The oolitic shoal reservoir in the Feixianguan Formation in the northeastern Sichuan basin, which has undergone strong diagenesis, is an important exploration target in the Sichuan basin.

川東北飛仙關(guān)組鮞灘儲層是四川盆地重要的勘探目的層色玖二代，受成巖作用的改造非常強烈三级黄色视屏。

The study on microstructure characteristics of the five pores on the surface of ostracoda at Nenjiang Formation of Songliao Basin in Cretaceous shows that during the depositional period of Nenjiang Formation in Cretaceous,Songliao Basin should be a continental depositional system and palaeolacustrine enviroment and furthermore its water body property should be fresh saltish.

本文對松遼盆地白堊紀(jì)嫩江組介形類化石殼體表面毛細(xì)管孔的顯微構(gòu)造特征研究表明国产一级精品A片观看视频，白堊紀(jì)嫩江組沉積時期一级黄片在线精彩视频免费播放，松遼古湖盆應(yīng)為一陸相沉積體系，其水體性質(zhì)應(yīng)為淡水—少鹽水的古湖泊環(huán)境91日韩在线观看视频。

The organic matter are high mature or overmature and at the gas-generating stage. In Biru basin, there occurs high surface geochemical abnormality, especially in the center of the basin.

比如盆地內(nèi)有機質(zhì)以高成熟和過成熟為主韩国aa人人清清片中国aa人清，主要處于生氣階段，地表地球化學(xué)異常較高丁香色色五月天，盆地中部異常最顯著，凱蒙呷拉蒙地區(qū)具有一定的含油氣遠(yuǎn)景国产高清在线a视频大全在线，為油氣勘探的有利區(qū)帶欧美一级多人婬片人妻欧美大片。

The regulating reservoir water leakage enters the oxygen unit, through the biological degeneration function, enable the organic pollutant to obtain the thorough degeneration, the good oxygen unit enters the water to enter the precipitation unit, the precipitation unit water leakage flows automatically enters the middle basin; In the middle basin by the pump promotion to the micro flocculation unit, in the water before the residual soluble organic matter and the filtration throws the coagulant response production suspended solid which adds through the filtration pot filtration, the micro flocculation filtration water leakage enters the disinfection area, achieves the sterilization goal in the disinfection area using the chlorine dioxide strong oxidability.

調(diào)節(jié)池出水進(jìn)入好氧單元，通過生物的降解作用欧美精品二区三区中文，使有機污染物得到徹底的降解久久午夜一级A片，好氧單元進(jìn)水進(jìn)入沉淀單元，沉淀單元出水自流進(jìn)入中間水池亚洲国产日韩你懂的网址；在中間水池由泵提升至微絮凝單元av网站有哪些，水中殘留溶解性有機物與過濾前投加的混凝劑反應(yīng)生成懸浮固體通過過濾罐濾除，微絮凝過濾出水進(jìn)入消毒區(qū)精品国产区，在消毒區(qū)內(nèi)利用二氧化氯的強氧化性達(dá)到殺菌目的99精品自拍视频在线播放。

There are a lot of layers of Palaeogene ang Neogene halite which are widely distributed in Kuqa basin. So Kuqa basin is one of the inland salt basins in which it is the most hopeful to search potash in China.

庫車盆地分布有沉積廣厚、層數(shù)眾多的古近紀(jì)和新近紀(jì)石鹽巖久久AV免费这里有精品，是我國最有找鉀希望的內(nèi)陸成鹽盆地之一欧美在线人一区二区三区视频。

The result of the basin's tectonic differentiation and the development of the salt-bearing strata indicate that in Palaeogene ang Neogene, the Kuqa basin had already had the tectonic environment in which the potash evaporite formed.

從盆地的構(gòu)造分異結(jié)果及其控制的含鹽系和其中石鹽巖的發(fā)育特征來看亚洲黄色欧美，古近紀(jì)和新近紀(jì)庫車盆地已具備鉀鹽蒸發(fā)巖形成的構(gòu)造條件。

It stably subsided after its formation. During Palaeogene ang Neogene salt-forming, Kuqa basin experienced strong-weak-strong tectonic stages, and its center of subsidence moved gradually from north to south and depocenter from northwest to east and southeast. Because of tectonic differentiation, series of second depression formed in Kuqa basin.

盆地自形成以來一直處于穩(wěn)定的沉降狀態(tài)亚洲日韩国产高清mp4，在古近紀(jì)和新近紀(jì)成鹽期免费欧美日韩一区二区视频，盆地經(jīng)歷了強-弱-強3個構(gòu)造演化階段，其沉降中心由北而南逐漸遷移99h久久久精品，沉積中心由北西逐漸向東91超碰在线播放、南東方向遷移，盆地內(nèi)的構(gòu)造分異漸趨明顯激情亚洲欧美另类录音，形成了一系列次級凹陷美日韩国产综合一区www。

The paper discusses five key points in the qualitative reconstruction: 1 timely, to combine a study of "reversed succession", 2 spatially, to synthesize a study of "inversion tectonics", 3 to emphasize significance of structural restoration in palaeogeographic reconstruction, 4 reformation events in the period of basin formation serving as a link between past and future, and 5 a study on basin geodynamics matched with the orogenic geodynamics.

文章討論了定性重建中的5個要點：l時間上，要結(jié)合&反序&的研究人妻少妇看A片偷精品视频，2空間上天堂婷婷久久，要結(jié)合&反轉(zhuǎn)構(gòu)造&的研究，3強調(diào)構(gòu)造復(fù)位在古地理重建中的意義上海黄色录像免费一级，4盆地建造階段中的改造事件所起的承前啟后作用人人操人人插人人射人人人，5盆地動力學(xué)與造山動力學(xué)的結(jié)合研究。

The basin's continental tectonic settings and its evolution of each phase is also discussed, and the lithofacies palaeogeographies of each phase are analyzed elementarily. At the same time, the tectonic palaeogeography and sedimentary basin evolution model diagrams are drawn.

分析和討論了沉積盆地在各個階段的構(gòu)造背景特征及其演化過程国产黄网站在线免费观看，初步恢復(fù)了每個階段盆地的巖相古地理格式欧美一级AA大片免费观看，繪制了盆地的構(gòu)造古地理格架圖和沉積盆地演化模式圖。

Silicalites, predominated by pelitic silicalite, occur in collisional zones and back-arc basins. In the collisional zones, they occur as rock sheet as an important part ofophiolitic mé lange, belonging to ophiolitic mélange type silicalite. In the back-arc or interarc basin, they occur as pelitic silicalite intercalation varying in thickness, characteristic of "silica merl",and belonging to abyssal back-arc basin type or carbonate type silicalite. In the magmatic arc, they occur as intercalation related to volcanic hydrotherm or volcalic exhalation, belonging to volcanic arc type silicalite.

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