clastic rocks, with carbonates locally

    晚二疊世以後形成的鹽上層系沉積，主要?碎屑巖，在局部地區有碳酸鹽巖。
  15. Petrologically, new discovery includes a suite of the late permian - early triassic ophiolites in the southern part of the surveyed area and ophiolites in duolie, dagring village

    巖石方面，在測區南部新發現了一套晚二疊世一早三疊世蛇綠巖。
  16. The sedimentary environment of the early feixianguan age of early triassic in northeastern sichuan basin mainly inherited the pattern of the late changhsingian age of late permian

    摘要四川盆地早三疊世飛仙關早期的環境基本上繼承了晚二疊世長興期末的格局。
  17. Distribution patterns of the rare - earth element in coal are similar for the coals from the same district, and different for the coals of different districts

    同一礦區晚二疊世煤的稀土元素配分模式具有一定的相似性，而不同地區晚二疊世煤的稀土元素配分模式則差異較大。
  18. From csql to csq5, the barrier system was the main system. from psql to psq5, the carbonate ramp was the main system and from psq6 to psq8 the main system was fluvial and fluvial - delta system in brackish basin. from psq9 - psql2, the main system turned to the fluvial - delta system

    晚石炭世csq1 ? csq5層序以碎屑海岸障壁?瀉湖和碳酸鹽緩坡沉積體系為主；早二疊世早期psq1 ? psq5層序以碳酸鹽緩坡沉積體系為主，早二疊世晚期psq6 ? psq8層序以半鹹水盆地河流、河流三角洲沉積體系為主；中二疊世psq9 ? psq12為陸相沖積扇、河流、湖泊三角洲沉積體系。
  19. During the early stage of middle permian, the studied area is dominant, from north to south, of alluvial fans, braided stream, braided delta plain, braided delta front and littoral deposits, while the extension of sedimentary facies belts in the middle and the late stage of middle permian is as the same as that of shanxi stage

    中二疊世早期，研究區由北向南依次為沖積扇、辮狀河、辮狀河三角洲平原、辮狀河三角洲前緣和濱淺湖所佔據。中二疊世中晚期，沉積相帶展布順序與山西期相同。
  20. Based on the data of the rare - earth element in coals from coal seams of the late permian liupanshui, leping, huangshi and chongqing coal mining districts in south china, this paper focuses on the discussion of the characters of content distribution, occurrence, distribution pattern and geologic factors of the rare - earth element in coals in the studied districts

    摘要在華南地區貴州六盤水、江西樂平和湖北黃石礦區以及重慶鐘梁山和磨心坡煤礦晚二疊世煤的稀土元素電感耦合等離子質譜分析數據的基礎上，系統研究了華南地區煤的稀土元素的質量分數分佈特徵、賦存特徵、配分模式及其地質控制因素。
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