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81.
82.
Xia Wenchen Zhou Jie Lei Jianxi Zhang Nianmao Peng YangChina U niversity of Geoscience W uhan Hubei Wang Yujun 《《地质学报》英文版》1995,69(4):341-357
On the basis of exhaustive researches on the facies sequences and depositlonal evolutionary process of various depositional systems, the genetic stratigraphic framework of the extensional rifted oceanic basin, which has undergone strong structural destruction, has been reconstructed by means of dynamic genetic stratigraphic analysis. Five depositional episodes have been distinguished from various isochronous stratigraphic boundaries and stratigraphic sequences with the three-dimensional structure of each depositional episode analysed in detail. The tectonic paleogeographic environment corresponding to different stages of each depositional episode has been reconstructed for individual depositional system tracts. And the evolution history of this rifted basin has been divided into four stages' initial rifting and oceanization of continental crust, stretching and spreading of the basin, subduction and basin differentiation, and convergence and collision. A NNE-trending intracontinental soft collision sutur 相似文献
83.
中国大陆原地复发强震的基本特征及其预测 总被引:7,自引:3,他引:7
在印度板块与欧亚块相碰撞形成的喜马拉雅弧板块边界力作用下,中国大陆有自己独特的现代构造运动和地震活动基本格架。格架是两组近似于对数螺线的现代构造滑移线,即最大剪切应力和剪切应变集中释放的区,带。在这种格架控制下,强震和大震在原地或基本在原地重复发生是中国大陆地震活动的重要特征。本文还提出了i-f-j复发轮回模式和估计当前轮回强震复发时间的概率分布以及计算未来强震复发概率分式。为中,长期预测原地复发 相似文献
84.
M. Franceschelli M. Puxeddu G. Cruciani D. Utzeri 《International Journal of Earth Sciences》2007,96(5):795-815
Metabasites with eclogite facies relics occur in northern Sardinia as massive to strongly foliated lenses or boudins embedded
within low- to medium-grade rocks (Anglona) and migmatites (NE Sardinia). U–Pb zircon dating yielded 453 ± 14, 457 ± 2 and
460 ± 5 Ma as the protolith ages; 400 ± 10 and 403 ± 4 Ma have been interpreted as the ages of the HP event and 352 ± 3 and
327 ± 7 Ma as the ages of the main Variscan retrograde events. A pre-eclogite stage is documented by the occurrence of tschermakite,
zoisite relics within garnet porphyroblasts (Punta de li Tulchi) and an edenite–andesine inclusion within a relict kyanite
porphyroblast (Golfo Aranci). Four main metamorphic stages have been distinguished in the eclogite evolution: (1) eclogite
stage, revealed by the occurrence of armoured omphacite relics within garnet porphyroblasts. The Golfo Aranci eclogites also
include kyanite, Mg-rich garnet and pargasite; (2) granulite stage, producing orthopyroxene and clinopyroxene–plagioclase
symplectites replacing omphacite. At Golfo Aranci, the symplectitic rims around relict kyanite consist of sapphirine, anorthite,
corundum and spinel; (3) amphibolite stage, leading to the formation of amphibole–plagioclase kelyphites between garnet porphyroblasts
and pyroxene–plagioclase symplectites and to the growth of cummingtonite on orthopyroxene. Tschermakite to Mg-hornblende,
plagioclase, cummingtonite, ilmenite, titanite and biotite are coexisting phases; (4) greenschist to sub-greenschist stage,
defined by the appearance of actinolite, chlorite, epidote ss, titanite, sericite and prehnite. The following P–T ranges have been estimated for the different stages. Eclogite stage 550–700°C; 1.3–1.7 GPa; granulite stage 650–900°C; 0.8–1.2 GPa,
clustering in the range 1.0–1.2 GPa; amphibolite stage 550–740°C; 0.3–0.7 GPa; greenschist stage 300–400°C; 0.2–0.3 GPa. Comparable
ranges characterise the other Variscan massifs in Europe; eclogite stage: T = 530–800°C; P from 0.7–1.1 to 1.7 ± 0.3 GPa; granulite stage T = 760–870°C and P from 1.1–1.4 to 7.2–9.9 GPa, clustering around 1.0–1.2 GPa. Whole-rock chemistry: Sardinian eclogites are N- to T-MORB;
European ones N- to E-MORB or calc-alkaline. 相似文献
85.
