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621.
In this paper, based on the previous study of practical use of seismic regime windows and seismic regime belts, the problem
of establishing a “seismic regime network” consisting of “windows” and “belts” is further posed and discussed according to
the observed fact that many “windows” and “belts” make responses to one earthquake. For the convenience of usage, the “seismic
regime network” is divided into two classes, the first class and the second one. The former can be used in tendency prediction
for long-term seismic activity in a large area, the latter used in short-term prediction in a small area. In this paper, after
briefly discussing the physical significance of “seismic regime network”, it is pointed out that this simple and easily used
method can be used to observe and extract seismic precursory information from a large area before a great earthquake, thus
it can provide a reliable basis for the analysis and judgement of seismic regime tendency in time and space. No doult, this
method is of certain practical significance.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 161–169, 1991.
The English version of this paper is improved by Prof. Shaoxie Xu. 相似文献
622.
重、磁常规数据处理在地质上得到广泛应用,我们建立了一个标准的常规数据处理工具库:HKl.LIB,同时,在库中加入图形函数,使得能够使用FOR-TRAN语言编制绘图软件。 相似文献
623.
624.
625.
大都市区的形成机制及其定界:以北京为例 总被引:49,自引:1,他引:49
源于欧美的大都市区,在中国具有特殊的形成机制和联系形式。对北京的研究表明,其形成主要由中心城市工业化的扩散和农村非农业化两种过程所决定,并据此提出了中国大都市区定界的初步方法。进一步研究还发现中国已经出现了都市连绵带。 相似文献
626.
627.
三维绿色生物量的遥感模式研究与绿化环境效益估算 总被引:4,自引:0,他引:4
本文从理论和技术上叙述了绿量的遥感模式研究和绿化环境效益估算,并取得了以下几个方面的进展:(1)提出了绿量的概念,进一步完善了城市绿化的量化指标体系;(2)成功地修正了“逻辑斯蒂曲线”方程,并以平面量模拟立体量的方法测算了上海市全市的绿量,不仅节省了人力物力,而且提高了精度;(3)提出了模式林的概念及测定了以绿量估算绿化环境效益中所必须的标准换算量;(4)首次用绿量在全市范围估算了绿化群落的吸碳产氧、吸收二氧化硫、滞尘及夏季降温等环境效益。为分析现有绿化群落布局与结构的合理性,及为绿化规划乃至整个城市的总体规划提供了很有价值的技术参数。 相似文献
628.
珠海市1:2万城区因是适应近年来该市市区建设迅速发展编制的一幅崭新地图,其遵循的基本原则包括突出城市个性、保证资料现势性、强调地围实用性和注重地图艺术性四个方面.该图在地图内容的表现和图面设计等方面体现了以下特点:表现现代城市街区的功能类型,采用晕渲和明暗等高线显示立体地貌,综合表示花园式城市的绿地景观,图面配置和地图设色的合理化以及文字注记的实用化等. 相似文献
629.
非等间距序列的灰色预测模型及其在岩石蠕变断裂中的应用 总被引:3,自引:1,他引:3
给出了非等间距序列的灰色预测模型,讨论了该模型的灰色预测平面和最优预测函数。最一将该模型应用于符合Kelvin模型的岩石材料的蠕变断裂研究,给出了应用实例,并验证了该方法的可行性。 相似文献
630.
The composition of the Earth 总被引:317,自引:0,他引:317
Compositional models of the Earth are critically dependent on three main sources of information: the seismic profile of the Earth and its interpretation, comparisons between primitive meteorites and the solar nebula composition, and chemical and petrological models of peridotite-basalt melting relationships. Whereas a family of compositional models for the Earth are permissible based on these methods, the model that is most consistent with the seismological and geodynamic structure of the Earth comprises an upper and lower mantle of similar composition, an Fe---Ni core having between 5% and 15% of a low-atomic-weight element, and a mantle which, when compared to CI carbonaceous chondrites, is depleted in Mg and Si relative to the refractory lithophile elements.The absolute and relative abundances of the refractory elements in carbonaceous, ordinary, and enstatite chondritic meteorites are compared. The bulk composition of an average CI carbonaceous chondrite is defined from previous compilations and from the refractory element compositions of different groups of chondrites. The absolute uncertainties in their refractory element compositions are evaluated by comparing ratios of these elements. These data are then used to evaluate existing models of the composition of the Silicate Earth.The systematic behavior of major and trace elements during differentiation of the mantle is used to constrain the Silicate Earth composition. Seemingly fertile peridotites have experienced a previous melting event that must be accounted for when developing these models. The approach taken here avoids unnecessary assumptions inherent in several existing models, and results in an internally consistent Silicate Earth composition having chondritic proportions of the refractory lithophile elements at 2.75 times that in CI carbonaceous chondrites. Element ratios in peridotites, komatiites, basalts and various crustal rocks are used to assess the abundances of both non-lithophile and non-refractory elements in the Silicate Earth. These data provide insights into the accretion processes of the Earth, the chemical evolution of the Earth's mantle, the effect of core formation, and indicate negligible exchange between the core and mantle throughout the geologic record (the last 3.5 Ga).The composition of the Earth's core is poorly constrained beyond its major constituents (i.e. an Fe---Ni alloy). Density contrasts between the inner and outer core boundary are used to suggest the presence ( 10 ± 5%) of a light element or a combination of elements (e.g., O, S, Si) in the outer core. The core is the dominant repository of siderophile elements in the Earth. The limits of our understanding of the core's composition (including the light-element component) depend on models of core formation and the class of chondritic meteorites we have chosen when constructing models of the bulk Earth's composition.The Earth has a bulk Fe/Al of 20 ± 2, established by assuming that the Earth's budget of Al is stored entirely within the Silicate Earth and Fe is partitioned between the Silicate Earth ( 14%) and the core ( 86%). Chondritic meteorites display a range of Fe/Al ratios, with many having a value close to 20. A comparison of the bulk composition of the Earth and chondritic meteorites reveals both similarities and differences, with the Earth being more strongly depleted in the more volatile elements. There is no group of meteorites that has a bulk composition matching that of the Earth's. 相似文献