At the same time, the four different genesis types of the sequence interfaces are divided: orogenic erosive sequence unconformity interface, uplift erosive sequence unconformity interface, transgression onlap sequence unconformity interface, exposural sequence unconformity interface; simultaneously the ten concrete mineral showing forms are summarized, i.e. paleo-weathering crust, drossy layer, river rejuvenation surface, paleo-karst surface, slope gravity current erosion surface, intrabasin turbid flow erosion surface, volcanic events surface, lithologic and lithofacies conversion surface, onlap surface and maximium sea flooding surface.

同時(shí)歸納出了4種不同的層序界面成因類型：造山侵蝕層序不整合界面、升隆侵蝕層序不整合界面、海侵上超層序不整合界面和暴露層序不整合界面等性感美女黄污被操黄污网站在线观看；同時(shí)總結(jié)出10種具體的物質(zhì)表現(xiàn)形式，即：古風(fēng)化殼www.kszhibo.com、渣狀層黄色影院欧美日韩、河流回春作用面、古喀斯特作用面欧美无吗视频看片a、斜坡重力流沖刷侵蝕面毛片看片网址、盆地內(nèi)濁流侵蝕面、火山事件作用面国产精品久久久精品A级、巖性欧美大片免费看用力操、巖相轉(zhuǎn)換面、上超面和最大海泛面国产一级一片免费播放网站。

The unit bottom was the unconformity developed by Wuling Movement, and the unit top was overlapped by glacial deposition of Nanhua System. What\'s more, an unconformity can be found in Northern Guizhou and North-western Hunan. At the same time, this boundary was an important transformation between different deposition types: Banxi Group was rift basin deposition with flysch suite, and bearing a vast amount of pyroclasts, and this suggests that there was strong activity of crust. But the overlapping glacial deposition stood for steady deposition with penecaprock characteristic, and under unique climate environment.

下為武陵運(yùn)動(dòng)形成的角度不整合面所限国产色欲一精品一aV一免费；其上被南華冰期沉積所超覆，在黔北—湘西北可見(jiàn)角度不大的不整合欧美性爱就爱操，而且這一界面是兩個(gè)不同沉積類型或建造之間的一個(gè)轉(zhuǎn)換：板溪群為具有復(fù)理石韻律的裂谷系充填广州深圳一级毛片，其中發(fā)育大量火山碎屑沉積，顯示較強(qiáng)的地殼活動(dòng)性96视频在线；而上覆的南華冰期沉積所代表的是一個(gè)具有準(zhǔn)蓋層性質(zhì)的色哟哟精彩视频一区国产在线、獨(dú)特氣候環(huán)境下的穩(wěn)定沉積。

The effects of the unconformity surface on karst mainly include two aspects: one is the configuration of unconformities which controls the development scale of regolith karst, another is the intensity of unconformities which controls the development depth of regolith karst.

不整合面對(duì)巖溶發(fā)育的控制主要體現(xiàn)在兩個(gè)方面欧洲亚洲熟女一区二区三区，一是不整合面形態(tài)對(duì)分化殼巖溶發(fā)育范圍的控制操草网站，二是不整合面的強(qiáng)度級(jí)別對(duì)分化殼巖溶發(fā)育深度的控制。

Yizheng movement, Wubao movement and Sanduo movement happened ordinally in Gaoyou depression and then regional unconformity formed. According to the feature of unconformity and stockwerke, the sedimentary cover could be compartmentalized as upper, middle and subjacent stockwerke. Fault activity is different because of different intensity of structural movement.

高郵凹陷先后經(jīng)歷了儀征運(yùn)動(dòng)那个有毛片网站、吳堡運(yùn)動(dòng)和三垛運(yùn)動(dòng)等幾大規(guī)模構(gòu)造運(yùn)動(dòng)大码老熟女Av毛片免费，形成了區(qū)域性不整合面，依據(jù)不整合及其分隔的構(gòu)造層的結(jié)構(gòu)特點(diǎn)天天日天天干天天搞，可將高郵凹陷的沉積蓋層劃分為上丰满少妇强力进入毛片、中、下三個(gè)構(gòu)造層草草草干干干。

There are three features in the minibasins induced by gravitational sliding on the slope: the firstly, feature is surface of unconformity developed by onlap on minibasin margins or surface of unconformity truncated by mass transport-complex are sequence boundary in the study area; the secondly , accommodation of gravity flow is controlled by up lift rate and sedimentation rate , and styles of filling in the minibasins are dominated by the interrelationship between the two factors; and the third , there are two stacking patterns that consists of upward of turbidite fan-hemipelagic drape mud or mass-transport complexes-turbidite fan-hemipelagic drape mud.

