Based on seismic, well logging, drilling and core data, five super sequence boundaries have been identified by using methods of sequence stratigrphy theory in deep formations of Shengping area, northern part of Songliao basion. They are the top boundaries of bed rock (SSB1), the bottom boundaries of Shahezi group (SSB2), the bottom boundaries of Yingcheng group (SSB3), the bottom boundaries of Denglouku group (SSB4) and the bottom boundaries of Quantou group (SSB5) respectively.

應(yīng)用層序地層學(xué)基本理論看黄片二级，在綜合分析工區(qū)地震、測井国产污视频网站在线观看、巖心等資料的基礎(chǔ)上H色视频网站，確立了超層序界面、準(zhǔn)層序和準(zhǔn)層序組識別標(biāo)志日韩高清视频免费观看，進(jìn)而對松遼盆地北部升平地區(qū)深層進(jìn)行超層序界面識別未满十八禁止18以下免费的AV，共識別出五個超層序界面，分別為基巖頂面(SSB1)免费视频啪啪538、沙河子組底面(SSB2)、營城組底面(SSB3)亚洲黄色网站WWW、登婁庫組底面(SSB4)和泉頭組底面(SSB5)本地自拍日韩在线观看网站视频。

It was the first time the sequence stratigraphy study had been done all across Naimanqi Depression. Jiufotang Formation of Naimanqi Depression was divided into two third-class sequences (SQ1 and SQ2) and five system tracts (SQ1 has LST, TST and HST; SQ2 has TST and HST), and in High System Tract of SQ2, two fourth-class sequences were defined (Ssq1 and Ssq2).2. According to the analysis of core and logging data, we considered that it is the delta fan facies and established the electrofacies model.3. The distribution of reservoir sand bodies had been predicted in the areas without well data by combining the methods of sequence stratigraphy and reservoir inversion. In addition, we summarized the method and process of combining geology and geophysics to predict reservoirs and we made a good prediction by applying it.4. Combining with sequence and depositional types, sandstone thicknesses and reservoir properties, based on Petrel Software platform, we used fuzzy mathematics to comprehensively evaluate reservoirs and define favorable areas. We classified the reservoirs in Naimanqi Depression into five types (TypeⅠ, TypeⅡ, TypeⅢ, TypeⅣand TypeⅤ) and pointed out four favorable areas: Block Nai 1, Block of western Naican 1-Zhangjia Depression, Block Nai 6 and Block of Xinfa-Zhangjia Depression.

其主要創(chuàng)新點如下：1、首次在整個奈曼旗凹陷范圍內(nèi)進(jìn)行了層序地層學(xué)的研究国产亚洲综合无码一区二区，將奈曼旗凹陷九佛堂組地層分為2個三級層序(SQ1和SQ2)和5個體系域(SQ1由LST狼友最新视频首页入口、TST和HST組成，SQ2由TST和HST組成)好操爽还要在线播放，并在SQ2的高位體系域中又識別出兩個四級層序(Ssq1和Ssq2)嘿咻视频视频在线网站。2、根據(jù)巖芯分析和測井資料識別欧美一级三级国产精品，定義了研究區(qū)扇三角洲沉積相類型欧美添逼视频，并建立了測井相模板。3av小草、通過層序地層學(xué)的研究久久综合精品免费毛片，結(jié)合儲層反演美国一级网站，對奈曼旗凹陷層序格架內(nèi)沒有井的區(qū)域進(jìn)行了儲層砂體的空間展布預(yù)測，并總結(jié)了地質(zhì)-地球物理綜合儲層預(yù)測的方法與思路流程不卡av免费网址，在應(yīng)用中取得了良好的預(yù)測效果啊啊啊免费啪啪啪视频。4、結(jié)合層序久久九九精品99精品、沉積類型18禁黄网站禁片无码观看、砂巖厚度和儲層物性等方面，以Petrel軟件為基礎(chǔ)平臺黑人的又黑又大又长，利用模糊數(shù)學(xué)的方法進(jìn)行儲層綜合評價及有利區(qū)劃分免费AAAA欧美在线观看，將奈曼旗凹陷儲層劃分為五個級別(Ⅰ類、Ⅱ類视频。在线男女国产、Ⅲ類日韩美欧精品人妻、Ⅳ類和Ⅴ類)，并預(yù)測了四個有利區(qū)塊亚洲欧美精品综合久久小说，分別為：奈1區(qū)塊中文字幕国产精品一区、奈參1西-張家洼子區(qū)塊、奈6區(qū)塊和新發(fā)-張家洼子區(qū)塊

Experimentally,at low temperature and with doping x(0≤x≤1),some manganite may have very differentphases,ferromagnetic or antiferromagnetic,with or without orbital or charge order.

