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continental相关的网络例句

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与 continental 相关的网络例句 [注:此内容来源于网络,仅供参考]

Keywords : outer continental shelf; Article 76 of UNCLOS; strategy on continental shelf

中国亟需制定一份属于自己的大陆架延伸战略。

Volcanic rifted margins are a kind of continental margin formed during continental breakup. Their geodynamic evolution is as complex as that of active margins.

火山型被动陆缘是大陆解体过程中形成的一类陆缘类型,其演化过程与活动陆缘一样复杂多变。

These are proper rear boundaries of continental margins, the geodynamics of which are characterized by rifting on shelves, continental slopes, and marginal oceanic depressions.

它们位于大陆边缘区的后缘,其地球动力学作用以大陆架、大陆斜坡和边缘海沉降区域的裂谷作用为特征。

Such features are typical of ancient lower continental crust, e.g., Archean granulite terranes that experienced extensive U-Th loss and developed time-integrated low radiogenic Pb compositions. The occurrence of the west Ujimqin andesites indicates the existence of ancient continental lower crust beneath the NE China fold belt.4 The Mesozoic granitoids in the Zhangguangcai Range and Jiamusi block have lower Nd ε_(Nd =-3.5~+ 2.1, T_ = 1.0~1.27Ga and highly radiogenic Pb and Sr isotopic composition ~(206Pb/~(204)Pb = 18.4~18.9,~(87)Sr/~(86)Sr = 0.705~0.711, suggesting that the pelagic sediments of the Paleo-Asian Ocean or their metamorphosed derivates were an important component in the region.5 The Pb isotope mapping results show that the mafic rocks in the northern Hinggan Mountains have higher and weakly variable ~(206)Pb/~(204)Pb ratios than those from the southern Hinggan Mountains and the Liaoyuan-Yanji area.

该套岩石的出现为证明东北地区存在古老大陆下地壳提供了重要证据。4张广才岭-佳木斯地区中生代花岗岩表现出低ε_(-3.5~+2.1)、高T_(1.0~1.27Ga)和高放射成因Sr~(87Sr/~(86)Sr=0.705~0.711和Pb同位素组成~(206Pb/~(204)Pb=18.4~18.9,反映了古亚洲洋远洋沉积物或变沉积岩为区域地壳的重要组分之一。5同位素填图结果表明,大兴安岭北区基性火山岩表现出较高且变化小的~(206)Pb/~(204)Pb比值;而南兴安岭-辽源-延吉地区中生代基性火山岩整体上表现出相对北区低~(206)Pb/~(204)Pb同位素比值特征。

For the former,continental law system takes it as unauthorized agency,that s,which can t generate the consequence of effect agency;For the latter,continental law system names it as agency by estoppels regarded as the agency of authorized agency.

对于前者,大陆法系理论界通称为狭义的无权代理,即不发生属于有效代理的法律后果;对于后者,则称为表见代理,表见代理即被称视为有代理权之代理,将发生与有权代理一样的法律后果。

For the former,continental law system takes it as unauthorized agency,thatis,which can t generate the consequence of effect agency;For the latter,continental law system names it as agency by estoppels regarded as the agency of authorized agency.

对于前者,大陆法系理论界通称为狭义的无权代理,即不发生属于有效代理的法律后果;对于后者,则称为表见代理,表见代理即被视为有代理权之无权代理,将发生与有权代理一样的法律后果。

In order to deepen understanding in the MQZ at the northern continental margin of the South China Sea, this paper summarized three possible occurrences of the global MQZs originated from physical, chemical and structural processes, respectively, located at marginal zones and abyssal zones of the global oceans, mainly Jurassic MQZs both in the Atlantic and the western Pacific, Cretaceous MQZs in the northern Pacific, the Indian and in the Southern. Meanwhile, it is worth attaching importance to mantle plume activities in different scales, small magnetic sources induced by initially fragmented ridge oblique to the continental margin and faint magnetic lineations in those MQZs.

为了加深认识南海北部陆缘磁静区,归纳了全球深海和边缘两大类型磁静区的物理、化学及构造三大成因,主要包括大西洋和西太平洋侏罗纪磁静区,以及北太平洋、印度洋和南大洋白垩纪磁静区,强调磁静区与不同程度地幔柱活动、斜交扩张初始产生的小型错断磁源体及隐含弱磁条带关系的重要性。

Based on the fractal theory and the area data of the global continental massifs,both of the characteristic yardstick of the modern global continental massifs and their frequency have been analyzed and discussed in this paper.

根据分形理论和各板块的面积以及现代大陆各地块面积资料,分别进行了全球岩石圈板块和全球大陆地块自相似性特征尺度与频度关系的研究讨论。

In the northern part of the Okinawa Trough,at about 7.5-7.0kaBP of the early Holocene, this studied region was controlled by the continental shelf water, and at about 7.0aBP Kuroshio water combined with continental shelf water intensively, then the region was controlled by the intensified Kuroshio water with upwellings during 7.0-6.0kaBP; from 6.0-2.0ka BP the upwellings developed stably and the thermocline gradually declined: from 6.0-5.0 kaBP the impact of the upwellings mainly focused on the thermocline and much less on the sea surface, from 5.0-4.0kaBP the SST decreased because the sea surface was influenced by the cool water brought by the intensified upwellings; from 2.0-1.2kaBP, the upwelling declined and the SST increased consequently; since 1.2 kaBP the upwelling increased and the thermocline declined obviously.

冲绳海槽北部、九州西南海区,全新世7.5-7.0ka BP陆源物质影响明显, 7.0kaBP前后黑潮侵入并与陆架水强烈混合,7.0-6.0ka BP期间黑潮影响逐渐控制了该区,上升流开始发生,温跃层开始变浅;约在6.0-2.0ka BP之间上升流持续稳定发育,温跃层深度逐渐下降:6.0-5.0ka BP上升流影响作用于温跃层但对表层影响较小,5.0-4.0ka BP海水表层温度受上升流冷水影响降低;而约2.0-1.2ka BP,上升流减弱,海水表层温度回升;近1200年来上升流加强、温跃层深度减小的趋势更加显著。

It is a rare example of an active continental rift zone, where a continental plate is attempting to split into two plates which are moving away from one another.

它是一种罕见的例子,一个活跃的大陆裂谷带,其中大陆板块是企图分裂成两大板块,其中正在远离1。

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