認(rèn)為在深水陸坡重力滑動(dòng)作用所形成的微盆地內(nèi)亚洲黄性图，層序邊界表現(xiàn)為微盆地邊緣上超不整合面或重力流對(duì)下伏地層的侵蝕不整合；逆沖構(gòu)造隆升速率與沉積速率共同控制了重力流可容空間和沉積充填樣式无码三级中文字幕在线视频；沉積垂向演化以塊狀搬運(yùn)復(fù)合體一濁積扇－深海披覆泥或濁積扇－深海披覆泥為特征国产日本精品三级片。

This study shows that there are 4 kinds of volcanic facies in deep volcanics in north Songliao Basin: eruptive facies, overflow facies, volcanic vent facies and volcanic sedimentary facies. There are 4 volcanic eruption cycles: Huoshiling period, Shahezi period, Yingchengzi period and Quantou period. There are 4 structural evolution stages: north-south accumulation, west-east subduction, uplift mantle and thin crust, alternative open and close. There are 4 kinds of pool-forming patterns:(1) pattern with the migration along the unconformity and fault to the near crater;(2) pattern with the migration along unconformity and fault to the rift margin;(3) pattern with the migration along unconformity, fault and fracture to the source rock;(4) pattern with the migration of the deep gas along the deep and large fault to the volcanic trap.

研究認(rèn)為，松遼盆地北部深層火山巖主要存在四種火山巖相：即爆發(fā)相久久99精品九九九久久婷婷、溢流相国产日韩欧美区、火山通道相中文无码天堂一区二区三区、火山沉積相，劃分為四個(gè)火山噴發(fā)旋回：即火石嶺期黄色视频免费观看网站、沙河子期亚洲自拍日韩欧美精品、營(yíng)城子期、泉頭期6080午夜理论在线毛片，經(jīng)歷了四個(gè)構(gòu)造演化過(guò)程：即南北夾攻国产嫖娼啪啪精品、東西俯沖、幔隆殼薄激情久久免费视频、開(kāi)合交替欧美BB网，具有四種成藏模式：即沿不整合面和斷層運(yùn)移至近火山口處火山巖圈閉聚集成藏模式日日操免费看毛片、沿不整合面和斷層砂巖疏導(dǎo)層運(yùn)移至斷陷邊部火山巖圈閉聚集成藏模式麻豆福利导航、沿不整合面及斷層、裂縫運(yùn)移至源巖區(qū)內(nèi)凹中隆火山巖圈閉聚集成藏模式欧美A级黄片午夜福利、深部無(wú)機(jī)成因天然氣沿深大斷裂運(yùn)移至火山巖圈閉聚集成藏模式网站黃色毛片。

This dissertation was focused on the research about the formation and evolution of NQB from the Late Triassic to the early middle Epoch of Jurassic Period, including integrated analyzing the characteristic of the key stratigraphic surfaces, the time of the key stratigraphy, regional rock straigraphy, biostratigraphy and chronostratigraphy, sedimentary system and depositional facies. On basis of these analysis, a tectonic evolution model have been established for NQB during from the Late Triassic to the early middle Epoch of Jurassic Period.1. After the systematic surface analysis about main stratigraphy units, we found that:(1) the bottom of Xiaochaka formation was comformity with the middle Triassic in the basin, and in the north margin it was deposited and overlapped on the different period stratigraphy before Triassic.(2) The top surface of Xiaochaka formation developed regionally karst and paleo-karst breccia, and was uncomformity with Nadigangri Formation, these things suggest that NQB in Xiaochaka depositing stage was developed from middle Triassic basin, and then an extensive regression occurred, the deposition was over and erosion come into being.(3) The lithologic assemblage, geochemistry, mixed fossils, and stratigraphy overlapping characteristic of Quemocuo Formation in early middle Jurassic indicted that the uncomformity surface was an extension-unconformity.2. Integrated analysis about stratigraphy division and correlation indicted that:(1) the paleontologic assemblage of Xiaochaka formation show its time was Carian -Norian stage of late Triassic. According to it was overlapped by late Triassic Nadigangri Formation, so Xiaochaka formation should be Carian - early Norian stage.(2) the SHRIMP Zircon U-Pb age of Nadigangri formation volcanic rocks wear vary form 216 to 205 Ma, so its time should be Norian, but maybe extended into Rhaetian Stage.(3) The age of its bottom volcanic rocks, the fossil assemblages of its middle and upper members and overlapped by lower Jurassic, indicted the age of Riganpeicuo Formation was Norian - Rhaetian stage. And the same time, the volcanic rocks geochemistry of Nadigangri and Riganpeicuo formation both reflected that they wear formed in rift tectonic settings. The lower lithologic and surface characteristic, fossil assemblages and its upper maybe was conformity with lower Jurassic, all reflected that the age of Tumengela Formation in Tumen area should be Norian - Rhaetian stage.

