According to the formative mechanism of deep basin gas,the pool-forming mechanism of Fu-yang oil layer in Songliao Basin was studied from the aspects of depositional reservoir character,overpressure of source rock,power of hydrocarbon migration and hydrocarbon distribution.

借鑒深盆氣的形成機(jī)理精品国产一区二区三区国产区，從沉積及儲(chǔ)集層特點(diǎn)、烴源巖超壓、油氣運(yùn)移動(dòng)力、油水分布特征等方面深入剖析松遼盆地扶楊油層的成藏機(jī)制野外一级黄色网站。

The deep basin reservoir pool-forming pattern of Fu-yang oil layer is established, by which a great resource potential is forecasted in the deep basin reservoirs.

建立了松遼盆地扶楊油層深盆油藏成藏模式，預(yù)測(cè)松遼盆地深盆油藏的資源潛力巨大亚州中文字幕精品一区，指出應(yīng)轉(zhuǎn)變勘探思路欧美激情在线观看A片大电影，向富油坳陷拓展岛国AAAA级午夜在线影院，轉(zhuǎn)變資源定位国产日韩一本无码免费专区，調(diào)整預(yù)探目標(biāo)和勘探技術(shù)序列，勘探深盆油藏免费一级无码婬片A片。

Greywacke samples of Middle and Late Triassic collected from Hongcan well in Zoige were analyzed by ICP-MS for REE and trace elements. The result shows that these samples were originated continental crust because they enriched in Cs,Rb,Th and high REE contents and depleted in Sr,Nb and Ta. Negative Eu anomalies and strong differentiation between heavy and light REE are significant. Both the contents and ratios of the inactive trace elements and the results based on discriminant diagrams indicated that the sedimentary tectonic setting of Zoige Basin was dominated by continental island arc and the sediment in this basin was strongly affected by continental island arc between Middle and Late Triassic.

對(duì)若爾蓋地區(qū)的紅參一井內(nèi)中三疊世中期和晚三疊世中期的37個(gè)雜砂巖樣品進(jìn)行了ICP-MS微量元素分析黄片一级片一区，其結(jié)果顯示這些砂巖樣品具有Cs、Rbyinyuan国产精品、Th等元素富集日韩性交无码视频，Sr、Nb和Ta虧損国产真实迷奸系列，稀土元素總量較高超清无码波多野吉衣中文，且負(fù)Eu異常和輕重稀土分異明顯等殼源物質(zhì)的特征；而微量不活動(dòng)元素的含量及比值特征以及構(gòu)造環(huán)境判別圖解的判別結(jié)果表明：若爾蓋盆地中三疊世中期到晚三疊世中期的沉積構(gòu)造環(huán)境為大陸島弧99最新视频，沉積物源受到大陸島弧的強(qiáng)烈影響免费看操网站。

Basic geological conditions for migration and accumulation mode of the deep marine basin are similar to the shallow ones, but the basin has deeper sags and rifts, bigger deposits and infillings, developed source rocks, and good source-reservoir-caprock associations.

該深水盆地油氣運(yùn)聚成藏的基本地質(zhì)條件亦與淺水區(qū)類似，但陸坡深水區(qū)凹陷裂陷更深A级毛片毛片免贯观看久、沉積充填規(guī)模更大中文字幕人妻日韩久久，且發(fā)育4套烴源巖和3套儲(chǔ)蓋組合類型，使深水油氣運(yùn)聚成藏有了良好的基礎(chǔ)久久网站国产精品。

By using a method of theoretical analysis combining with practical application, the author studies the theory and methodology of taking a river basin as an integral unit to manage water environment in the background of administrative regional management, so as to provide a guidance to implement river basin management.

本文采用理論與實(shí)踐相結(jié)合的方法免费不卡黄网站在线观看，探討了在行政區(qū)域管理體制背景下的江河流域水環(huán)境管理的原理與方法，以便為實(shí)施流域水環(huán)境管理提供理論與方法上的指導(dǎo)在线看无码黄又污的网站。

This dissertation focuses on the basin geothermal history, tectonothermal evolution and the relationship between geothermal field evolution and hydrocarbon generation Based on the research of present-day geothermal field, geothermal history of Eastern Subdepression of Liaohe Basin was reconstructed with available data from drillings, loggings, seismic cross-sections, BHTs and thermal indicators

本文綜合運(yùn)用鉆井九九草影院、測(cè)井、地震欧美一级a一片免费观看、古溫標(biāo)等數(shù)據(jù)資料国产免费黄片视频在线播放，在現(xiàn)今溫度場(chǎng)研究的基礎(chǔ)上對(duì)遼河盆地東部凹陷新生代熱歷史進(jìn)行了恢復(fù)。全文以盆地?zé)崾费芯繛橹骶€欧洲美女色黄A片,视频，進(jìn)行了盆地構(gòu)造-熱演化分析操h网站，并探討了溫度場(chǎng)演化與油氣形成之間的關(guān)系99在线视频精品。

Referencing to the internal and external documents, we have plotted the balanced evolutions for the various typical structures by computer, which is the first time at home; applied the balancing technique by computer to the representative structures in Sichuan Oil and Gas Basin, and also established the geological modellings on three different structural elements and their own balanced evocutions in Sichuan Basin.

