stratigraphic facies 中文意思是什麼

stratigraphic facies 解釋
地層相
  • stratigraphic : adj. 【地質學;地理學】地層學的。adv. -cally
  • facies : n. 〈pl. 〉 〈單復同〉1. 顏面,外觀;外表。2. 【生態】演替系列混優種社會,演替系列變群叢。3. 【地質學;地理學】相。4. 【醫學】面色;表面。
  1. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現,紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖,以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陷陡坡背景下,上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系,下降半旋迴高水位期,扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。
  2. By comparing with the strata of " holocene series of the coastal plain of laizhou bay " and combining 14c age measurement, the strata position and features of the lagoon ? hallow sea ? each sedimentary facies are confirmed. the stratigraphic division of upper marine facies of holocene is done and the sedimentary environment of every stratum is affirmed

    通過與「萊州灣濱海平原全新統」進行地層對比並結合~ ( 14 ) c測年數據,確定了該沉積區全新世瀉湖?淺海?海灘相沉積層的層位和特徵,並對該層及其以上地層進行地層劃分,判斷出各層的沉積環境。
  3. Based on the synchronic seqence stratigraphic framework, through comprehensive investigation of the evaluation of seqence, the type of sedimentary facies and sedimentary system with it ' s area distribution, the domination of paleogeographic structure to paleocurrent and sedimentary system, draw a conclusion : the boundaries of the thickness of sequence was bounded by the boundary faults. the irregularity of sedimentary facies was dominated by base level rise to fall and accommodation

    在建立等時層序地層格架的基礎上,分析了層序的充填演化規律、沉積相和沉積體系的類型及其平面分佈特徵、古構造對古水流和沉積體系分佈的影響,得出以下認識:層序發育的厚度受邊界斷層控制,層序內部沉積相的變化規律受基準面和可容納空間的控制。
  4. On the basis of all kinds of stratigraphic and petrologic data of outcrop and well sections, the maps of single factors and sedimentary facies of the paleocene - eocene, oligocene and miocene were compiled with the single factor analysis and multifactor comprehensive mapping method proposed by professor feng zengzhao

    摘要根據柴達木盆地北緣露頭剖面、鉆井剖面的地層學和巖石學研究所取得的各種定量及定性資料,採用馮增昭教授倡導的單因素分析多因素綜合作圖法,編制了柴達木盆地北緣結綠素紅山地區古新統始新統、漸新統和中新統的各種單因素圖和沉積相圖。
  5. And it is also possible to analyze the reservoir property in reservoir framework. taking the reservoir of zonation 6 - 10 in s32 of pucheng oil field in henan province as an example, we founded the detailed reservoir stratigraphic framework through base - level correlation. in the strata frame, sediment distribution and its development are discussed based on sediment volume partitioning and facies differentiation analysis

    依據基準面變化中的過程?沉積響應,分析沉積過程中沉積物體積分配及與其相伴生的相分異,進行等時地層對比,建立精細地層格架,預測儲層空間展布及其非均質性的思路為儲層精細描述提供了新的方向。
  6. Through the analysis of the stratigraphy and sedimentary facies of the research areas, the description model between the stratigraphic framework and deposite environment can be set up firstly by the transition from the " three horizons sandstone with two intercalated limestone horizons ' mn yanshiping area to shale and marl in amdo - zigetang co, and to oil shale in bilong co, then by the transition of the shallow water platform facies to the deep water continental shelf, slope, and to the deep water basin

    通過對研究區地層和沉積相分析,建立起一個從北向南由雁石坪地層類型「三砂夾兩灰」過渡為安多?茲格塘錯地層類型泥頁巖、泥灰巖,最後到比洛錯地層類型黑色油頁巖,由淺水臺地相過渡到深水陸棚、斜坡,最後到深水盆地相的地層格架與沉積環境解釋模式。
  7. Abstract according to the " stratigraphic guide of china and its explanation " and based on the general rules for naming stratigraphic units and the principles of priority, a fairly detailed discussion is made on the correct use of the formation - rank names of the lithostratigraphic units of the mesozoic paralic facies of the longzhaogou group in the east of heilongjiang province

