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The intermediate-basic volcanic rocks with SiO2 content less than 57.48 wt% are high in Al2O3(20.22-16.34 wt%) and K2O, enriched in large ion lithophile elements, show obvious Nb, Ta negative anomaly, these are same to the basalts which formed in island arc. The andesite, dacite and rhyolite rocks with SiO2 content between 62.11-75.19 wt%, are similar with the I-type granitic rocks formed in island arc in their geochemistry. It is suggested that the Jueluotage area of East Tianshan was in island arc setting during Late Carboniferous, when the subduction of the ancient Asian Ocean was in progress.

其中w(SiO2)小于57.48%的中基性火山岩具有高w(Al2O3)(16.34%~20.22%),较富钾,富集大离子亲石元素,具明显的Nb、Ta负异常;w(SiO2)介于62.11%~75.19%之间的安山岩、英安岩和流纹岩岩石化学特征与准铝质的Ⅰ型花岗质岩石相似,其地球化学特征也反映出岛弧花岗岩的特点,表明东天山觉罗塔格地区路白山一带在晚石炭世仍处于古亚洲洋向南俯冲的岛弧环境。

The variations of fronts in the southeast Indian Ocean are analyzed in eddy kinetic energy and thermohaline properties, and the frontogenesis of oceanic fronts is also discussed preliminarily.

极锋区的东向输送流幅宽达4.3个纬度,大于SAF的输送,其间有多个速度峰值,反映了该断面的PF2和PF1具有较大的南北摆动幅度,甚至可能分裂为多个锋。

In this article, seepage and stability against deep sliding are studied and discussed in detail as regard to Dongzhang Dam which has glacis weak surfaces in the dam foundation, some valuable results are obtained.

本文结合坝基含有缓倾角软弱夹层的东张水库大坝工程,对坝基渗流及抗滑稳定性问题进行了较为深入的研究,得出了一些有意义的结论。

East coast of the low-middle-latitude Pacific Ocean and northwest coast of Gulf Stream.

降水量效应主要出现在低纬度海洋、中低纬度太平洋的东海岸和湾流的西北海岸。

In central Himalaya, massif was mainly uplifted in the tectonic model of channel flow during 17~7 Ma at a velocity of ~2 mm/a, then was extruded to earth surface at a much lower velocity. In eastern Himalaya Syntaxis, massif was mainly uplifted in the structural style of titling at a background of isostasy since 4.0~2.2 Ma.

喜马拉雅中段主要在17~7 Ma前以通道流的方式快速隆升,之后的抬升过程相对缓慢;东喜马拉雅构造结则主要在3 Ma以来,以地壳均衡作用为背景的掀斜式抬升为主要隆升模式。

The wind forcing is the most important factor(80%) for generating the JB cyclonic gyre In addition the wind forcing drives the Liman Current and damos the East Korean warm Current in the Winter , and generates the UTB eddies along the Japan Nearshore Branch in all seasons .

风强迫是产生日本海盆气旋性式涡旋的最重要的因素(80%)。此外,风强迫在冬季驱动了Liman Cold Current流,抑制了东朝鲜暖流,并且在全年都产生UTB涡旋和沿着日本近岸分支的一些涡旋。

The wind forcing is the most important factor(80%) for generating the JB cyclonic gyre In addition the wind forcing drives the Liman Current and damos the East Korean warm Current in the Winter , and generates the UTB eddies al ong the Japan Nearshore Branch in all seasons .

风强迫是产生日本海盆气旋性式涡旋的最重要的因素(80%)。此外,风强迫在冬季驱动了Liman Cold Current流,抑制了东朝鲜暖流,并且在全年都产生UTB涡旋和沿着日本近岸分支的一些涡旋。

Based on geology research of the deposits,mechanism of exhalative sedimentary metallization in Dongchuan Copper Field is suggested.

作者结合矿床地质的研究,建立了东川铜矿的喷流沉积成矿机制。

It begins off the east coast of Taiwan and flows northeastward past Japan, where it merges with the easterly drift of the North Pacific Current.

自菲律宾开始,穿过台湾东部海域,沿著日本往东北向流,在与亲潮相遇后汇入东向的北太平洋洋流。

Based on the analysis of Sea Surface Height Anomaly from satellite observation, it is proved that the oscillation with period of 70~210 days is dominating in two branches of the eastward countercurrent in Subtropical North Pacific: Subtropical Countercurrent and Hawaiian Lee Countercurrent.

根据对卫星观测的海平面高度资料的分析,进一步证实了在北太平洋副热带两支向东的流(副热带逆流和夏威夷背风逆流)所在的区域内,海平面高度的70~210天周期振荡是主要的低频变化。

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