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Based on the date of outcrop, log and lithology, sequence stratigraphic division and correlation were made on Neopaleozoic in south of North China Basin, and high-precision geologic correlation framework was built up in the basin.

以露头、测井和岩性资料为基础,对华北盆地南部上古生界进行了层序地层的划分与对比工作,建立了盆地范围内的高精度地层对比格架。

In the term of sedimentary features of Neopaleozoic in south of North China Basin, lateral variation of sedimentary facies was studied selectively in Benxi-Taiyuan Formation, Shanxi Formation, Lower Shihezi Formation, Upper Shihezi Formation and Shiqianfeng Formation. Lithofacies paleographic features and the sedimentary evolutionary process of Late Paleozoic in south of North China Basin were worked also.

根据华北盆地南部上古生界的沉积特点,按本溪组—太原组、山西组、下石盒子组、上石盒子组和石千峰组5个层组分别开展了沉积相的横向变化对比研究,并以此为基础探讨了华北盆地南部晚古生代的岩相古地理特征及其沉积演化过程。

Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei palaeohigh s in Tarim Basin;2. The palaeohigh in Junggar basin underwent multistage evolution from Neopaleozoic to Cenozoic, and four basic types such as successional, discontinuous, tilted and thrust ones were developed.

准噶尔盆地古隆起经历了自晚古生代至新生代的多期次演化,发育了继承型、间断型、掀斜型和冲断带型等4种古隆起基本类型,通过构造沉积演化及油气成藏分析探讨了陆梁隆起、莫索湾凸起、车莫隆起的油气勘探领域和勘探方向。

By comprehensive analysis of the characteristics of formation and reconstruction, six tectonic belts in the northeast part of Junggar basin were divided: marginal obduction zone in Early Paleozoic(O1-2)?melange mag-ma collision zone of late Paleozoic (D1), volcanic arc-compression zone of Late Paleozoic (D1), back-arc folded belt of Late Paleozoic (D2_3), marginal depression folded belt of Late Paleozoic (C1-P2) and foreland basin gentle anticline belt of Mesozioc era, etc.

通过&建造&与&改造&特征的综合分析,划分了准噶尔盆地东北缘的构造带:早古生代(1-2)陆缘逆冲带;晚古生代(D1)混杂岩浆碰撞带;晚古生代(D1)火山岩浆岛弧挤带;晚古生代(D2-3)弧后盆地褶皱带;晚古生代(C1-P2)陆缘盆地褶皱带以及中生代前陆盆地平缓背斜带等6个构造带。

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.

川东北飞仙关组鲕滩储层是四川盆地重要的勘探目的层,受成岩作用的改造非常强烈。

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.

本文对松辽盆地白垩纪嫩江组介形类化石壳体表面毛细管孔的显微构造特征研究表明,白垩纪嫩江组沉积时期,松辽古湖盆应为一陆相沉积体系,其水体性质应为淡水—少盐水的古湖泊环境。

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.

比如盆地内有机质以高成熟和过成熟为主,主要处于生气阶段,地表地球化学异常较高,盆地中部异常最显著,凯蒙呷拉蒙地区具有一定的含油气远景,为油气勘探的有利区带。

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.

调节池出水进入好氧单元,通过生物的降解作用,使有机污染物得到彻底的降解,好氧单元进水进入沉淀单元,沉淀单元出水自流进入中间水池;在中间水池由泵提升至微絮凝单元,水中残留溶解性有机物与过滤前投加的混凝剂反应生成悬浮固体通过过滤罐滤除,微絮凝过滤出水进入消毒区,在消毒区内利用二氧化氯的强氧化性达到杀菌目的。

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.

库车盆地分布有沉积广厚、层数众多的古近纪和新近纪石盐岩,是我国最有找钾希望的内陆成盐盆地之一。

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.

从盆地的构造分异结果及其控制的含盐系和其中石盐岩的发育特征来看,古近纪和新近纪库车盆地已具备钾盐蒸发岩形成的构造条件。

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