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41.
Abstract Whether there existed the Songpan-Garzê massif is a controversial problem. This paper expounds and proves that the old basement of the massif is represented by the pre-Sinian granitic rock series. This massif and the South Qinling fold belt might both be a part of the old Yangtze platform. Rifting generated by the Caledonian orogeny in the terminal Early Palaeozoic caused the massif to be disintegrated from the northwestern part of the Yangtze platform. This disintegration, however, was not thorough, and the rift troughs were later gradually closed and filled up. The Emei taphrogeny that was initiated in the Early Permian Maokou'an Stage involved a second disintegration of this massif from the Yangtze platform. The rift line largely goes along the Muli-Pingwu line. This rifting belongs to synchronous extensional rifting at peripheries of the Yangtze platform and in its interior, showing that the posterior, lateral and interior extension resulting from rapid northward shift of the Yangtze platform led to isolation of this massif together with South Qinling from their adjacent areas. During the Ladinian Stage, the Songpan-Garzê massif and southern Qinling sank strongly en masse. This subsidence continued till the end of the Late Triassic when the late Indosinian movement caused the sea trough to be closed and Songpan-Garzê and southern Qinling to be folded and uplifted and become mountains. 相似文献
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43.
GenerationofMuscovite/Two-MicaGranilandIntracontinentalSubduction¥DengJinfu;ZhaoHailing;LaiShaocong;LiuHouxiang;LuoZhaohua(De... 相似文献
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47.
西部地区资源实现可持续利用的道路初探 总被引:1,自引:0,他引:1
介绍了我国西部资源的国情,指出资源利用中存在的问题,其原因在于不正确的人与自然观导致了人们对资源的不合理利用;粗放型的经济增长方式;资源的管理体制不完善等等,提出了实现西部地区资源可持续利用的七大对策;转变经济增长方式;依靠科技进步;树立正确的资源观;制定一个系统有效的统一管理体制;全方位的资源综合利用,进行资源核算,实行资产化管理。 相似文献
48.
3-D S-waveQ structure in Jiashi earthquake region is inverted based on the attenuation of seismic waves recorded from earthquakes in
this region in 1998 by the Research Center of Exploration Geophysics (RCEG), CSB, and a rough configuration of deep crustal
faults in the earthquake region is presented. First, amplitude spectra of S-waves are extracted from 450 carefully-chosen
earthquake records, called observed amplitude spectra. Then, after instrumental and site effect correction, theoretical amplitude
spectra are made to fit observed amplitude spectra with nonlinear damped least-squares method to get the observed travel time
overQ, provided that earthquake sources conform to Brune’s disk dislocation model. Finally, by 3-D ray tracing method, theoretical
travel time overQ is made to fit observed travel time overQ with nonlinear damped least-squares method. In the course of fitting, the velocity model, which is obtained by 3-D travel
time tomography, remains unchanged, while onlyQ model is modified. When fitting came to the given accuracy, the ultimateQ model is obtained. The result shows that an NE-trending lowQ zone exists at the depths of 10–18 km, and an NW-trending lowQ zone exists at the depths of 12–18 km. These roughly coincide with the NE-trending and the NW-trending low velocity zones
revealed by other scientists. The difference is that the lowQ zones have a wider range than the low velocity zones.
Foundation item: Joint Seismological Science Foundation of China (957-07-414) and State Key Basic Research Development and Programming Project
(95-13-02-02).
Contribution No. RCEG200105, Research Center of Exploration Geophysics, China Seismological Bureau. 相似文献
49.
建立了哈尔滨市地下水资源优化管理模型 ,将求解多目标最优化问题的约束法和线性加权法相结合 ,给出了一种综合解法 ,并将此法应用于所建立的水资源优化管理模型的求解。其结果可为该地区地下水资源的管理提供有参考价值的科学依据。 相似文献
50.
Shen Weizhou Zhang Bangtong Ling Hongfei Lai Mingyuan Yang Jiedong Tao Xiancong 《《地质学报》英文版》1992,66(2):165-176
Nd, Sr and O isotopic study on the spilite-keratophyre sequence in Xiqiu shows that its ∈_(Nd) values are inthe range of 4.02-5.26, and its ∈_(Sr) values, +1.4-2.6. According to the points of these data in the ∈_(Nd)-T,∈_(Sr)-T and ∈_(Nd)-∈_(Sr) diagrams, the spilite-keratophyre is interpreted as being slightly contaminated by crustalmaterials. Its δ~(18)O values are 3.9-5.0‰. The depletion of ~(18)O in the rocks resulted from the influence ofseawater hydrothermal alteration during or soon after the rock formation. Based on the isotopic characteristicsand available geochemical data, it is believed that the spilite-keratophyre was formed in the well-developedisland-arc environment during the Late Proterozoic subduction of the palaeo-Pacific plate beneath thesoutheastern margin of the Yangtze massif. 相似文献