在详细研究组成内陆叠合型盆地的各个单型盆地的沉积体系三维构成的基础上 ,采用动态成因地层和层序地层分析方法 ,恢复了叠合型内陆盆地的成因地层格架 ,并根据各类等时地层界面的构型 ,将盆地地层序列划分为 7个沉积幕、3个构造沉积幕。进而分析了内陆盆地在同生裂陷和衰减坳陷等不同阶段的充填过程。 相似文献
86.
Analytical expressions are derived for the Poisson's ratios associated with a three-dimensional network of regular, corner-sharing
tetrahedra in which: (1) the tetrahedra are assumed to be rigid and free to rotate relative to each other; (2) the tetrahedra
are assumed to maintain shape and orientation but are free to change size (dilate); (3) tetrahedral rotation and dilation
are assumed to act concurrently. The structure has a primitive unit cell containing four tetrahedra and is analogous to the
molecular structure of α-cristobalite. Strain-dependent variations in Poisson's ratio are also predicted by the models. For
deformation due to tetrahedral rotation the network is found to exhibit negative Poisson's ratios in each of the three principal
directions, with the magnitude of the Poisson's ratio being dependent on the angle of rotation of the tetrahedra. The behaviour
of the Poisson's ratio is isotropic in the transverse plane, but anisotropic elsewhere. In the dilation model negative Poisson's
ratios equal to −1 are observed for uniaxial loading in any of the principal directions, with the value being constant irrespective
of tetrahedral size. The model for concurrent tetrahedral rotation and dilation allows positive as well as negative Poisson's
ratios, with the values determined by the framework geometry and relative strengths of the two mechanisms. The concurrent
model also offers a design route to materials and structures having ultrahigh Young's moduli.
Received: 15 February 2000 / Accepted: 1 October 2000 相似文献
87.
湖南洞庭坳陷大地电磁测深研究 总被引:1,自引:0,他引:1
介绍了大地电磁测深在湖南洞庭坳陷的主要研究成果。详细分析、推断了洞庭地区的区域构造格局,深部电性结构及壳、幔高导层的分布特点 相似文献
88.
海洋沉积物动力学的示踪物方法 总被引:4,自引:1,他引:3
本文的论题是示踪物方法在海洋物源追踪和沉积物输运率计算中的应用 ,以及示踪物方法的普适性理论框架。定量的物源追踪需要适当的示踪标记和物质混合模型 ,有必要根据沉积动力过程的研究来确定示踪标记的变换函数 ,从而将改进的示踪标记用于混合模型分析。人工示踪物实验的现有方法以空间积分法最为常用 ,其关键是示踪物质心运动和沉积物活动层的界定。天然示踪物的质心位置是无法定义的 ,因此不能借用传统人工示踪物方法来估算物质输运率 ;在某些特殊情形下 ,可以利用天然示踪物的质量守衡原理来获得物质输运信息。今后 ,以示踪物质的连续方程为基础 ,有可能建立一种同时适用于人工和天然示踪物的普适理论框架。其中需解决的问题包括示踪物与现场物质的差异、沉积速率和活动层厚度的时间尺度、沉积物扩散过程等。 相似文献
89.
论述了如何在Java应用开发领域中使用设计模式和MVC(Model-View-Controller)架构。介绍了设计模式的概念和特点,以及MVC架构的设计思想,并分析了MVC架构中包含的几种主要模式,采用MVC架构作为开发的基本架构,可以使开发的项目耦合度降低,提高程序的可扩展性。根据Java应用系统的特点,在实际的“数值预报业务监控系统”的应用开发中如何采用MVC架构提出了一些自己的想法。 相似文献
90.
塔里木盆地沉积剥蚀过程与油气关系 总被引:3,自引:0,他引:3
塔里木盆地典型井的周期分析表明,塔里木盆地在其地质历史时期100Ma左右的周期是很明显的,自寒武纪以来共经历了4个完整的周期,每一完整周期都由正相位和负相位两个半周期所组成。而第三纪为第5个周期的正相位阶段。该周期控制了盆地内的沉积与剥蚀的过程及成藏旋回。对沉积与剥蚀过程的控制作用表现在周期波正相位和负相位分别对应于沉积期和剥蚀期,这在地质年代序列中表现为沉积与间断的互为消长的演化进程。对食油气系统的控制作用表现在:第1个周期波构成以早古生代地层为主体的含油气系统,第2个周期波至第4个周期波构成以晚古生代至中生代地层为主体的含油气系统,第5个周期的正相位阶段构成以第三纪地层为主体的含油气系统。 相似文献