Three periods petroleum accumulation exists in South-of-fifth-area oil field, the first period oil and gas is the Jiamuhe group mature and high mature hydrocarbon and the Fengcheng group mature hydrocarbon in late Permian to early Triassic, was destroyed in the Indo-Chinese movement intermediate stage, but some still is conserved in good conserved condition, which is one of exploration objects. The second period is the Fengcheng group high mature hydrocarbon in late Triassic to early Jurassic, which is the important exploration target. The third period is the Jiamuhe group overmature dry gas in the late Jurassic Period to the early Cretaceous.

五區(qū)南油氣藏存在三期成藏欧美黑人巨大巨粗性XXXX，第一期是佳木河組過(guò)成熟干氣和風(fēng)城組成熟油氣羞羞自拍无码视频在线观看中文字幕，成藏期在晚二疊世到早三疊世91国内自拍第九页，在印支運(yùn)動(dòng)中期被破壞了，但是在保存條件好的地區(qū)仍存在這一期油氣藏自拍偷拍色，它是勘探的對(duì)象之一；第二期是風(fēng)城組高成熟油氣全彩H漫无遮挡全彩3D，成藏期在晚三疊世到早侏羅世黄色h精品在线，也是勘探的對(duì)象之一在线观看黄v视频国产；第三期是佳木河組過(guò)成熟干氣，成藏期在侏羅紀(jì)到早白堊世国产一区鲁鲁在线视频免费播放。

In the scorch stage, average yield of withered grass of second and third year growth prematurity type of Phleum pratense L. is 10672.5 kg/hm2, by cradling one time per year, average yield of wind hay grass is 7575 kg/hm2, the plant average height of selective colony is 160.0cm, the plant height of colony is rather equality. In the course of general nutrition composition analysis, discover that nutrition value of late-maturity type is higher than nutrition value ofprematurity type, coarse fibre and coarse protein and coarse fat of late-maturity type are 10.7%, 3.58%, 24.82% respectively, coarse fibre and coarse protein and coarse fat of prematurity type are 9.84%, 2.61%, 27.59% respectively, dry matter content of prematurity type is 92.63%, dry matter content of late-maturity type is 92.22%.

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We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

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Results and Conclusions （1）MRI is better than CT to show the lesion of cerebellar fossa and brain stem.（2）Late radiation encephalopathy may be the result of immunal response to the damage of brain tissue and blood vessel after radiotherapy（3） 18 F-FDG-PET is a effective screenage examimation to diagnosis late radiation encephalopathy.（4）To some degree,the symptoms of the patients were alleviated after therapy with dexamethasome,mannital and vitamine B,etc.Late radiation encephalopathy ought to be given priority to prevention and treated vigorously as soon as possible.

結(jié)果和結(jié)論（1）CT對(duì)鼻咽癌遲發(fā)性放射性腦病的診斷有一定價(jià)值黄色免费在线网观看，但MRI對(duì)后顱窩和腦干病變的顯示優(yōu)于CT；（2）遲發(fā)性放射性腦病可能是放療致腦組織血管損傷后引起免疫改變的結(jié)果黄片在线免费看啊啊啊；（3）18-氟代脫氧葡萄糖（ 18F-FDG）-PET是診斷遲發(fā)性放射性腦病的有效的影像學(xué)檢查方法中文字幕欧美亚洲；（4）本組患者經(jīng)應(yīng)用激素、甘露醇在线观看的黄、多種維生素等治療无码免费婬AA片在线视，均取得不同程度的改善。

Sixteen ( 15 new) amphibian and twenty-two ( 11 new) squamate species have been reported across China, including the oldest Chinese tetrapod Sinostega pani from the Late Devonian of Ningxia Hui Autonomous Region, the large stereospondyl amphibian Yuanansuchus laticeps from the Middle Triassic of Hubei Province, Late Jurassic/Early Cretaceous lissamphibians ( e. G., the anurans Callobatrachus sanyanensis and Mesophryne beipiaoensis, the caudates Jeholotriton paradoxus and Laccotriton subsolanus) from Northeast China, Paleogene lizards (e. G., Brevidensilacerta xichuanensis and Tinosaurus yuanquensis) from North China, and numerous lizards from the Late Cretaceous of Nei Mongol Autonomous Region.

