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61.
Xue-jie Li Zhe Wang Yong-jian Yao Hong-fang Gao Song Zhu Zi-ying Xu 《China Geology》2023,6(1):154-167
The existing genetic models of the South China Sea(SCS) include an extrusion model of the Indochina Peninsula, a back-arc extension model, and a subduction and dragging model of the Proto-South China Sea(PSCS). However, none of these models has been universally accepted because they do not fully match a large number of geological phenomena and facts. By examining the regional tectonics and integrating them with measured data for the SCS, in this study, a back-arc spreading-sinistral shear model ... 相似文献
62.
赵健赟 《测绘与空间地理信息》2020,(1):14-17,22
新型测绘是未来测绘行业发展的趋势,在分析目前全国大学生测绘技能大赛与高校测绘教学现状的基础上,构建面向新型测绘的技能竞赛体系,并根据新型测绘的基本构架设计对应的理论与实践教学模块和基本的理论教学改革方案,提出基于CDIO模式进行测量实践教学改革,以实现技能竞赛引导下的创新性、应用性人才培养。 相似文献
63.
Based on new multibeam bathymetric data and about 300 km long single seismic profiles, three topographic units were identified:the canyons, fractural valley and submarine terrace on the north of Chiwei Island where is a structural transition zone between the southern trough and the middle trough. The Chiwei Canyon and the North Chiwei Canyon are two of the largest canyons in the East China Sea (ECS) slope. Topographic features and architectures of them are described. The study shows that both of them are originated along faults. The evolution and spatial distribution of topographic units in the study area are controlled mainly by three groups of faults which were formed and reactive in the recent extensional phase of Okinawa Trough. The Chiwei Canyon was initiated during the middle Pleistocene and guided by F4 that is a N-S trending fault on the slope and F1, a large NW-SE trending fault on the trough. The pathway migration from the remnant channel to the present one of Chiwei Canyon is the result of uplift of tilted fault block that is coupled to the recent extension movements of the southern trough. The submarine terrace is detached from the ECS slope by the NEE-trending fault. The North Chiwei Canyon, developing during the late Pleistocene, is guided by F5, a N-S trending fault, diverted and blocked by the submarine terrace. 相似文献
64.
研究了基于组件嵌入式网络GIS解决方案,首先介绍了网络GIS实现的主流Java方法,分析了它们的优缺点,重点论述了嵌入式组件技术和基于组件嵌入式网络GIS的实现原理,介绍了它的设计和实现方法,最后给出了实验结果并和Java实现方式作了比较。 相似文献
65.
东海陆架边缘的构造特征记录了有关冲绳海槽张裂过程的关键信息,对于进一步理解海槽的形成演化以及弧后张裂与弧-陆碰撞之间的相互作用至关重要。本文基于多道地震和重磁资料,分析了东海陆架边缘的地形和构造特征,并对冲绳海槽早期张裂过程、北西向断裂带的分隔控制作用、钓鱼岛隆起带南北构造差异和冲绳海槽的向西前展等问题进行了探讨。结果表明,冲绳海槽西侧陆坡存在的分段性,各分段在地形地貌、地层展布和构造特征等方面的不同,体现了其构造演化和现今构造活动性的差异。冲绳海槽中—北段的张裂始于陆架前缘坳陷,在晚中新世向东扩展至整个海槽,晚中新世至今以分散式张裂为主。北西向断裂带对东海陆架边缘不同分段的构造特征和构造活动起到了分隔控制和转换协调作用,控制了不同类型陆坡的形成和发育。受冲绳海槽在全宽度上向西前展的影响,钓鱼岛隆起带南段的基底隆起及其支撑的陆架边缘发生了破坏和沉降,形成基底起伏较大、地形崎岖不平的陆坡。 相似文献
66.
