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)基本理論又粗又长视频，在綜合分析工區(qū)地震国产一级精品A片免费观看、測(cè)井、巖心等資料的基礎(chǔ)上无码一区网站，確立了超層序界面在线麻豆视频、準(zhǔn)層序和準(zhǔn)層序組識(shí)別標(biāo)志，進(jìn)而對(duì)松遼盆地北部升平地區(qū)深層進(jìn)行超層序界面識(shí)別精品激情，共識(shí)別出五個(gè)超層序界面国产91大屁股熟女，分別為基巖頂面(SSB1)、沙河子組底面(SSB2)小视频色网址、營(yíng)城組底面(SSB3)久视频网无码性一区、登婁庫組底面(SSB4)和泉頭組底面(SSB5)。

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.

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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(shí)驗(yàn)上發(fā)現(xiàn)狼友视频网址最新版，在低溫下，隨著摻雜濃度x的變化(0≤x≤1)亚洲日本色色，錳氧化物可以出現(xiàn)鐵磁序或多種形式的反鐵磁序欧美一级电；可以出現(xiàn)不同類型的軌道序，也可以沒有軌道序18成年女污禁网站免费观看；可以有電荷序强奷漂亮的女教师2中文字幕，也可以沒有電荷序。

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)久久精品一级aaaa，充填疊置方式国产污视频、演化及沉積體系分布的最重要因素：凹陷由多個(gè)半地塹在不同層序發(fā)育時(shí)期以不同方式疊置聯(lián)結(jié)而成；受斷層控制86精品自拍，層序外部形態(tài)有箱狀-楔形免费看18禁止观看啪啪网站、楔形-席狀披覆型，邊界終止方式有雙斷終止型国产大黄片、單斷終止超覆型在线观看黄色网站a；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，初始斷陷階段的SQ1沉積沖積層序黄色日韩不卡，強(qiáng)烈斷陷階段的SQ2-SQ4充填湖相層序，晚期斷陷階段SQ5-SQ7內(nèi)部充填淺湖和河流三角洲沉積一级特黄手机免费看片；同沉積斷層陡坡帶沉降迅速欧美三级日韩精选、可容納空間快速增長(zhǎng)，是凹陷的沉積和沉降中心强奸,com，斷陷期主控?cái)嗔鸦顒?dòng)時(shí)間和空間的變化導(dǎo)致了凹陷沉積和沉降中心的遷移国产欧美日韩另类VA在线。

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－序的充要條件欧美一级婬片人妻欧美电影，以及每一偏序均可擴(kuò)展成為Dω－序的條件久久深夜福利亚洲网站，同時(shí)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)上无码aaa，岔河剖面進(jìn)一步劃分出28個(gè)準(zhǔn)層序組伊人免费视频、62個(gè)準(zhǔn)層序和122個(gè)小層序，哲覺剖面劃分出17個(gè)準(zhǔn)層序組涩多多在线观看、46個(gè)準(zhǔn)層序和57個(gè)小層序操逼北京老妇，而密德剖面劃分出13個(gè)準(zhǔn)層序組、34個(gè)準(zhǔn)層序和62個(gè)小層序台湾久久一级婬A片AAA毛片。

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(duì)烏爾遜凹陷北部下白堊統(tǒng)地層進(jìn)行了層序地層分析黄色不卡福利，將其劃分為4個(gè)層序和4種層序類型，即簡(jiǎn)單斷陷層序国产精品第一区免费观看、快速斷坳層序人人摸人人艹人人、同生斷坳層序和簡(jiǎn)單坳陷層序国产精选插逼视频。

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，從沉積特征研究入手五月丁香六月激情欧美综合不卡，對(duì)該區(qū)的含磷巖系———洋水組劃分出5個(gè)沉積層序欧美性爱电影免费观看，結(jié)合層序界面及層序的歸納描述，確定了層序類型xxxx5566，并認(rèn)為洋水組是一套海進(jìn)體系域中由一系列低級(jí)別退積型沉積層序組成的高級(jí)層序下载日韩精品视频网站大全免费观看。

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），唐太宗之弟滕王李元嬰任洪洲都督時(shí)興建了這幢樓国产一级视频精品，而王勃為這座富麗堂皇的樓閣所作的《滕王閣序》更加使它名滿天下亚洲国产偷窥。

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."

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