實驗上發(fā)現(xiàn)男人的天堂网免费网站，在低溫下先锋影音最新AV看片资源，隨著摻雜濃度x的變化(0≤x≤1)，錳氧化物可以出現(xiàn)鐵磁序或多種形式的反鐵磁序免费人成黄页在线观看国际；可以出現(xiàn)不同類型的軌道序在线黄色AV观看，也可以沒有軌道序；可以有電荷序人人操人人操人人舔，也可以沒有電荷序安卓官网番茄社区。

Tectonic subsidence play dominant role in their geometric shapes, basin fillings, sequence evolution and sediment distribution in the Wushi Sag. Outline of the sequences are in shape of box-wedge or sheet-wedge and boundaries of sequences are varied from bilateral fault to monoclinal fault overlap, so that the sequences show distinct semigrabens which overlay in different ways. Seven sequences were formed in different stage of tectonic evolution. The sequence of SQ1 formed in initial rift stage and deposited alluvial sequence. Sequences SQ2-SQ4 developed in intense rift stage and sediment lacustrine sequence. Sequences SQ5-SQ7 formed in late period of rift before thermal subsidence and deposit mere and delta sediment. The place adjacent to the synsedimentary fault is the subsidence center and depocenter; meanwhile, controlling fracture migrates in horizontal made subsidence and sedimentary center of the sag changed.

構(gòu)造沉降是控制層序幾何形態(tài)，充填疊置方式人人看人人亲人人操、演化及沉積體系分布的最重要因素：凹陷由多個半地塹在不同層序發(fā)育時期以不同方式疊置聯(lián)結(jié)而成一级a爱做片2；受斷層控制，層序外部形態(tài)有箱狀-楔形欧美三级片国产免费性爱视频、楔形-席狀披覆型最近免费中文字幕视频在线MV，邊界終止方式有雙斷終止型、單斷終止超覆型久久国国产免费999；不同構(gòu)造演化階段層序內(nèi)部充填的沉積體系各具特征久久精品一二三美女，初始斷陷階段的SQ1沉積沖積層序，強(qiáng)烈斷陷階段的SQ2-SQ4充填湖相層序可以永久免费观看的一级视频，晚期斷陷階段SQ5-SQ7內(nèi)部充填淺湖和河流三角洲沉積91在线视频第一页；同沉積斷層陡坡帶沉降迅速、可容納空間快速增長，是凹陷的沉積和沉降中心中文字幕亚洲日韩，斷陷期主控斷裂活動時間和空間的變化導(dǎo)致了凹陷沉積和沉降中心的遷移专业偷拍熟女在公司里偷星图片。

In this paper,we discuss the extension of the Dω-order and D*ω-order in partiany or-dered group,obtain the necessary and sufficient condition for an extension of the partial-or-der in partially ordered group to Dω-order and D*ω-order, and the condition for the exten-sion of every partial order in a group to Dω-order.

討論了偏序群的Dω－序擴(kuò)展，得到了偏序群的偏序可擴(kuò)展成為Dω－序的充要條件国产精品11页，以及每一偏序均可擴(kuò)展成為Dω－序的條件女人自慰喷潮A片免费观看网站，同時刻劃了Dω－序群。

Based on the mentioned above, Chahe section can be subdivided into 28 parasequence sets, 62 parasequences and 122 small sequences , Zhejue section can be subdivided into 17 parasequence sets, 46 parasequences and 57 small sequences, Mide section can be subdivided into 13 parasequence sets, 34 parasequences and 62 small sequences.

在此基礎(chǔ)上免费永久黄色网站，岔河剖面進(jìn)一步劃分出28個準(zhǔn)層序組91精品欧美综合1区、62個準(zhǔn)層序和122個小層序，哲覺剖面劃分出17個準(zhǔn)層序組一级黄色毛片网站、46個準(zhǔn)層序和57個小層序污污视频三级片，而密德剖面劃分出13個準(zhǔn)層序組、34個準(zhǔn)層序和62個小層序黄片观看无码在线。

According to the interpreted approaches of sequence stratigraphy,the lower Cretaceous strata in the northern Wuerxun sag can be divided into four types of sequence,namely simply faulted sequence,quickly faulted-depressed sequence,syngenetic faulted-depressed sequence and simply depressed sequence.

應(yīng)用層序地層學(xué)解釋方法對烏爾遜凹陷北部下白堊統(tǒng)地層進(jìn)行了層序地層分析日本黄色一级小视频，將其劃分為4個層序和4種層序類型，即簡單斷陷層序欧美日韩口爆吞精一二区、快速斷坳層序国产在线对白视频黄、同生斷坳層序和簡單坳陷層序。

Cycle are divided into for the phosphoric rock series of the Yangshui Formation at this zone, in association with sequence interface and its relative characterization, the types of the sequences are determined and the Yangshui Formation is considered a high-ranking I-level sequence that is constituted by a series of low-grade retrograding type of de.