Angela Dikou 《Marine Ecology》2009,30(4):405-415
Skeletal linear extension rates of a foliaceous, IndoPacific, skiophilous, heterotrophic, scleractinian Merulina ampliata (Ellis & Solander 1786) were obtained along a sediment/nutrient load gradient at the southern islands of Singapore. Measurements were made during November 1999– November 2000 using the alizarin red‐S staining technique. Suspended particulate matter concentration (r2adj = 0.76), turbidity (r2adj = 0.59), the organic content of suspended sediments (r2 = 0.50), and nitrite‐nitrate concentration (r2adj = 0.50) were significant predictors of the skeletal linear extension rate of M. ampliata. Maximum linear extension growth rates of M. ampliata (mean ± SD: 1.43 ± 0.67–3.26 ± 0.59 cm·year?1) were comparable to 15‐year‐old accounts at the same research sites, indicating adaptation to low‐light, high‐sediment waters. 相似文献
67.
On the basis of the soil environment investigation in Da'an City, Jilin Province, China, 40 soil samples from main land use types were obtained and tested by standard method. Soil organic matter (SOM), total N (TN), total P (TP), total K (TK), available N (AN), available P (AP) and available K (AK) were chosen as the evaluation factors. A regional soil nutrient evaluation model was developed based on the matter-element model. The results show that the soil samples with nutrient grade Ⅱ-Ⅴ respectively account for 10%, 30%, 32.5% and 27.5%, and those with grade Ⅳ and Ⅴ account for 60% in all samples. The relationship between soil nutrients and land types indicates that the nutrients of farmland are relatively good, with 41.7% of soil samples with the nutrient grade Ⅳ and Ⅴ. The nutrients of saline-alkali land and sandy land are the worst, with 100% of soil samples with the nutrient grade Ⅳ and Ⅴ. And the ratios of soil samples grade Ⅳ and Ⅴ in grassland and wasteland are respectively 62.5 % and 54.55%. Generally speaking, the soil nutrients status in Da'an City is poor, 60% of soil samples are in poor and extremely poor conditions, indicating that the soil has been severely eroded. Being a relatively superior evaluation method with more accurate resuits and spatial distribution consistency, matter-element analysis is more suitable for regional soil nutrient evaluation than previous models. 相似文献
68.
机载LiDAR在公路勘测方面的用途日益广泛。该文对直升机机载LiDAR在高速公路改扩建中的应用技术路线可行性进行了研究论证,从地面控制测量、点云数据获取、点云数据处理、成果应用等多个方面进行了阐述,通过分析LiDAR点云数据在5种不同地面控制点布设方案校正下的点云数据精度,论证了利用地面控制点对直升机机载LiDAR点云数据进行平面和高程校正的可行性。 相似文献
69.
可拓学是研究事物拓展的可能性和拓展规律与方法的科学,它可以广泛的应用于各种矛盾和对立问题的解决.可拓分类方法是利用可拓学理论对事物类型归属进行研究的动态分类方法.为了解决储层流动单元分类中现存误判率较高的问题,本文利用可拓分类方法对储层流动单元分类进行了研究,并把利用可拓分类获得的流动单元分类结果与灰关联聚类法判别分析结果进行了比较,发现可拓分类方法具有更强的判别能力,具有实用性强、误判率低的特点,判别准确率可比灰关联聚类法提高15%.这种方法不仅仅适用于流动单元分类,对于油气勘探开发的很多环节都将具有适用性. 相似文献
70.
W. Franke 《International Journal of Earth Sciences》1993,82(3):505-515
The brachyanticlinal structure of the Saxonian Granulite Complex was formed, or at least overprinted, by large-scale crustal extension, which is documented in an extreme reduction of the metamorphic profile and a pressure-temperature path with nearly isothermal decompression. the granulite is situated within a south-west-northeast trending belt characterized by basaltic volcanism and an intrabasinal, sediment-producing rise, both active in Frasnian times. These features are taken to reflect at least part of the extension which has exhumed the high grade rocks; however, Cambro-Ordovician rifting possibly initiated the process. The Frasnian palaeogeography and geophysical data suggest that the axis of the granulite dome extends at least 150 km towards the south-west. The overall setting strongly resembles the metamorphic core complexes of the western USA, but the exhumation of rocks preserving evidence of metamorphic pressures of 10–12 kbar requires much higher extensional strain, possibly due to the longer period of stretching. Early Carboniferous compression and minor post-collisional extension (Late Carboniferous to Permian) have not significantly modified the earlier geometry. U-Pb and Sm-Nd data ranging between 380 and 340 Ma are interpreted to record retrogression during uplift rather than peak metamorphism. 相似文献