借鑒國(guó)內(nèi)外的資料，在國(guó)內(nèi)首次用計(jì)算機(jī)繪制出各種典型構(gòu)造的平衡演化剖面www精品.国产，并應(yīng)用機(jī)制平衡技術(shù)對(duì)四川油氣盆地內(nèi)的代表構(gòu)造作了詳細(xì)的平衡計(jì)算泰国一级牲交片，建立起四川盆地內(nèi)三個(gè)不同構(gòu)造單元的地質(zhì)模型以及構(gòu)造平衡演化剖面。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根據(jù)Ar-Ar熱年代學(xué)研究女人逼的视频，精確測(cè)定了早二疊世伸展變形和晚二疊世擠壓變形的峰期時(shí)代分別為290Ma和259Ma.2欧美激情性A片三p、提出了關(guān)于哈爾里克山南麓小鋪一帶變質(zhì)帶和變質(zhì)作用的新認(rèn)識(shí)根據(jù)顯微觀察資料和特征變質(zhì)礦物的出現(xiàn)，把小鋪一帶的變質(zhì)巖由SW向NE方向依次劃分為黑云母帶黄片视频在线播放、石榴石帶最新国模吧、十字石帶、紅柱石帶和矽線石帶等變質(zhì)帶日韩一区高清在线播放免费；初步確定該區(qū)的變質(zhì)作用屬于中溫-低壓型免费黄色强奸A片，變質(zhì)作用發(fā)生的時(shí)代為290Ma左右，是該區(qū)早二疊世地殼伸展的產(chǎn)物亚洲黄色高清视频在线观看。3欧美,性爱精品亚洲性爱免费观看视、首次提出哈爾里克山南麓在石炭紀(jì)可能發(fā)育弧后盆地的新觀點(diǎn)根據(jù)哈爾里克山南麓原&居里得能組&巖屑砂巖的碎屑鋯石SHRIMP U-Pb定年，確認(rèn)這套地層的沉積不早于晚泥盆世啪啪啪com，很可能是石炭紀(jì)日韩欧美国产一区呦呦，而不是前人所說(shuō)的前寒武紀(jì)；結(jié)合對(duì)其區(qū)域地質(zhì)背景免费观看肉肉啪啪污网站、源區(qū)位置和沉積環(huán)境分析在线午夜视频，推測(cè)該區(qū)石炭紀(jì)可能為滯后弧后盆地和弧后隆起區(qū)構(gòu)造背景。4黄色网站在线观看欧美、進(jìn)一步證明哈爾里克山不發(fā)育與島弧演化相關(guān)的泥盆紀(jì)巖漿活動(dòng)根據(jù)對(duì)代表性閃長(zhǎng)巖和花崗巖的鋯石SHRIMP年代學(xué)研究獲得的新資料自拍偷拍ww，結(jié)合該區(qū)已有相關(guān)資料的綜合研究，確定哈爾里克山巖漿巖分別形成于奧陶紀(jì)-志留紀(jì)和石炭紀(jì)晚期-二疊紀(jì)久久国产精品首页久久久精品，不存在泥盆紀(jì)的巖漿巖国内精品嫩模AV私拍，進(jìn)而認(rèn)為該區(qū)泥盆紀(jì)不屬于島弧環(huán)境。5亚洲5566、重建了哈爾里克山古生代以來(lái)的地質(zhì)演化過(guò)程根據(jù)區(qū)域資料以及本次研究所獲得的資料无人区卡一卡二卡三乱码直播，把哈爾里克山古生代以來(lái)的構(gòu)造演化劃分中奧陶世-早志留世為島弧、中志留世-晚泥盆世為弧后區(qū)中文字幕免费黄色网站、石炭紀(jì)弧后伸展爱搞社区、二疊紀(jì)為后碰撞伸展與擠壓、中生代差異隆升和晚新生代陸內(nèi)再造山過(guò)程等構(gòu)造階段欧美黑人一级A片在线高清。6欧美一区二区精品视频中国、初步估算了哈爾里克山地殼縮短率和縮短量根據(jù)前中生代地層褶皺估算的哈爾里克山南山口-口門子、石城子-白石頭和沁城-小鋪三條剖面的地殼縮短率分別為16.2%www.黄色网站在线视频、19.8%和20.1%一级毛片一级毛，相應(yīng)的地殼縮短量分別為4.3km久久精品国产精国、9km和11.3km。

The results of investigation show that the crust in Junggar basin features continental character, and the basement of the basin is characterized by two-layer structure, the upper layer is Hercynian folded basement, and the lower is Pre-Cambrian crystalline basement.

結(jié)果表明欧美黑人又粗又长精品，準(zhǔn)噶爾盆地地殼具有陸殼性質(zhì)高端自拍无码在线，基底為雙層結(jié)構(gòu)，上層為海西運(yùn)動(dòng)期褶皺基底色污网站网站，下層為前寒武系結(jié)晶基底亚洲精品国精品91，褶皺基底厚度不超過(guò)10 km，在三個(gè)泉凸起以北厚度較大自拍偷拍精品专区，為3~10 km999A片免费看在线播放。

Accordingly, we start the thesis from two small oil fields of Beipu and Laoyemiao in Nanpu depression. Firstly, we analyze regional geology background of the area and find that its structure evolvement can be divided into three greatest stages: the formation and evolution of pre-tertiary basement, the lower-tertiary fault basin and the upper-tertiary depression basin.

因此本論文從南堡凹陷北堡和老爺廟兩個(gè)小型油田入手，首先分析了研究區(qū)的區(qū)域地質(zhì)背景噜噜性爱，明確了其構(gòu)造演化分為三大階段：即前第三紀(jì)基底的形成與演化女生按摩破处视频在线观看、早第三紀(jì)斷陷盆地的形成與演化、晚第三紀(jì)坳陷盆地的形成與演化性爱资源网站。