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Geological model of unconformities'transportation system is built, mechanism of hydrocarbon in the unconformities is analyzed and concavo-convex vergent of hydrocarbon migration within the unconformities is proposed, which effectively guided the research of accumulation rule and exploration in Huimin Depression.

建立了不整合輸導(dǎo)的地質(zhì)模型，分析了油氣在不整合巖層中的動(dòng)力學(xué)機(jī)制久久久久久久国产精品电影，提出了不整合油氣運(yùn)移的凹凸匯散理論男和女的黄色视频xx日，有效指導(dǎo)了惠民凹陷的油氣成藏規(guī)律研究和油氣勘探工作。

This *** is titled "Relationship between Pre-Tertiary unconformity and hydrocarbon migration-accumulation in Jizhong depression". Unconformity can be divided into five types in Jizhong depression: truncation unconformity, fault-fold unconformity, parallel unconformity, truncation-onlap unconformity and fault-onlap unconformity by massive two-dimensional and three-dimasional seismic interpretations . Different types of unconformity have different distribution law.

本論文以&冀中坳陷前第三系不整合與油氣運(yùn)聚關(guān)系&為題无码黄片视频，通過(guò)大量的二維和三維地震解釋亚洲中文字幕一区女教师，把研究區(qū)不整合分為削截不整合、斷褶不整合95视、平行不整合欧美性交黄片A片、削截-超覆不整合和斷層-超覆不整合等五種類型，不同類型的不整合在空間上具有不同分布規(guī)律99性爱精品视频网。

Connecting sand body migration systems may controls the forming of oil-gas reservoir due to bottom bed overlap. lithologic pinch out, and/or the fault barrier. The migration system consisting of unconfornfity surface, sand bodyunconformity surface, and/or unconformity surface-fault, may control the forming of the bedrock weathered crust type oil-gas reservoir. The migration system consists of fault, sand body-fault, and/or sand body-unconformity surface, may control formation of oil-gas reservoir due to fault block, anticline, structure-lithologic, and/or fault-lithology.

連通砂體輸導(dǎo)系統(tǒng)可控制底層超覆日本com、巖性尖滅、斷層遮擋油氣藏的形成7色在色在线视频；不整合面18禁点击进入网址免费、砂體-不整合面、不整合面-斷層組成的輸導(dǎo)系統(tǒng)可控制基巖風(fēng)化殼油氣藏的形成欧洲美女A视频一级毛片；斷層黄色网站污污污亚洲免费、砂體-斷層、砂體-不整合面-斷層組成的輸導(dǎo)系統(tǒng)可控制斷塊色黄视频久久久、背斜午夜操逼视频、構(gòu)造-巖性和斷層-巖性油氣藏的形成。

discordant coastline：不整合海岸線

不整合蓋層分佈圖 lap-out map | 不整合海岸線 discordant coastline | 不整合現(xiàn)象 unconformability

disconformity：平行不整合

主要的不整合有非整合(nonconformity)国产福利亚洲一区二区三区、角度不整合(angular unconformity)、 平行不整合(disconformity)和小間斷(diastems). 非整合是指沉積巖覆蓋在較老的變質(zhì)巖或深成火成巖之上. 角度不整合將年輕的精品国无码一区二区三区不卡、變形較輕的沉積巖同傾斜或褶皺的沉積巖分開(kāi),

discordant bedding：不整合層理

discordant batholith 不整合巖基 | discordant bedding 不整合層理 | discordant injection 不整合侵入

discordant injection：不整合侵入

discordant bedding 不整合層理 | discordant injection 不整合侵入 | discordant intrusive 不整合侵入巖體

unconformable：不整合的

unconformability 不一致的狀態(tài)或性質(zhì) 不整合 不整合性 | unconformable 不整合的 | unconformablecontact 不整合接觸

unconformable contact：不整合接觸面

unconformability 不整合 | unconformable contact 不整合接觸面 | unconformable stratification 不整合層理

unconformable surface：不整合面

unconformable stratification 不整合層理 | unconformable surface 不整合面 | unconformable 不整合的

unconformity：不整合

上升可以形成侵蝕面,然后又被新沉積物所覆蓋,這種埋藏的侵蝕面稱為不整合(unconformity). 可以用它來(lái)確定地層的相對(duì)年代. 主要的不整合有非整合(nonconformity)91中文视频在线观看、角度不整合(angular unconformity)、 平行不整合(disconformity)和小間斷(diastems).

angular unconformity：角度不整合

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unconformability：不一致的狀態(tài)或性質(zhì) 不整合 不整合性

unconfirmedoffer 虛盤(pán) | unconformability 不一致的狀態(tài)或性質(zhì) 不整合 不整合性 | unconformable 不整合的