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During the sediment of late Cretaceous Taizhou Formation and Paleocene Epoch Funing Formation, Subei Basin have formed dark shale containing lots of ostracoda that include predominated whole basin E12 Formation and E14 Formation and local K2t2 Formation, which have become main source rocks of the basin.

海侵的原因,可能是从晚白垩世晚期起,中国东部的地应力条件以引张力占优势,并在华北-渤海湾、苏北-南黄海和东海陆架区,发育了一系列为早第三纪巨厚沉积物所充填的半地堑箕状盆地,海水由东海向黄海海侵,造成陆架上箕状盆地在短时期内与海水相通。

Integrated analysis based on stratigraphy, sedimentary facies and paleophysiography data indicate that small basin-mountain pairs formed in the Kuche Basin during early Mesozonic, and large basin-mountain pairs.

地层、沉积相,生物古地理等综合分析表明库车盆地中生代早期形成了小波长盆山共轭对,中晚期为大波长盆山对。

Directed under plate tectonics theories, author applied the relationship between orogenyy belt and basin, analyzation of proto-type basin restoration of Paleo-structures etc to systematically draw the Paleo-structural maps and Paleo-sedimental photographical maps on Z, O, S, D, C, P, T, J, K, E, N〓j, N1〓k, N〓k etc in Tarim basin.

以板块构造理论为指导,运用造山带与盆地、原型盆地分析、古构造分析等分析方法,系统编制了Z、O、S、D、C、P、T、J、K、E、N〓j、N〓K,N〓K等盆地及周缘古构造岩相图,全面系统地研究和恢复了塔里木大型叠合复合盆地构造演化历史,并将塔里木盆地构造演化史划分为7个构造演化阶段。

In Chapter 4, using the points of view of dissipative theory, the dissipative structure characteristics of ecological-economic system in the Changjiang River basin is analyzed, the development course and evolution characteristic of the ecological-economic system in the Changjiang River basin is demonstrated, and at last the negentropy sources and the entropy value of the ecological-economic system in the Changjiang River basin is radicated.

第四章运用耗散结构观分析研究了长江流域生态经济系统耗散结构特征,并用耗散结构理论论证了长江流域生态经济系统演变过程与演化特征,最后确立了长江流域生态经济系统的负熵源与熵值。

Analysis on mineral characteristics (percent of shingly fragment, maturation index and heavy mineral coefficient of stability) and depositional environment in Mesozoic remanet strata show that provenance located in the north of Yanqi basin, clast were moved from north to south in Mesozoic, and the sedimentary environment in northern basin were braided stream facies while shallow lacustrine stream facies in southern basin.

通过对焉耆盆地现今残留中生代地层中的岩矿特征(碎屑含砾百分比、成熟度指数和重矿物稳定系数)及沉积环境分析,焉耆盆地中生代物源区位于盆地北部,碎屑由北至南搬运;盆地北部为辫状河相沉积环境,南部为浅湖相沉积环境。

On the other hand, there are no open sets in riddled basin but there are open sets in wada basin. The further study hints that this complex basin may be caused by riddling bifurcation and local-global riddling bifurcation.

通过比较发现该复杂筛形域的不确定性指数接近于零而Wada域的不确定性指数明显大于零;在该复杂筛形域中不存在开集,而Wada域中则存在着开集。

Based on the previous researches, combined with the further understanding of the present oil\|gas exploration, the exploitation of the Junggar basin, the analysis of the sedimental strata characteristics in different stages and the mountains profiles on the margin of the Junngar basin, it is considered that there are three\|period foreland basins formed since the Permain in Junggar basin.

基于前人的研究成果,结合在准噶尔盆地油气勘探开发实践中取得的新认识和对准噶尔盆地周缘盆—山耦合区带地质剖面及盆地不同时期沉积地层特征的分析,认为该盆地自二叠纪以来发育了3期前陆盆地,这3期前陆盆地及与其相关坳陷的组合和叠加是形成准噶尔盆地丰富油气资源和多样化成藏模式的主要原因。

The transfer structures in Bohai Bay Basin can be divided into two styles of transfer zone and transfer fault according to the connection or non-connection status. The transfer structure in Bohai Bay Basin is mainly exhibited in the style of transfer zone, especially in basin or depression, while the transfer fault only militates in the sag-control level.

将渤海湾盆地变换构造分为变换带和变换断层两种类型:一般表现为变换带样式,尤其是在盆地或坳陷层次;而变换断层仅在局部的控凹层次上有所体现。

Therefore, taking as examples the Qinshui Basin, Fuxin Basin in China, and the Powder River Basin in the U.S.A, it is discussed both high rank and low rank CBM reservoiring, and it is analyzed the different Impacts of groundwater's supply, movement, drainage, and stagnant nowadays on the rebuilding and adjustment of the CBM reservoir afterwards.

为此,以我国沁水、阜新盆地和美国粉河盆地为例,探讨了高、低煤阶煤层气的成藏过程,分析了现今地下水的补给、运移、排泄和滞流等格局对煤层气藏后期调整和改造所起的不同作用。

The Jianghan basin is a Cretaceous-Paleogene rifted basin developed on Yangtze paraplatform and also a typical continental petroliferous basin containing salt layers.

江汉盆地是在扬子准地台上发育起来的白垩系—古近系断陷盆地,也是我国陆相盆地中典型的含盐含油气盆地。

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