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151.
介绍了地质科学应用程序从Basic向Visual Basic(简称VB,下同)移植的基本技巧,并结合实际开发经验对变量定义、数据读取、成果输出和存储等开发、移植过程做了说明. 相似文献
152.
Wang Xiuxi Li Jijun Song Chunhui Zhang Jun Zhao Zhijun Gao Junping Pan Meihui 《Frontiers of Earth Science》2007,1(3):304-308
The Cenozoic sedimentation in the Tianshui basin, which is located at the junction of the liupanshan and West Qinling, northeast
margin of the Tibetan plateau, provides a record for the regional tectonism and exhumation history of the surrounding mountains.
Thermochronologic study on the detrital apatite grains from sandstones at Yaodian, near Tianshui, has revealed two rapid tectonic
uplift-exhumation events of the source area, which happened at 23.7 and 14.1 Ma, respectively. The fast exhumation (0.34 mm/a)
at 23.7 Ma, which recorded the tectonic uplift of West Qinling, led to the formation of the Neogene Tianshui basin and initiated
the reception of alluvial deposits. This event is most likely in response to the synchronous tectonism of the Tibetan plateau.
The source region experienced another rapid exhumation (1.05 mm/a) at 14.1 Ma, when the Tianshui basin began to depress broadly
and fluvial-lacustrine sediments dominated the Late Miocene.
Translated from Acta Sedimentologica Sinica, 2006, 24(6): 783–789 [译自: 沉积学报] 相似文献
153.
Twenty broadband seismographs were deployed along Hongyuan, Sichuan to Wuwei, Gansu. 81 teleseismic events were recorded in one year. We computed receiver functions from teleseismic waveform data and obtained S wave velocity structure beneath each station along the profile by using receiver function inversion method. The results revealed that the crustal structure is very complex and crustal average S wave velocity is to be on the low side. Low velocity structure generally exists in the depth range of 10~40 km in the crust between Aba arc fault and northern edge fault of Qinling earth's axis and it is a tectonic feature of complex geological process such as ancient A'nyemaqen Tethys ocean from closing and side colliding to subducted plate exhumed or thrust rock slice lifted. The Moho is about 50 km depth along the profile and is slightly deeper in the south than in the north. 相似文献
154.
We investigate the estimation of interfacial areas, curvatures, and common curve lengths in multiphase porous medium systems. Algorithms are developed to obtain estimates of these quantities based upon a variety of potential data sources and estimation approaches. The accuracy of the derived approximations are evaluated as a function of the data type and resolution of the data. The methods advanced improve upon standard approaches now in use and show excellent accuracy at resolutions on the order of five lattice points per minimum radius of curvature of the object being resolved. Finally, we suggest a promising class of extensions that could lead to further improvements in the accuracy of such methods. 相似文献
155.
Precipitation is often the sole source of water replenishment in arid and semi‐arid areas and, thus, plays a pertinent role in sustaining desert ecosystems. Revegetation over 40 years using mainly Artemisia ordosica and Caragana korshinskii at Shapotou Desert Experimental Research Station near Lanzhou, China, has established a dwarf‐shrub and microbiotic soil crust cover on the stabilized sand dunes. The redistribution of infiltrated moisture through percolation, root extraction, and evapotranspiration pathways was investigated. Three sets of time‐domain reflectometry (TDR) probes were inserted horizontally at 5, 10, 15, 20, 30 and 40 cm depths below the ground surface in a soil pit. The three sets of TDR probes were installed in dwarf‐shrub sites of A. ordosica and C. korshinskii community with and without a microbiotic soil crust cover, and an additional set was placed in a bare sand dune area that had neither vegetation nor a microbiotic soil crust present. Volumetric soil moisture content was recorded at hourly intervals and used in the assessment of infiltration for the different surface covers. Infiltration varied greatly, from 7·5 cm to more than 45 cm, depending upon rainfall quantity and soil surface conditions. In the shrub community area without microbiotic soil crust cover, infiltration increased due to preferential flow associated with root tunnels. The microbiotic soil crust cover had a significant negative influence on the infiltration for small rainfall events (~10 mm), restricting the infiltration depth to less than 20 cm and increasing soil moisture content just beneath the soil profile of 10 cm, whereas it was not as strong or clear for larger rainfall events (~60 mm). For small rainfall events, the wetting front depth for the three kinds of surface cover was as follows: shrub community without microbiotic soil crust > bare area > shrub community with microbiotic soil crust. In contrast, for large rainfall events, infiltration was similar in shrub communities with and without microbiotic soil crust cover, but significantly higher than measured in the bare area. Soil water extraction by roots associated with evapotranspiration restricted the wetting front penetration after 1 to 3 h of rainfall. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
156.
157.
158.
某水电工程地应力场数值模拟研究 总被引:2,自引:2,他引:2
运用有限元法模拟位于深切河谷中的某水电工程区地应力场的形成过程,并与地应力的实测成果进行拟合分析。在此基础上,对研究区的一些特殊现象进行解释。 相似文献
159.
采用在经典离子晶体作用势中附加Morse势 ,并进行必要的量子化修正 ,对石英 α型SiO2 结构随压力变化特性进行分子动力学计算模拟 ,获得了压力高于 2 4 .6GPa ,从晶相向非晶相相变模拟结果 ,并利用其离子间相互作用势、摩尔体积变化、键角等重要信息对模拟结果作了深入的探讨 ,获得了与实验结果较一致的模拟结果。 相似文献
160.
扫描数字化地图数据的误差构成及精度分析 总被引:1,自引:0,他引:1
从扫描数字化的基本原理及实施过程出发,分析了基于大比例尺地形图的扫描数字化的误差来源,着重讨论了影响扫描数字化数据结果精度的主要原因及采取的措施。 相似文献