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991.
992.
苏南地区地热资源研究 总被引:2,自引:0,他引:2
在充分收集区域地质,水文于质,物化探及地热资料的基础上,分析了苏南地区地下热水的形成和赋存的背景,条件,规律及特征,并进行地下热水的划分与预测,为进一步的研究,勘察,开发提供的依据。 相似文献
993.
西扬子大陆区泥盆系因有丰富的矿产资源一直为地学界所关注.在泥盆纪盆地演化中,地质事件与成矿关系极为密切.盆地沉积类型有台地型和海槽型两种.台地型泥盆系在沉积建造、生物群落、地质事件及沉积矿产等多方面均能与中、下扬子区相对比,故归属南方区扬子型泥盆系;海槽型泥盆系与台地型泥盆系在时空上均紧密衔接,但成矿作用有明显差别.海槽型泥盆系多产出层控型金和多金属矿床,台地型则以沉积矿床为主. 相似文献
994.
云南白垩系分布在滇中、滇西和澜沧江以西三个地域,彼此之间被深断裂所,它们的地质历程、构造特征各不相同。不能将澜沧江以西勐海、潞西地区的白垩系解体归属不同地层区。澜沧江以西的白垩系,分布于冈瓦纳古陆和古特提斯造带的小型山间盆地,地层层序齐全,岩性、厚度稳定,今古生物化石。有两套岩石序列,三个沉积旋回。 相似文献
995.
在叠前深度偏移和非零炮检距声波方程正演计算过程中包含了大量的可并行计算的成分。作者在本文中提出叠前正演模拟与偏移的网络并行计算算法,并基于TCP/IP协议,将该算法设计成网络并行处理程序,极大地提高了计算效率。实际运算结果证明,本文提出的并行算法和技术路线是切实可行的。 相似文献
996.
Variations in chemical compositions of the eolian dust in Chinese Loess Plateau over the past 2.5 Ma and chemical weathering in the Asian inland 总被引:5,自引:0,他引:5
Major and trace elements as well as strontium isotopic composition have been analyzed on the acid-insoluble (AI) phase of
the loess-paleosol sequence from Luochuan, Shaanxi Province, China. Results show that the chemical composition of AI phase
of loess and paleosols is distinctive to the average composition of upper continental crust (UCC), characterized by depletion
of mobile elements Na, Ca and Sr. The distribution pattern of elements in AI phase reveals that initial dust, derived from
a vast area of Asian inland, has suffered from Na- and Ca-removed chemical weathering compared to UCC. Some geochemical parameters
(such as CIA values, Na/K, Rb/Sr and87Sr/86Sr ratios) display a regular variation and evolution, reflecting that the chemical weathering in the source region of loess
deposits has decreased gradually since 2.5 Ma with the general increase of global ice volume. This coincidence reflects that
the aridity of Asian inland since the Quaternary is a possible regional response to the global climate change. 相似文献
997.
Anisotropy of the apparent resistivity variation rate near the epicentral region for strong earthquakes 总被引:1,自引:0,他引:1
IntroductionThe geo-electrical anisotropy before earthquake is of special significance for the prediction of earthquake location and for the research on crustal stress status near the epicentral region. The anisotropy has been studied from various aspects (CHEN, et al, 1983; QIAN, et al, 1985, 1996; LU, et al, 1990a; MAO, et al, 1995; RUAN, et al, 1999). But the anisotropic phenomena presented by geo-electrical data are not practically satisfactory and not clear as compared with the res… 相似文献
998.
Post-earthquake investigation on several geosynthetic-reinforced soil retaining walls and slopes during the Ji-Ji earthquake of Taiwan 总被引:1,自引:0,他引:1
Hoe I. Ling Dov Leshchinsky Nelson N. S. Chou 《Soil Dynamics and Earthquake Engineering》2001,21(4):3087
This paper gives an overview on the application of geosynthetic-reinforced soil structures in Taiwan. Taiwan has an unique topography and geotechnical conditions that rendered a less conservative and more challenging design compared to that of North America, Europe and Japan. The Ji-Ji (Chi-Chi) earthquake of 1999 gave an opportunity to examine the behavior of reinforced soil structures. The performance of several modular-block reinforced soil retaining walls and reinforced slopes at the vicinity of the fault was evaluated. Reinforced structures performed better than unreinforced soil retaining walls. The failure cases were highlighted and the cause of failure was identified. The lack of seismic design consideration could be a major cause of failure. The compound failure mode, the inertia force of the blocks, and the connection stiffness and strength relative to the large dynamic earth pressure, were among major items that would warrant further design consideration. 相似文献
999.
Fabrizio Eva 《GeoJournal》2001,52(4):295-301
Discussion of the future of Europe continues to be a marginal political issue, partly because of the resistance of states, on both the practical (bureaucratic) and conceptual levels, created by the government leaders and heads of state. In turn, the nation-states are challenged from within by independent and separatist movements that have laid bare the fundamental hypocrisy of rhetorical discussions of the principle regarding the self-determination of peoples; interfering with states (and their borders) has proven to be a taboo for Europe. The growing flexibility of the globalised economy should be paralleled by a growing flexibility in the conception of the division and political organisation of territory, but this is not the case. Further inflexibility stems from the socio-economic inequity that we accept in our daily lives as normal, in particular as regards inequality in the use and division of territory. Equality, or better egaliberté (equality and liberty), is a sufficiently dynamic and flexible concept to be taken as a point of reference in envisaging the society, Europe, and world of tomorrow. It is only through the concept of egaliberté that we can imagine a Europe based on relations between regions that are conceived and organised on multiple scales and not as region-nations conceived on the basis of ethnicity or in the name of supposed cultural homogeneity. 相似文献
1000.
A. D. Shukla N. Bhandari Sheela Kusumgar P. N. Shukla Z. G. Ghevariya K. Gopalan V. Balaram 《Journal of Earth System Science》2001,110(2):111-132
Chemical analysis of nine Deccan flow basalts at Anjar, Kutch, western India, indicates that all, except the uppermost flow
F-9, are alkaline. In their major and trace element composition, the alkali basalts resemble Ocean island basalts (OIB). Similarities
of many diagnostic trace element ratios (e.g. Sm/Nd, Ba/Nb,Y/Nb and Zr/Nb) are similar to those found in the Réunion Island
basalts. The uppermost basalt is tholeiitic and chemically resembles the least contaminated Deccan basalt (Ambenali type).
The Anjar basalts have iridium concentration ranging between 2 and 178 pg/g. Some of these values are higher by about an order
of magnitude compared to the Ir concentration in other basalts of the Deccan. A synthesis of chemical, palaeomagnetic and
geochronologic data enables us to construct a chemical and magnetic stratigraphy for these flows.
The three flows below the iridium enriched intertrappean bed (IT III) show normal magnetic polarity whereas all except one
of the upper basalts show reversed magnetic polarity. The sequence seems to have started in polarity zones 31N and probably
continued up to 28R or 27R. The results presented here support the view that Deccan volcanism in Kutch occurred on a time
span of a few million years. 相似文献