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871.
872.
南澜沧江结合带火山岩岩浆成因——洋脊洋岛与弧岩浆作用的性质 总被引:9,自引:1,他引:9
在对滇西南昌宁—孟连带石炭—二叠纪火山岩和南澜沧江带二叠—三叠纪火山岩的微量元素和稀土元素研究的基础上,划分了岩浆作用类型和岩浆演化系列,探讨了岩浆源区成分特点。昌宁—孟连带玄武质岩浆的演化主要受部分熔融和分离结晶作用控制;这些岩浆可以划分为3个岩浆演化系列:(1)稀土曲线平坦型的洋脊型拉斑玄武岩浆演化系列,其岩浆起源于亏损型地幔;(2)稀土曲线中等富集型的准洋脊型拉斑玄武岩浆演化系列,其岩浆起源于过渡型地幔;(3)稀土曲线强烈富集型的洋岛型碱性玄武岩浆演化系列,其岩浆起源于富集型地幔。南澜沧江带弧火山岩的岩浆成因主要受分离结晶作用控制,也可以划分为3个岩浆演化系列:(1)二叠纪低钾拉斑—中钾钙碱性岩浆演化系列;(2)中南段的晚三叠世低钾拉斑—中钾钙碱性岩浆演化系列;(3)北段的晚三叠世钾玄岩—高钾钙碱性岩浆演化系列 相似文献
873.
874.
利用遥感技术进行干旱半干旱区找水的方法和实践 总被引:1,自引:0,他引:1
随着遥感技术和地面物探技术的发展和深入应用,产生了一种现代的综合勘探方法。本文介绍了在内蒙古锡林浩特市胜利煤田露天矿区供水水文地质普查中运用综合水文地质勘察方法的情况、遥感方案的选择、技术思路,以及利用遥感方法进行区域水文地质调绘所取得的成果,对遥感水文地质的发展提出了作者的看法。 相似文献
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876.
多种类型金矿化群聚于铜石碱性钾质次火山岩体中及其周围,构筑了成矿模式的框架。归来庄金矿床属于富含贵金属的石英-萤石-冰长石型浅成中-低温热液金矿床。 相似文献
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878.
This paper mainly reports the permanent impact of displacement damage induced by heavy-ion strikes on the deep-submicron MOSFETs. Upon the heavy ion track through the device, it can lead to displacement damage, including the vacancies and the interstitials. As the featured size of device scales down, the damage can change the dopant distribution in the channel and source/drain regions through the generation of radiation-induced defects and thus have significant impacts on their electrical characteristics. The measured results show that the radiation-induced damage can cause DC characteristics degradations including the threshold voltage, subthreshold swing, saturation drain current, transconductance, etc. The radiation-induced displacement damage may become the dominant issue while it was the secondary concern for the traditional devices after the heavy ion irradiation. The samples are also irradiated by Co-60 gamma ray for comparison with the heavy ion irradiation results. Corresponding explanations and analysis are discussed. 相似文献
879.
Tan K. Wang Ben Jhong Yang Jia-Ming Deng Chao-Shing Lee Char-Shine Liu 《Marine Geophysical Researches》2010,31(1-2):59-76
Horizon velocity analysis and pre-stack depth migration of seismic profiles collected by R/V Maurice Ewing in 1995 across the accretionary prism off SW Taiwan and along the continental slope of the northernmost South China Sea were implemented for identifying gas hydrates. Similarly, a survey of 32 ocean-bottom seismometers (OBS), with a spacing of about 500 m, was conducted for exploring gas hydrates on the accretionary prism off SW Taiwan in April 2006. Travel times of head wave, refraction, reflection and converted shear wave identified from the hydrophone, vertical and horizontal components of these OBS data were applied for imaging P-wave velocity and Poisson’s ratio of hydrate-bearing sediments. In the accretionary prism off SW Taiwan, we found hydrate-bearing sediment, with a thickness of about 100–200 m, a relatively high P-wave velocity of 1.87–2.04 km/s and a relatively low Poisson’s ratio of 0.445–0.455, below anticlinal ridges near imbricate emergent thrusts in the drainage system of the Penghu and Kaoping Canyons. Free-gas layer, with a thickness of about 30–120 m, a relatively low P-wave velocity of 1.4–1.8 km/s and a relatively high Poisson’s ratio (0.47–0.48), was also observed below most of the bottom-simulating reflectors (BSR). Subsequently, based on rock physics of the three-phase effective medium, we evaluated the hydrate saturation of about 12–30% and the free-gas saturation of about 1–4%. The highest saturation (30% and 4%) of gas hydrates is found below anticlines due to N–S trending thrust-bounded folds and NE-SW thrusting and strike-slip ramps in the lower slope of the accretionary prism. We suggest that fluid may have migrated through the relay-fault array due to decollement folding and gas hydrates have been trapped in anticlines formed by the basement rises along the thrust faults. In contrast, in the rifted continental margin of the northernmost South China Sea, P-wave velocities of 1.9–2.2 km/s and 1.3–1.6 km/s, and thicknesses of about 50–200 m and 100–200 m, respectively, for a hydrate layer and a free-gas layer were imaged below the remnant and erosional ridges in the upper continental slope. High P-wave velocity of hydrate-bearing sediment below erosional ridges may also indicate high saturation of hydrates there. Normal faults due to rifting in the South China continental crust may have provided conduits for gas migration below the erosional ridges where P-wave velocity of hydrate-bearing sediment in the passive continental margin of the northernmost South China Sea is greater than that in the active accretionary prism off SW Taiwan. 相似文献
880.