共報(bào)道了16種兩棲類和22種有鱗類欧美视频黄网，其中15種兩棲類和11種有鱗類為新種国产精品久久久久久久三级，包括我國(guó)最古老的四足動(dòng)物寧夏晚泥盆世的潘氏中國(guó)螈，湖北中三疊世的大型全椎兩棲類寬頭遠(yuǎn)安鯢播放一级毛片无码免费播放，東北晚侏羅世/早白堊世的多種滑體兩棲類(如無(wú)尾類三燕麗蟾和北票中蟾欧美人妻区精品视频，有尾類奇異熱河螈和東方塘螈)，華北古近紀(jì)的蜥蜴類(如淅川短齒蜥和垣曲響蜥)迷j白嫩玩弄灌醉在线视频，以及內(nèi)蒙古晚白堊世的多種蜥蜴類等欧美风月片在线视频。

The site that is located on the eminence of nose structure, and far-source the underwater distributary channel and estuary bar experiencing the late dagenetic period B is the most promising for accumulation of oil and gas. Vertically, late diagenetic period B sand layer is advantageous for oil and gas gathering, while late diagenetic subperiod A3 sand layer is disadvantageous for oil and gas gathering.

平面上處于鼻狀構(gòu)造高部位，又處于晚成巖B期的遠(yuǎn)源水下分流河道尤物成人最新电影在线观看网站视频、河口壩是最有利于油氣富集的部位五月综合色婷婷开心网潮喷；縱向上，晚成巖B期的砂體有利于油氣聚集影音先锋你懂，而晚成巖A3亞期的砂體不利于油氣聚集专区在线你懂。

Through the age analysis on apatite and zircon fission track, there have five stages of tectonic movements, respectively occurred in late Trias, from mid-late period in early Cretaceous to late Cretaceous, Eocene, Oligocene and Miocene.

通過(guò)對(duì)盆地內(nèi)磷灰石和鋯石年齡分析，焉耆盆地存在5期構(gòu)造運(yùn)動(dòng)：晚三疊世日韩一级AAAAAAAA毛片、早白堊世中晚期-晚白堊世少妇无码一区二区三区免费视频、始新世、漸新世和中新世免费欧美网黄色网站。

The late Triassic strata unconformably overlying the granite indicates that the formation time of these thrust structures might be from the late Permian to the early Triassic, no later than the Late Triassic.

西北緣晚三疊世地層不整合覆蓋于花崗巖之上99丫视频，這種現(xiàn)象將本區(qū)沖斷構(gòu)造發(fā)生的時(shí)間限定為晚二疊世至早三疊世，最晚不超過(guò)晚三疊世又粗又大又长的免费视频。

Based on the regional tectonic evolution, combined with the high precision isotopic ages from this paper and other geologists, we have some new acquaintances as follows: 1 There has no Caledonian granite belt distributed in north margin of North China Craton. So, the traditional evolving model of North China Carton, which formed on this idea and the acquaintance about the collision of North China plate and Siberian plate, must be incorrect; 2 The age date show that the earliest magmatic activity began since late-Palaeozoic Permian, which is inconsistent with the previous idea that there were Caledonian and Hercynian active continental margin in the north of North China Craton and in the south Xingkai Massif. 3 the crust and lithosphere were thickened by the subduction and collision of Siberia plate and North China plate during Late Paleozoic. The magma is formed when the crust is heated and melts caused by thickened lithosphere delamination and caused the Asthenosphere upwelling. But only a little basaltic magma erupted, most magma underplate under the bottom of the crust. Thermal energy derived from basaltic magma underplating made the middle and lower crust melt partially and the late Permian-early Triassic granites is formed in large scale.

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Some scholars believe that the Late Ming Dynasty carried out a double-recognition policy toward Annan but, through the analysis of the Late Ming Dynasty's diplomatic relationship with the Li and the Mo governments and its disposal of bonier disturbance, this thesis maintains that the Late Ming Dynasty did not break away from the One-Annan policy.

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