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991.
全数字航测相机ADS40及其应用初探 总被引:1,自引:0,他引:1
本文简单介绍了目前国际上比较流行的线阵航空数字传感器ADS40的一些基本情况,分析了该传感器的技术优势与应用意义,并对配套应用技术的开发问题进行了初步的讨论。 相似文献
992.
新建拉林铁路桑珠岭隧道高地应力、高地温隧道开挖过程中岩爆灾害突出。考虑开挖卸荷与温降共同耦合作用,对隧道开挖过程中不同温度时洞周应力释放过程进行数值模拟,同时对隧道开挖后的二次应力进行现场实测,就高地温对隧道洞周应力的影响进行了比较分析,最后就不同岩爆判据下高地温对岩爆发生的影响性进行了讨论。研究结果表明,采用应力释放率和温降指标反映开挖卸荷与温降共同耦合作用能合理描述高地应力高地温段开挖过程中的应力特征和岩爆发生规律。当温降超过55 ℃,应力释放率大于40%以后, 及 量值随应力释放率增大而线性增长,当应力释放率达到100%时达到最大,不同位置洞周应力拱脚处增长最快,拱顶次之,其他位置较低。在开挖中受高地温影响岩爆发生时间提前,岩爆发生等级亦不断增加。 相似文献
993.
The diagenetic environment, diagenetic responses, diagenetic transformation model and formation mechanisms of high-quality reservoirs (beach-bar sandstones of the Paleogene fourth member) in the Dongying depression were studied through the analysis of fluid inclusions, thin section and burial evolution history. The diagenetic fluids of the beach-bar sandstone reservoirs evolved from early high salinity and weak alkalinity to low salinity and strong acidity, late high salinity and strong alkalinity and late low salinity and acidity, which were accompanied by two stages of oil and gas filling. The fluids at the margins of the sandbodies were continuously highly saline and strongly alkaline. The western (eastern) reservoirs experienced early open (closed), middle open, and late closed diagenetic environments during their burial history. The flow pattern was characterized by upwelling during the majority of the diagenesis (in the east, a non-circulating pattern transitioned into an upwelling current). Due to the evolution of the diagenetic fluids, the diagenetic sequence of the beach-bar reservoirs was as follows: early weak carbonate cementation; feldspar and carbonate cement dissolution and authigenic quartz cementation; late carbonate and anhydrite cementation, authigenic feldspar cementation, and late quartz dissolution; and late carbonate cementation, feldspar dissolution, and authigenic quartz cementation. The diagenetic strength during these stages varied or was absent altogether in different parts of the reservoirs. Due to the closeness of the diagenetic environment and the flow pattern of the diagenetic fluids, the diagenetic products are variably distributed in the sandstones interbedded with mudstones and in the fault blocks. The evolution of multiple alternating alkaline and acidic diagenetic environments controlled the distribution patterns of the reservoir diagenesis and reservoir space, and the reservoir quality index, RQI, increased gradually from the margins to the centers of the sandstones. The closeness of the diagenetic environment and the flow patterns of the diagenetic fluids controlled the differences in the reservoir properties among the fault blocks. With increasing distance from the oil-source faults, the RQI values in the west gradually decreased and in the east initially increased and then decreased. 相似文献
994.
Tropical cyclones represent major natural disasters in low- and mid-latitude coastal areas. Effective assessment of tropical cyclone disasters provides a scientific reference for the formulation of tropical cyclone prevention and disaster-relief measures. Tropical cyclone disasters in Zhejiang Province are mainly studied based on GIS technology, by considering disaster-causing factors, disaster-affected bodies, the disaster-formative environment, and spatial distribution of disaster prevention and relief capacity. In light of an uncertain nonlinear relationship between assessment factors and disaster factors, we used support vector machines to establish a fine, quantitative assessment model. This model evaluates the following disaster indices: Disaster-affected population, direct economic loss, affected crop area, and number of damaged houses resulting from a tropical cyclone disaster in Zhejiang, with the county as basic assessment unit. Assessment of tropical cyclone No. 0908 shows that the developed assessment model is able to accurately evaluate the geographical distribution of losses caused by a tropical cyclone. 相似文献
995.
996.
997.
通过模型磁异常分解,结合功率谱分析及异常振幅计算场源深度并判断场源分布平面位置,表明小波多尺度分析在位场分离中的有效性.将该方法应用于北衙铁金矿区磁异常分析解释,通过功率谱分析估算了各阶细节及四阶逼近的场源深度,结合不同深度异常振幅推断了磁源空间展布关系特征.分析表明,区内北部和西部强磁异常主要由矿体引起,且矿体在中深部产状发生改变;而东部大范围磁异常区主要为二叠系玄武岩所致. 相似文献
998.
新疆哈密东盐池附近变质基底属于塔里木板块北缘北山古生代裂谷带西段一部分,而板块北缘的北山地区古生代进入了陆块裂解、陆内裂谷发展演化时期。笔者对东盐池附近的变质岩进行了研究,将该区域变质作用分为区域变质、动力变质及接触变质等3个类型;将区内变质相分为低角闪岩相、高绿片岩相、低绿片岩相及葡萄石—绿纤石相等4个变质相带相系。研究了地质事件与变质变形的演化趋势,即变质作用从区域中高温变质、区域低温动力变质到区域埋深变质,变质作用的温度和压力随时代更新逐次降低。探讨了变质作用与矿产的关系,即变质作用控制变质矿产的分布。各种变质作用所形成的热液与其他热液一起促使成矿物质的活化迁移至有利部位成矿,形成了黑色岩系中的磷矿、石墨矿和钒矿等。 相似文献
999.
Fan Zhang Xubo Zhang Weiwei Ding Tingting Wang Jian Zhu 《International Geology Review》2020,62(7-8):840-858
ABSTRACT We investigated the oceanic crustal structure and lithospheric dynamics of the South China Sea (SCS) basin through a comprehensive analysis of residual gravity anomaly and bathymetry combined with seismic constraints and interpretation from geodynamic modelling. We first calculated the residual mantle Bouguer anomaly (RMBA) of the oceanic crustal regions of the SCS by removing from free-air gravity anomaly the predicted gravitational attractions of water-sediment, sediment-crust, and crust-mantle interfaces, as well as the effects of lithospheric plate cooling, using the latest crustal age constraints including IODP Expedition 349 and recent deep-tow magnetic surveys. We then calculated models of the gravity-derived crustal thickness and calibrated them using the available seismic refraction profiles of the SCS. The gravity-derived crustal thickness models correlate positively with seismically determined crustal thickness values. Our analysis revealed that the isochron-averaged RMBA are consistently more negative over the northern flank of the SCS basin than the southern conjugate for magnetic anomaly chrons C8n (~25.18 Ma) to C5Dn (~17.38 Ma), implying warmer mantle and/or thicker crust over much of the northern flank. Computational geodynamic modelling yielded the following interpretations: (1) Models of asymmetric and variable spreading rates based on the relatively high-resolution deep-tow magnetic analysis would predict alternating thicker and thinner crust at the northern flank than the southern conjugate, which is inconsistent with the observed systematically thicker crust on the northern flank. (2) Models of episodic southward ridge jumps could reproduce the observed N-S asymmetry, but only for crustal age of 23.6–20 Ma. (3) Southward migration of the SCS ridge axis would predict slightly thinner crust at the northern flank, which is inconsistent with the observations. (4) Models of higher mantle temperatures of up to 25–50°C or >2% less depleted mantle sources on the northern flank could produce large enough anomalies to explain the observed N-S asymmetries. 相似文献
1000.