    摘要以《中國地層指南及中國地層指南說明書》 (修訂版)為依據,以地層單位命名的一般規定為準繩,以地層單位命名的優先權為法則,對黑龍江省東部地區中生代晚期海陸交互相地層龍爪溝群組級巖石地層單位名稱的正確使用問題,進行了較為詳細的討論。
  8. Guided by the basic theory of high - resolution sequence stratigraphy, and based on the core observation, the analysis of chemical composition of rocks, and data of natural potential logging and apparent resistivity logging, authors have set up the high - resolution sequence stratigraphy framework of the ore - hosting yaojia formation, and discussed the relation of the stratigraphic structure of the middle cycle, as well as the paleotopography, the micro - facies to the formation of uranium deposit

    在高解析度層序地層學基本理論指導下,筆者通過巖心觀察、巖石化學組分分析、自然電位及視電阻率測井等手段,建立了賦鈾巖系姚家組高解析度層序地層格架,探討了中期旋迴內地層結構、古地形和沉積微相與鈾礦床形成的關系。
  9. Based on the principles of palaeobiology, stratigraphic geology, sedimentology, diagenesis and reservoir geology, taken field profile and drilling cores as research object, and combined with achievement of predecessors, the sedimentary facies, diagenesis essential characteristics of reservoir and controlling factors for reservoir of feixianguang formation in northwest sichuan have been comprehensively studied. both classic and mordern methods have been used in this research. the main confents includes : stratigraphic classification and correlation of feixianguan formation in lower triassic, the rock fexture characteristics, type and forming conditions of rock ; determining dirtributary law of the sedimentary facies in vertical and horizontal direction and distribution in plane and the essetial contronling factors through correlation of sedimentary facies transverse profile and regionnal geologic characteristics ; establishing plane stereoscopic modle of sedimentary of oolitics beach by studying diagenesis

    主要內容包括:對川西北地區下三疊統飛仙關組地層進行了劃分與對比,研究了飛仙關組地層的巖石結構組分特徵、類型和形成條件;通過沉積相橫向剖面的對比,並結合區域地質特徵,深入研究了沉積相在縱、橫向上的變化規律,確定了沉積相在平面上的分佈及主要控制因素,分析了沉積相的縱向演化過程和建立了沉積相的平面立體模式;詳細研究了該套地層所經歷的成巖作用類型、特徵及對儲集空間的影響,建立了鮞粒灘相儲層的形成與演化模式;最後,從沉積相、成巖作用的角度,分析了區內飛仙關組地層的生油潛力、儲層的分佈規律和發育區塊。
  10. In this paper, the author paticular analysis 11 core holes and established the partition of strutum gyration of key layers in the area, then stratigraphic analyzed the 225 well and identified microfacies of the target area, then established the mode of facies. the author analyzed the evolvement law of different type of channel combined sedimentary environment

    本文首先通過對11口取芯井的詳細解剖,確立了研究層段的層序地層格架劃分方案,進而對研究區225口井進行了精細劃分對比,進行了不同類型河道所處環境的微相識別與劃分,並建立了研究區的相模式。
  11. This paper focuses on the establishment of the synchronic stratigraphic framework, the effect of paleogeographic structure to the direction of paleocurrent and the distribution of sedimentary system in time and space, the type of sedimentary facies and it ' s evolution, the matching relations of generation, reservoir, seal rock, the prediction of favorable zone

    重點分析層序格架的建立、古地理格局及其對古水流和沉積體系作用的影響、沉積相的類型和演變特徵、沉積體系的時空展布特徵、生儲蓋的組合及勘探有利區帶的預測等幾方面。
  12. Six lithofacies palaeogeographic maps of doushantuo, dengying, qiongzhusi, canglangpu, and longwangmiao ages of late sinian and early cambrian have been made in the light of dominant facies and in the way to make stratigraphic map

    中揚子地區上震旦統發育了從碳酸鹽潮坪、開闊臺地、淺灘、臺地邊緣、斜坡到臺地前緣盆地等沉積,下寒武統下部主要?細碎屑巖和碳酸鹽巖組成的混合型淺海陸棚沉積,上部變成碳酸鹽潮坪、開闊臺地、臺緣斜坡和臺緣盆地沉積。
  13. Will be discussed in this paper, based on the analysis of the sedimentary facies characters and paleo - environment indexes such as clay mineral, chemical element and spore - pollen of the sediment samples collected from the middle - part of the stratigraphic profile including upper and lower cultural layers of the dongfang plaza cultural site

    依據對遺址區剖面中段包含了上下兩個文化層沉積樣品的沉積相特徵以及粘土礦物化學元素和孢粉等古環境指標的分析,探討了2 . 6萬年前後至1 . 4萬年前後古環境的演變過程。
  14. Time stratigraphic facies

    時間地層相
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