排序方式： 共有22条查询结果，搜索用时 15 毫秒
11.
12.
杨吝 《广东海洋大学学报》1991,(1)
根据农牧渔业部水产局下达的“294.2千瓦综合节能渔船”项目网具节能课题的要求,新设计了一项低阻底拖网,并进行了网模水池试验和海上实测及一周年商业性捕鱼生产,获得了很好的效果。试验和捕鱼生产结果充分证明:新设计的拖网网口高、阻力小、渔获量高,是一种较为理想的节能型双船底拖网网型,具有增产节能兼优的经济效益和社会效益。 相似文献
13.
14.
Major and trace element, and Sr-Nd isotope constraints on the origin of Paleogene volcanism in South China prior to the South China Sea opening 总被引：15，自引：0，他引：15
Sun-Lin Chung Hai Cheng Bor-ming Jahn Suzanne Y. O''Reilly Bingquan Zhu 《Lithos》1997,40(2-4):203-220
Paleogene volcanic rocks crop out in three sedimentary basins, namely, Sanshui, Heyuan and Lienping, in the attenuated continental margin of south China. Lavas from the Sanshui basin which erupted during 64-43 Ma are bimodal, consisting of intraplate tholeiitic basalt and trachyte/rhyolite associations. Similar to Cretaceous A-type granites from the nearby region, the felsic member shows peralkaline nature [Na2O + K2O ≈ 10–12%; (Na + K)/Al≈ 0.98−1.08], general enrichment in the incompatible trace elements and significant depletion in Ba, Sr, Eu, P and Ti. Although both types of the Sanshui lavas have rather uniform Nd isotope compositions [Nd(T) ≈ +6 to +4]that are comparable to Late Cenozoic basalts around the South China Sea, the felsic rocks possess apparently higher initial Sr isotope ratios (ISr up to 0.713) and form a horizontal array to the right in the Nd vs. Sr isotope plot. Closed system differentiation of mantle-derived magmas in a ‘double diffusive’ magma chamber is considered for the bimodal volcanism, in which the trachytes and rhyolites represent A-type melts after extensive crystal fractionation in the upper portion of the chamber. Such A-type melts were later contaminated by small amounts (1–3%) of upper crustal materials during ascent. On the other hand, composition of lavas in the other two basins varies from tholeiitic basalt to andesite. Their Sr and Nd isotope ratios [ISr ≈ 0.705 to 0.711; Nd(T) ≈ +1 to − 5] and generally correlative Nb-Ta depletions suggest a distinct magma chamber process involving fractional crystallization concomitant with assimilation of the country rock. We conclude that these Paleogene volcanic activities resulted from the lithospheric extension in south China that migrated southwards and eventually led to opening of the South China Sea during 30-16 Ma. 相似文献
16.
17.
Miocene intra‐arc rifting associated with the opening of the Japan Sea formed grabens in several areas in Southwest (SW) Japan, but the extensional tectonics of the arc are still not well understood. In this study, we first document the tectonostratigraphy of the Hokutan Group in the northwestern part of the Kinki district, and demonstrate the termination of extensional tectonics at ca 16.5 Ma, as inferred from grabens in the lower part of the group being unconformably overlain by sediments of the upper part. Second, we review early Miocene grabens in SW Japan to suggest that intra‐arc rifting was abandoned at ca 16 Ma, essentially simultaneously with the end of rotation of the SW Japan arc as evidenced by paleomagnetic studies. The lesser numbers of grabens and reduced thicknesses of graben fills suggest that extensional deformation of the SW Japan arc was significantly weaker than that of the Northeast (NE) Japan arc, which was broken into blocks, indicating various degrees of paleomagnetic rotation within NE Japan. The weak deformation has allowed paleomagnetic studies to infer the coherent rotation of the SW Japan arc. 相似文献
18.
重大活动关键时段的定点预报一直是天气预报服务的难点,因此对2015年北京田径世锦赛开幕式天气的预报思路和方法进行分析总结,结果表明开幕式天气采取了时间、空间逐步递进的精细化预报思路,每个阶段的预报重点、使用的预报方法和信息资料是不同的。短期预报以天气诊断和数值预报方法为主,应用多尺度数值模式和集合预报产品,预报出开幕式当天在东北冷涡背景下北京东部的强对流天气和鸟巢出现弱降水的可能性;短时临近预报依据高时空分辨率的探测资料、快速更新的同化产品和中尺度模式,采用多资料融合技术,对稳定度、水汽和阵风锋等多要素综合分析,预判雷暴的生消变化,跟进预报了开幕式鸟巢地区无降水,保障活动顺利举行。 相似文献
19.
Temperature changing in soil has an influence on the redistribution of water and salt. With constant temperature in an open
system we performed two unidirectional freezing tests with different temperature settings of clay collected at Beiluhe test
site along Qinghai–Tibet Railway. The groundwater supply of the soil was simulated during the experiments by attaching a liquid
replenishment system to the bottom of the sample container. Water content and ions content of the soil were measured after
the experiments. By analyzing the two main ions in the soil we obtained the laws and the properties of water and salt redistribution
during freezing of clay soil. The results show that the water content increases in freezing section while it decreases in
unfrozen section compared with initial water content. To the salt, under this circumstance the diffusion due to the concentration
gradient dominated the transfer way in clay soil, so the ions content in the unfreezing section decreased with the decreasing
of the distance to freezing front. At the ice segregation layer the ions content is less due to the ice self-purification,
and almost nothing changed in frozen section. 相似文献
20.