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These sedimentary structures, including the domal structure, the irregular reticular and the irregular chaotic tepee ridges, and the palimpsest ripple, make up an association of the microbial induced sedimentary structure.

这些沉积构造包括穹窿状构造、规则网状和杂乱的帐篷脊、变余波痕等,构成一个潮下相灰岩层面上的特别的微生物形成的沉积构造(Microbial Induced Sedimentary Structure, MISS)组合。

This paper mainly studies the sedimentary characteristic s and sedimentary facies,the features of hydrocarbon resource rock,the production time of ejectment hydrocarbon and the condition of movement.

主要对塔里木盆地孔雀河斜坡带寒武—奥陶系的沉积特征和沉积相、烃源岩的特征以及生烃时间、运移条件等进行了研究,认为该地区油气源充足,具备了形成大型油气藏的基础,指出塔东一井东、北、西北一带,其次是群克1井以南地段,是重点寻找寒武—奥陶系油气的远景区块。

TheJiyang depression located in paleomonsoon climate zone in the period of the sahejieformation sedimentation, the wet and hot climate made ancient lake become deeperwater, enhanced stratification, reduced primary productivity of plankton, decreasingsedimentary velocity of carbonate, increasing sedimentary velocity of clay, fortifiedreductibility on certain degree, and then would be available for development of blackshale, dark shale and oil shale; In the contrast, the cold and dry climate lead ancientlake to shallower water, subdued stratification, increaser primary productivity ofplankton, enhancive sedimentary velocity of aphanitic carbonate, decreasedsedimentary velocity of clay, and then would be available for development calciteshale, calcite laminar shale, calcite mudstone, shaly carbonate rock, even laminarcarbonate or dolomite rock.

济阳坳陷在古近系沙河街组沉积期属于古季风气候带,在湿热的气候条件下古湖水加深,分层性增强,浮游生物的古生产力降低,隐晶碳酸盐的沉淀速率变小,粘土沉积速率加快,还原性一定程度上有所加强,有利于黑页岩、油页岩和暗色泥岩的形成:而相对干冷气候下,古湖水变浅,分层性减弱,浮游生物的古生产力增高,隐晶碳酸盐的沉积速率变大,粘土的沉积速率减慢,有利于钙质页岩、钙质纹层页岩、钙质泥岩、泥灰岩甚至纹层状碳酸盐岩、灰岩的发育。

The late period of loess accumulation with high contents of hornblende and epidote is mainly far-source sedimentary with wind transport, and the early and middle periods of loess accumulation with high contents of magnetite and dens are mainly near-source sedimentary with complex transport.

普通角闪石、绿帘石含量较高的黄土堆积后期是以远源沉积为主,且以风力搬运为主;磁铁矿、岩屑含量较高的早、中期是以近源沉积为主,搬运动力较复杂。

The late period of loess accumulation with high contents of hornblende and epidote is mainly far source sedimentary with wind transport, and the early and middle periods of loess accumulation with high contents of magnetite and deris are mainly near-source sedimentary with comp lex transport.

普通角闪石、绿帘石含量较高的黄土堆积后期是以远源沉积为主,且以风力搬运为主;磁铁矿、岩屑含量较高的早、中期是以近源沉积为主,搬运动力较复杂。

Therefore, it is important to study the sedimentary characteristics and the distribution pattern of sedimentary facies in this area.

因此,详细开展滩海西部地区沉积特征及沉积相分布规律的研究具有重要的影响和意义。

Palaeodepth analysis in sedimentary period is the base of study on sedimentary facies.

沉积时期的古水深分析是沉积相研究的基础。

So blocking out sedimentary microfacies and studying distribution of sedimentary facies are important content in this study area.

由于其上三叠统延长组油气的富集主要受有利储集相带的控制,所以进行沉积相研究,探讨沉积微相的平面展布与油气富集之间的规律,是该区的一相重要研究内容。

The lithologic pool such as that developed in the actic region while the basin is rifting or in the glacis region while the basin is depressing all which can be found in this basin. Five kinds of sedimentary facies and thirteen sedimentary parfacies can be found in the Shengbei concave during the period of Jurassic series and Cretaceous series.

在该盆地内部既有可能发育断陷期陡坡带的岩性油气藏,又有可能发育坳陷期缓坡带的岩性油气藏,其胜北洼陷在中侏罗统-白垩系沉积时期主要发育5种陆相沉积相类型、10种沉积亚相类型。

In a comprehensive study of various macro-and micro-heterogeneous reservoir parameters on the basis of the reservoir quality, we launched a comprehensive evaluation to determine the evaluation criteria. The reservoir quality in 2+3 was divided into three types. The research shows that distribution of interlay and insulating layer is controlled by sedimentary microfacies. The developmental stages and the size of the sedimentary microfacies determine the plane and the vertical distribution of interlay and insulating layer.

本研究运用高分辨率层序地层学的原理和方法,从油田生产的实际需要开发,将双河油田Ⅶ下单元的14个小层,重新划分为31个;在综合研究各种储层宏观和微观非均质性参数对储层质量影响的基础上,开展了储层多参数综合评价,对Ⅶ下单元的隔夹层进行研究,绘制了各小层的平面分布图,并对Ⅶ下单元的31个活动单元划分为4种类型,在平面上画出了所有小层的评价图。

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整个国家陷入内战状态之后,大名往往拥有小而巩固的领地,领地内所有土地都属于他们自己或他们的家臣。