upper triassic 中文意思是什麼
upper triassic
解釋
上三疊紀-
The sanwan opeirogeny is marked by the regional disconformity - angular overlapping unconformity below the upper triassic sanqiutian and yangmeilong formations, while the sandu opeirogeny is recorded by the regional disconformity - angular overlapping unconformity below the upper triassic zaoshang, duojiang and tanglong formations
三灣造陸運動以上三疊統三丘田組、楊梅壠組之下的區域性假整合-角度超覆不整合為標志；三都造陸運動以上三疊統造上組、多江組、唐壠組之下的區域性假整合-角度超覆不整合為特徵。 -
The yanchang formation of upper triassic in north shaanxi is major terrigenous clastic system deposited in fluvial - latchstring environment, under the influence of the llocyclicity factor which include indosinian tectonic, eustacy, sedimentary supplies and the autocyclicity factor. in late triassic, north shaanxi was divided into two parts bounded by zhidan - ganquan - yichuan demarcation line
陜北地區上三疊統延長組是以河流一湖泊相為特徵的陸源碎屑巖系，當時的陜北地區，以志丹?甘泉?宜川沿線為界，南側以明顯的斜坡向深湖盆地過渡，北部則為一地形平緩的淺水臺地。 -
Under the upper pressures belt or minute super pressures of the upper triassic series and jurassic system interface formation, the fluid in the upper triassic series moved along stratum interface, fault and crack network thoroughfare, formed " secondary gas pool " in the jurassic system
上三疊統和侏羅系界面形成的超壓帶或微超壓帶，使上三疊統氣藏流體在壓力差的作用下，沿斷層、地層界面和裂縫網路通道運移，在良好的侏羅系圈閉中形成「次生氣藏」 。 -
Delta sediments and evolution of the yanchang formation of upper triassic in ordos basin
鄂爾多斯盆地上三疊統延長組三角洲沉積及演化 -
The article mainly analyzes the chang 6 reservoir in the upper triassic in ordos basin. by tectonics, sequence stratigraphy, sedimentology and diagenesis, poly - statistics, and so on. it touches many professional fields, composing of 7 chapters and 23 sections
論文主要應用構造學，層序地層學，沉積學和成巖作用，以及多元統計等知識對鄂爾多斯盆地上三疊統延長組6段儲層進行了細致的研究，內容較豐富，共有7章23節。 -
Biological processes for the formation of carbonate concretions in the upper triassic wayao formation of guanling, guizhou
貴州關嶺上三疊統瓦窯組中碳酸鹽巖結核形成的生物作用 -
A great deal of statistic data illustrates that the mesozoic strata, especially the upper triassic immature sediments, are presumably an important source of ore - forming metals
大量統計表明，中生代地層、特別是晚三疊世低成熟度沉積巖是重要的礦源層。 -
Three sets of source rocks had been formed juring the steady sinking of the basin. the first source rock, being clay and calcium clay stone in tiemulike formation of permian was formed in deep lake environment ; the second source rock, being clay stone in xiaoquangou group of middle to upper triassic was formed in the offshore and the shallow lake environment ; and the third source rock, being coal beds in badaowan formation of lower jurassic was formed in the lake - swamp environment. the first one is the most potential, since it has the biggest thickness, the highest organic matter abundance, high maturity and the highest hydrogen generating capacity
在盆地穩定沉降時期，相應地形成三套烴源巖，即上二疊統鐵木里克組（ p _ （ 2t ） ）深湖、半深湖相泥巖、泥灰巖；中上三疊統小泉溝群（ t _ （ 2 - 3xq ） ）濱淺湖相泥巖及下侏羅統八道灣組（ j _ （ 1b ） ）湖沼相煤系地層。 -
Based on the investigations of 46 species of fossil spores and pollen belonging to 28 genera which were found from the yongping formation and wayaopu formation of upper triassic in tongchuan region of shaanxi province, the early to late late triassic palynoflora in the region was established
摘要本文基於陜西銅川地區上三疊統水坪組和瓦窯堡組發現的孢子花粉化石28屬46種的研究，建立了研究區晚三疊世早期至晚期孢粉植物群。 -
Formation of laumontite of the upper triassic yanchang group in ordos basin and its effect on reservoirs
