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91.
92.
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
93.
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
94.
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
95.
96.
中国土地利用时空特征分析 总被引:195,自引:5,他引:195
在遥感技术与GIS技术的支持下,对中国近5年来土地利用的时间动态特征和空间动态特征进行了定量分析。具体表现为通过数学建模,利用土地利用动态度模型、土地利用程度模型、垦殖指数模型等对土地利用时空特征进行了分析。研究结果表明:5年间中国土地利用类型发生变化比较大的区域主要分布在东部和北部地区,特别是东北部地区土地利用类型变化比较剧烈,而西部变化相对缓慢;土地利用各类型中面积增加的有耕地、水域、建设用地和未利用地,而林地、草地面积减少;耕地增加的区域位于东北部地区,特别是黑龙江省耕地面积增加最多;林草地以及未利用地的面积变化主要发生在新疆、内蒙和黑龙江等地区,其它地区变化幅度相对较小。 相似文献
97.
通过地面调查及钻井地质资料分析,对柴达木盆地干柴沟地区第三系湖盆边缘斜坡带沉积体系构成进行分析研究,该体系主要由扇三角洲沉积体系,水下洪积扇-近岸浊流沉积体系,辫状河三角洲沉积体系,常态湖三角洲沉积体系和湖泊沉积体系组成。对其成因地层格架及湖盆充填模式进行了探讨分析。 相似文献
98.
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
99.
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
100.
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