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Cycle are divided into for the phosphoric rock series of the Yangshui Formation at this zone, in association with sequence interface and its relative characterization, the types of the sequences are determined and the Yangshui Formation is considered a high-ranking I-level sequence that is constituted by a series of low-grade retrograding type of de.

应用层序地层学的概念和方法,从沉积特征研究入手,对该区的含磷岩系———洋水组划分出5个沉积层序,结合层序界面及层序的归纳描述,确定了层序类型,并认为洋水组是一套海进体系域中由一系列低级别退积型沉积层序组成的高级层序。

Applying the principles and methods of high-resolution sequence stratigraphy, and combining with the data of exploration wells and development wells in encrypted network of wells, the authors identified 41 short-term base-level cycles of 7 types, which were formed under the conditions of deeping upward, shallowing upward, symmetrical in different accommodation space in Fuyu oil layer of Chao 1-Chao gas 3 blocks, and makes detailed analysis on the genesis and characteristics based on the sedimentary dynamics.

运用高分辨率层序地层学原理和方法,结合探井及密井网开发井资料,在朝阳沟油田朝1-朝气3区块扶余油层识别出向上&变深&、向上&变浅&、对称型及其不同可容纳空间条件下的7类共41个短期基准面旋回,并以沉积动力学观点详细剖析了其成因及特征。

In this paper, the upper member of Eh〓, Shuanghe ~ Zhaoao area, Biyang basin, is treated as a case to study outer and iuner configuration of terrigenous sequence, based on the synthetical analysis of seismic, core, welllog and geological data. Using computer simulation technique of quantitative sequence stratigraphy, accommodation diagram, and baselevel analysis theory, the controling factors. formation, and procedure-responsed mechanics of terrigenous sequence are discussed.

文中以双河~赵凹地区下第三系核三〓段为例,综合利用地震、钻井、测井、地质等资料,剖析了泌阳断陷陆相层序外部构型和内部构型;采用定量层序地层学计算机模拟技术、可容空间图解方法及沉积基准面分析原理,探讨了泌阳断陷陆相层序控制因素、形成机理及其过程—响应机制。

Applying the high-resolution sequence stratigraphy theory,analyzing different scales of base-level cycles and stacking patterns with sediment dynamics,based on 11 well cores and loggings of 825 wells,Fuyu reservoir were classified into 1 long-term level cycle,4 mid-term level cycles and 35 short-term level cycles,proposed sequence framework that is regression followed by transgression.

松辽盆地三肇凹陷扶余油层为典型大型凹陷向斜区油气倒灌式成藏,应用高分辨率层序地层学原理,通过对各级基准面旋回结构、叠加样式的沉积动力学分析,利用11口井岩心和825口井测井曲线,把扶余油层划分为1个长期基准面旋回、4个中期基准面旋回、35个短期基准面旋回,认为扶余油层为先水退后水进的层序格架。

Through the analysis and contrast between HM core and Dh core, combined with the data of AMS14C, six pollen assemblages were ploted Out. At the mean time, six stages about the vegetation change and climate fluctuation were rebuild. In addition, there were three sub-assemblages ploted out in the Atlantic period, Sub-Boreal period and Sub-Atlantic period, which reflected the less vibration of the large-scale climatic change. Pollen assemblage dominated by Concentricystes in the hard and green clay of late Pleistocene can make it sure that the hard green clay layer was formed by water.

通过对上海地区鹤鸣孔和东海1井两个钻孔进行孢粉分析鉴定和对比,结合AMS14C测年等资料,划分出了6个孢粉组合带,恢复了本区的植被演化和气候波动的6个阶段,对鹤鸣孔的大西洋期、亚北方期和亚大西洋期各划分出了两个孢粉组合亚带,反应了大气候环境下气候的次一级波动,在晚更新世晚期的硬绿色粘土中还发现了以环纹藻为主的孢粉组合,从孢粉学角度上证实了这一硬绿色粘土层&水成沉积&的观点。

Taphonomic reconstruction of ecology and preservation depends on the applicability of analogous processes in modern ecology and limnology.

鱼化石埋藏学方法在古湖泊环境研究中主要是利用鱼死亡及其骨骼解体和保存的方式,去推测湖泊的水文状况、沉积环境、群落结构、鱼类的生活史、死亡方式和保存特征等,这种方法的可行性取决于对现代湖泊中生物与环境对应关系的观察研究。

The data of femur biodymamics showed that acupuncture and moxibustion could increase the biggest load, modulus of elasticity, the biggest flexibility. The data of shank bone morphometry showed that acupuncture and moxibustion could increase percentage of bone trabecula bulk, lessen percentage of bone trabecula absorption and restoration, slow the rate of bone trabecula mineralization. Slices indicated that the structure of bone trabecula became basically complete.

股骨骨生物力学参数显示,针灸可提高OP症大鼠股骨最大载荷、弹性模量和最大挠度;胫骨骨组织形态计量学指标显示,针灸可增加骨小梁体积百分比,减少骨小梁吸收表面百分比和骨小梁形成表面百分比,降低骨小梁矿化沉积速率;胫骨骨组织切片显示,针灸后大鼠骨小梁结构已基本完整。

By analyzing the conditions and patterns of the regional oil and gas bearing formations with typical crosssections, we have established the patterns of sedimentary conditions for different reserviors.

为了解决上述问题,论文大力开展区域层序地层学研究,建立起全盆地层序和体系域的等时地层格架,揭示沉积体系的时空展布和演化特征,搞清大的地质背景。

Study on minerageny of the clay sediment in the west of Philippine Sea .

西菲律宾海西部海域粘土沉积物的成因矿物学研究。

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