應(yīng)用層序地層學(xué)的概念和方法理论日韩中文，從沉積特征研究入手超碰在线欧美精品，對該區(qū)的含磷巖系———洋水組劃分出5個沉積層序，結(jié)合層序界面及層序的歸納描述欧美又大又粗一区二区，確定了層序類型偷拍视频无码，并認(rèn)為洋水組是一套海進(jìn)體系域中由一系列低級別退積型沉積層序組成的高級層序。

Tang永徽four years (AD 653), the Emperor's younger brother Lee Teng Wang元嬰term captaincy general洪洲floor of this building, when built, and Wang Bo for this magnificent pavilion's "滕王閣序" more of it over the world.

唐永徽四年（公元653年）亚洲色欲综合网在线观看A，唐太宗之弟滕王李元嬰任洪洲都督時興建了這幢樓欧美一级视频网站免费在线观看，而王勃為這座富麗堂皇的樓閣所作的《滕王閣序》更加使它名滿天下。

Legend was passed by the poet Wang Bo relatives Nanchang, is to catch up with Yan滕王閣captaincy general rehabilitation after the Court on the banquet guests, Wang Bo wrote on the spot in this stretch here guests praise the service's "Autumn登洪House滕王閣餞別order"( that is,"滕王閣序"), prefaced by Wang Bo, another仲舒for Wang in mind that for Fu WANG history known as the "three kings article."

傳說當(dāng)時詩人王勃探親路過南昌日韩无码另类，正趕上閻都督重修滕王閣后男人操女的亚洲国产视频，在閣上大宴賓客，王勃當(dāng)場一氣寫下這篇令在座賓客贊服的《秋日登洪府滕王閣餞別序》激情欧美老妇视频，王勃作序后，又有王仲舒作記三级片黄色网站视频真人，王緒作賦日高清在线亚洲专区黄片，歷史上稱為&三王文章&。

antitone mapping：反序變換,反序映射

antithrust bearing 止推軸承,推力軸承 | antitone mapping 反序變換,反序映射 | antitonic regression 反序回歸

big endian：正序

微 處理機(jī)中的存放順序有正序(big endian)和逆序(little endian)之分. 正序存放就是高字節(jié)存放在前低字節(jié)在后,而逆序存放就是低字節(jié)在前高字節(jié)在后. 例如,十六進(jìn)制數(shù)為A02B,正序存放就是A02B, 逆序存放就是2BA0. 摩托羅拉(Mo

infix：中序

q+1, right); } } 22.Algorithm Gossip: 中序式轉(zhuǎn)后序式(前序式) 中序式轉(zhuǎn)后序式(前序式) 說明平常所使用的運(yùn)算式,主要是將運(yùn)算元放在運(yùn)算子的兩旁,例如a+b/d這樣的式子,這稱 之為中序(Infix)表示式,對于人類來說,

order homomorphism：序同態(tài);保序同態(tài)

序函數(shù) order function | 序同態(tài);保序同態(tài) order homomorphism | 零化理想 order ideal

partially ordered set：偏序集;部分序集

偏微分 partially differentiate | 偏序集;部分序集 partially ordered set | 偏序空間 partially ordered space

partially ordered set：半序集,偏序集

partially ordered plan 局部有序規(guī)劃 | partially ordered set 半序集,偏序集 | partially ordered space 半序空間

well ordered set：良序集,正序集

well-ordered 良序的 | well-ordered set 良序集,正序集 | well-ordering 良序

I. The Black Night: A Prefatory Poem：[黑夜黑夜黑夜黑夜::::序詩序詩序詩序詩]

6) The Black Desert [ 黑色沙漠黑色沙漠黑色沙漠黑色沙漠] | I. The Black Night: A Prefatory Poem [黑夜黑夜黑夜黑夜::::序詩序詩序詩序詩] | II. The Black Swamp [ 黑色沼澤黑色沼澤黑色沼澤黑色沼澤]

preorder traversal：先序遍歷

子樹記作 遍歷根的左子樹記作 L 遍歷根的右子樹記作 遍歷根的右子樹記作 R 則可能的遍歷次序有 DLR DRL 逆先序 先序 LDR RDL 逆中序 中序 LRD RLD 逆后序 后序 先序遍歷 (Preorder Traversal) 先序遍歷二叉樹算法的框架是 若二叉樹為空,

preorder inorder postorder：前序 中序 后序

preemption 有優(yōu)先權(quán)的 | preorder inorder postorder 前序中序后序 | presentation application layer 表示層應(yīng)用層