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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.

分析和讨论了沉积盆地在各个阶段的构造背景特征及其演化过程,初步恢复了每个阶段盆地的岩相古地理格式,绘制了盆地的构造古地理格架图和沉积盆地演化模式图。

Under the rock characteristics, the signs of biological and sedimentary structure will be divided into open lagoon, tidal flat, open platform, and sea-level changes, palaeogeography are discussed.

根据岩石特征,生物与沉积构造等相标志,将其划分为开放泻湖、潮坪、开阔台地等沉积相,并对海平面升降,古地理作出讨论。

The study of sedimentation manganese ore deposit from material source、sediment mineralization to the quality of control basin、attribute、palaeogeography、microfacies、sequence stratigraphy, etc.

沉积锰矿床的研究已从单纯研究锰的物质来源、沉积成矿作用等,转向控锰盆地的性质、属性、古地理及微相、沉积层序的研究。

Biogenic silica content was determined in 25 surface sediment samples from the southern South China Sea to study its distribution and its modern oceanic environmental significance, which may provide further scientific evidence for paleoceanography explaination.

对南海南部25个表层沉积样进行了生物硅的测定分析,试图揭示南海南部表层沉积生物硅的分布及其对现代海洋环境的指示意义,以便为古海洋学研究提供进一步的科学依据。

According to the consolidation ratio,the original thickness of deposits at certain depth can be calculated,too,so that it is possible to delineate the lithofacies—paleogeographic profile of original deposits.

根据压实比换算出过去一定埋深范围内的原始沉积厚度,从而作出原始沉积的岩相古地理剖面图。

Through a detailed field surveying of Fenghuangshan section of Chaobei area and systematic studies on petrology,petrography and sedimentology,especially on microfacies ,analyzed paleogeographic characteristics and depositional environment.

通过对安徽巢北凤凰山剖面进行详细的野外测量和系统的岩石学、岩相学、沉积学的研究,尤其是进行岩石微相研究,分析其古地理特征及沉积环境。

The concept of stratigraphic pile-up sequences and decomposition model of overlapping process of Logistic chaotic series are applied to extract the weak signal for the sequence of lithologic ratio parameters, which has established the basis for dynamic modeling of three dimensions in the paleogeographic environment of hydrothermal sedimentary basin.

运用地层垒积序列的概念和Logistic混沌序列叠加过程分解模型,对岩比参数序列中的弱信号进行提取,进一步研究热水沉积作用强度演化的定量特征,为对热水沉积盆地古地理环境进行三维动态模拟奠定了基础

By substantive field and indoor practice development work, this paper systemic researched the source, the sedimentary system, sedimentary facies, paleogeographic environment, under the guidance of sedimendary geology and petrolume geology theory.

论文通过大量的野外和室内的研究工作,结合现代沉积地质学和石油地质学理论,对鄂尔多斯盆地堡子湾地区延长组长6的物源方向及母岩性质、沉积相的确定标志及类型特征、古地理环境特征进行了系统全面的研究。

The concept of stratigraphic pile-up sequences and decompositionmodel of overlapping process of Logistic chaotic series are applied to extract the weak signal for the sequence of lithologic ratio parameters, which has established the basis for dynamic modeling of three dimensions in the paleogeographic environment of hydrothermal sedimentary basin.

运用地层垒积序列的概念和Logistic混沌序列叠加过程分解模型,对岩比参数序列中的弱信号进行提取,进一步研究热水沉积作用强度演化的定量特征,为对热水沉积盆地古地理环境进行三维动态模拟奠定了基础。

Based on the synthetic study of field outcrops, drilling section data, charts drawn in rooms, and data of stratigraphic correlation, the authors propose that the paleogeographic pattern of Ordos Basin was a fan fluvial sedimentary system at Jurassic Fuxian Stage.

在综合研究野外露头、钻井剖面及室内编图、地层对比的基础上,指出鄂尔多斯盆地冲积扇-河流沉积体系是侏罗纪富县期主要的古地理格局,富县期沉积受与古地貌密切相关的五条河谷控制。

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