sequence boundary造句
例句與造句
- discussion of the methods of using logging curves to recognize sequence boundaries
測井曲線識別層序邊界的方法探討 - classification of sequence boundary of member 2 of sangonghe formation in hinterland of junggar basin
準(zhǔn)噶爾盆地腹部三工河組二段層序界面厘定 - characteristics of sedimentary facies and sequence boundary in upper cretaceous qingshankou-yaojia formation of northern songliao basin
姚家組沉積相及層序地層界面特征 - the key sequence boundaries with different orders, the lasting time of different sequences and the characteristic of every sequence are studied
研究了層序的持續(xù)時(shí)限及限定地層層序級別的關(guān)鍵性界面，并分析了層序的沉積特征。 - the occurrence of the palaeokarstification is closely associated with the sequence boundaries and lowstand systems tract created by the guizhou-guangxi, ziyun and dongwu movements
古巖溶作用的發(fā)生與黔桂運(yùn)動、紫云運(yùn)動、東吳運(yùn)動等所形成的層序界面和低位體系域密切。 - It's difficult to find sequence boundary in a sentence. 用sequence boundary造句挺難的
- the result shows that a sequence boundary is identified inside member 2 of sangonghe formation of lower jurassic, which is characterized by lithology of scour surface and conglomerate and gravel bearing gritstone over it, and by well logs of abrupt contact
通過巖心、錄井、測井、地震的綜合研究發(fā)現(xiàn)，在下侏羅統(tǒng)三工河組二段內(nèi)部可以識別出一個(gè)三級層序界面。 - the new results of which are as follows : l . paricular seven identification mark from up-shallowing to exposed surface in taphrogenic trough have been built, the first modelling of the identification mark of carbonate sequence boundary is very important in theory
首次將碳酸鹽巖層序變化識別特征模式化，具有重要的理論意義。2、提出了影響油氣聚集勘探單元?jiǎng)澐值男乱娊狻?/li> - controlled by the fouth sequence boundary, with chronostratigraphic modeling research with gridstat pro software, some models such as depositional facies model, lithology distribution and reservoir quality model ( include porosity, permeability and productivity ratio ) have been built
應(yīng)用四級層序界面進(jìn)行控制，利用gridstatpro軟件開展了等時(shí)性相控建模研究，建立了沉積相模型、巖性分布模型及儲層物性模型(包括孔隙度、滲透率及產(chǎn)能系數(shù)模型)。 - basing on the analysis and correlation of the7 wells, 8 seismic sequence boundaries are obtained by logging-seismic correlation, based on seismogram synthesis . more over, they can be traced in the studying region . the synchronic sequence stratigraphic framework is established finally
在單井分析和連井對比的基礎(chǔ)上，通過合成記錄標(biāo)定、地震層序的分析，識別出8個(gè)三級層序界面，而且完成了全區(qū)的主干剖面解釋，建立了井震統(tǒng)一的等時(shí)層序地層格架。 - it is most important to define the sequence boundary and the maximum flood surface for sequence classification . sequence boundary is the turn-point of the falling and rising of the baselevel . the maximum flood surface is the turn-point of the rising and falling of the baselevel
層序的劃分最重要是確定層序界面和最大洪泛面，層序界面為基準(zhǔn)面下降和上升的轉(zhuǎn)折點(diǎn)，而最大洪泛面是基準(zhǔn)面上升到下降的轉(zhuǎn)折點(diǎn)，這兩個(gè)面一旦確定，就可以劃分一個(gè)相對完整的層序。 - it is most important to define the sequence boundary and the maximum flood surface for sequence classification . sequence boundary is the turn-point of the falling and rising of the baselevel . the maximum flood surface is the turn-point of the rising and falling of the baselevel
層序的劃分最重要是確定層序界面和最大洪泛面，層序界面為基準(zhǔn)面下降和上升的轉(zhuǎn)折點(diǎn)，而最大洪泛面是基準(zhǔn)面上升到下降的轉(zhuǎn)折點(diǎn)，這兩個(gè)面一旦確定，就可以劃分一個(gè)相對完整的層序。 - cross, this paper has provided four grade sequences classifying synthetic plan, which has considered sequence boundary characteristics, boundary grades, sequence structure and superposing style . the classifying plan includes : super long, long, middle and short cycle sequence . on base of this plan, the jurassic sequence of the studied area can be divided into 4 super long cycle sequences, 8 long ones, 22 middle ones and more than 100 short cycle sequences
cross按基準(zhǔn)面旋回級別劃分層序和層序命名的原則，提出同時(shí)考慮界面性質(zhì)、界面級別、層序結(jié)構(gòu)和疊加樣式的超長期、長期、中期和短期4個(gè)級別的層序地層綜合劃分方案，將研究區(qū)侏羅系地層劃分為：4個(gè)超長期旋回層序，8個(gè)長期旋回層序，22個(gè)中期旋回層序及百余個(gè)短期旋回層序。 - the development of sedimentary environment of yanchang formation be analyzed and discussed further . based on the analyses of all kinds of sedimentary deposit . under the direction of the theory and methods of sequence stratigraphy, 4 type i sequence boundary could be recognized in the study area, according to the marked bed including plane of deflation, scour, the plane of lithological salutation, structural transformation, down cutting channel sheet sand and so on . type i sequence consists of low stand systems tract, transgressive systems tract and high stand systems tract
本文采用當(dāng)代層序地層學(xué)理論和方法，利用風(fēng)化剝蝕、沖刷面、巖性巖相突變、結(jié)構(gòu)轉(zhuǎn)換面、構(gòu)造機(jī)制轉(zhuǎn)換面等層序界面的識別標(biāo)志，將研究區(qū)延長組劃分為四個(gè)層序，其層序界面都為型層序界面，具有三元體系域結(jié)構(gòu)特征，由低水位體系域、水進(jìn)體系域和高水位體系域三個(gè)部分組成。