漸厚地層 的英文怎麼說
中文拼音 [jiānhòudecéng]
漸厚地層
英文
expanding bed-
Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock
摘要以現有資料為基礎，通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究，認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化，沉積了巨厚的新生代地層，自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。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
根據濱北地區地層的沉積特點和地球化學研究，各層源巖表現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源巖發育最好。Through the correlation of nww - see and sn, the thickness and limestone intervals of matuo formation gradually increase from west to east. this represent the center of sedimentation is possible located in east of the region. the matuo formation thickness gradually increase and then reduce from north to south
通過北西西?南東爾向和南北向剖面對比，瑪托組地層橫向變化表現為由西往東，瑪托組地層厚度逐漸加大，灰巖夾層也增多，反映當時沉積中心在研究區東部，而由北往南，厚度先逐漸增大，后減小，灰巖夾層增多，由北往南的古地理格架為濱面?碳酸鹽臺地?斜坡環境。The stratigraphic analysis reveals that the upper part of kongdian formation is characterized by thickness range from 461 - 744 m and average of thickness of 602. 5 m. the number quantity of sandstone increased to the north and northwest, indicating more sand bodied are found at these directions
地層學分析表明南斜坡主要發育孔店組上段，地層自南向北逐漸增厚，地層厚度一般為461 - 744m ，平均厚602 . 5m 。The general thickening from the southwest towards the northeast and north, combined with increasing of fine clastic to the northeast and north, indicate principle source of the upper kongdian formation from the southwest and south
自南而北地層逐漸加厚、細粒沉積物含量以及地層內部反射結構表明孔店組沉積時期物源來自研究區南部。It is a picturesque expanse, framed in lofty crags in large strata, encrusted with white salt, - a superb sheet of water, which was formerly of larger extent than now, its shores having encroached with the lapse of time, and thus at once reduced its breadth and increased its depth
在這個美麗的大湖裡有許多光怪陸離的礁石，礁石的底座寬大，上面厚厚地蓋著一層雪白的海鹽。一片遼闊無邊的海面十分沉靜。從前大鹹湖的面積比現在大得多，隨著歲月的增長沿岸陸地日益擴大，湖面逐漸縮小，然而，湖底卻越變越深。分享友人