靖安油田上三疊系延長統濁沸石的形成及對儲層的影響 -
Characteristics and significance of lacustrine turbidites in the member 1 of yanchang formation, upper triassic in the southeastern ordos basin
鄂爾多斯盆地東南部三疊系延長組一段湖相濁積巖特徵及意義 -
In the present research, therefore, identification of the shape of permeable sands seems very important. in a word, it ' s of great significance in the theory and in practice to find out the location, shape and extending direction of lacustrine delta and characteristics of different microfacies in the upper triassic yanchang formation
因而，在當前各項研究中，弄清良好的滲透性砂體的形態及其展布就顯得十分重要，即精確確定上三疊統延長組的湖泊三角洲砂體形態、展布方向及其沉積微相特徵，進一步了解砂體的物性特徵，對指導鄂爾多斯盆地中生界油氣的開發具有重要的理論和實踐意義。 -
In the present work, sequence - paleogeographic mapping is implemented on the s econd member of the upper triassic xujiahe fm. and the upper jurassic ponlaizhen g fm. in western sichuan, china, with system tracks taken as the mapping units
研究重點選擇上三疊統須家河組二段和上侏羅統蓬萊鎮組，按體系域進行層序-巖相古地理編圖。 -
The paper put forward the particular mode of sequence stratigraphy in the foreland basin, which includes lacustrine margin alluvial systems tract ( ast ), lacustrine expanding systems tract ( ltst ), and lacustrine highstand systems tract ( lhst ). the upper triassic can be divided into three marine and one nonmarine sequences
2 、提出了川西前陸盆地的層序地層模式，認為川西前陸盆地一個完整的陸相層序是由湖盆邊緣沖積體系域、湖侵體系域和湖泊高水位體系域三部分構成。 -
Guided by a series of theories and methods of high - resolution sequence stratigraphy and sedimentology, the characteristics of medium - term, short - term and ultra short - term base - level cycle sequences have been studied in chang 6 member, upper triassic, fuxian exploration area, and the base - level cycle sequence structure types and stacking - patters formulized in detail. the sedimentary characteristics of two types of sedimentary facies, four kinds of sedimentary subfacies and ten species of sedimentary microfacies have been generalized. it has been researched that the distribution and evolution rule of sequence sedimentary facies
本文以高解析度層序地層學和沉積學的理論與方法為指導，研究了富縣探區上三疊統長6段中期、短期和超短期基準面旋迴層序的特徵，詳細闡述了各級次基準面旋迴層序結構及疊加樣式；總結了長6段兩類沉積相、四種亞相以及十種微相的沉積特徵；闡明了長6段層序沉積相的展布與演化規律；在深入論述高解析度層序地層和沉積相與儲層發育關系的基礎上，評價預測了本區長6段的有利儲集相帶。 -
The high - resolution sequence stratigraphy analysis of the upper triassic xiangxi formation in the moxi - longnusi structure of sichuan, china
龍女寺構造香溪群高解析度層序地層分析 -
Sedimentary characteristics of sublacustrine fan of the interval 6 of yanchang formation of upper triassic in southwestern ordos basin
鄂爾多斯盆地西南部上三疊統長6油層組湖底扇特徵 -
Source characteristics and gas origin of xujiahe formation, upper triassic in chishui area
赤水地區上三疊統須家河組源巖特徵及天然氣成因 -
Research on source characteristics and origin of xujiahe formation, upper triassic in chishui area, sichuan basin
四川盆地赤水地區上三疊統須家河組烴源巖特徵及天然氣成因探討 -
After field profiles being observed and some indoor tests and analysis being fulfilled, this paper researched distribution, organic type and abundance of the xujiahe formation, upper triassic in chishui and other areas in the sichuan basin, analysed the main geo - chemical characteristics of the gas from the xujiahe formation, discovered the source characteristics of the xujiahe formation, and discussed the origin of the natural gas found in the formation
摘要細致觀測了野外剖面，並進行了相關的室內分析化驗，對比研究了赤水地區與四川盆地其他地區上三疊統須家河組烴源巖分佈特徵、有機質類型及豐度，結合赤水地區須家河組天然氣的主要地球化學特徵，揭示了赤水地區須家河組的源巖特徵，初步探討了其天然氣成因。
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