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The differential movement of lithosphere and asthenosphere causes the Neozoic deformation of Tianshan.

岩石圈和软流圈的差异运动导致了天山新生代构造变形。

All the volcanic rocks present younger K-Ar age (less than 5Ma), which can be termed as Cenozoic rocks. In general speaking, volcansim can be dividied into two eruptive stages. In the first stage, volcanic rocks for Pliocene epoch (4. 4-5Ma) consist of basanite and tephrite, which distributed on Mt. Crater, Cape Bird, and southern bank of Bonney Lake; In the second stage, volcanic rocks for Quaternary (less than 1 Ma) are mainly composed of latite, which are distributed on Cape Rodeys and Cape Evens.On the basis of geochemical data such as major elements, trace elements , rare earth elements, isotope, microprobe analysis, combined with main achievement taken by previous researcher in this area, conclusions are drawn basically as follows

所喷发的火山岩K-Ar年龄值均小于5Ma,为新生代火山岩,大体上可以分为两个喷发阶段,第一个阶段为上新世火山岩(年龄值为4.4-5.0Ma),主要由碧玄岩和碱玄岩组成,分布于罗斯岛上的克雷克特山、鸟角和泰勒谷的博尼湖南岸;第二阶段为第四纪火山岩(年龄值均小于1Ma),主要由安粗岩组成,分布于罗斯岛上的罗德角和伊万思角,通过主要元素、微量元素、同位素结合电子探针以及前人的研究成果,我们大体上可以得出如下认识

The determined thermal conductivity values vary from 0882 to 678 W/m?K and the calculated heat flow values in Jianghan Basin range from 419 to 609 mW/m2,with a average of 523 mW/m2.It shows that the influence of tectonothermal event before Cenozoic in Jianghan Basin has faded away,and the basin has cooled down.

结果显示江汉盆地热流419~609 mW/m2,平均523 mW/m2,盆地总体表现为较低的大地热流,反映了中新生代以来构造活动逐渐减弱,盆地不断冷却的结果;从盆地内热流分布看,热流分布南高北低,反映了江汉盆地构造活动的不均一性。

Cenozoic deformation is well developed in the basin/range coupling regions on both sides of Tianshan Mountains, where is also a natural laboratory for studying the coupling dynamics of basin and range.

天山两侧山前新生代构造变形强烈,是研究盆山耦合动力学机制的理想场所。

However, obviously, his attitude to life is not purely sensory, autistic, negative or cynical, even not neutral. At least, according to the painter's statement, the motivation of the concern is "re-propose the issue of interaction between people and society and the new objective for reflection", to show an ideal of "overcome loneliness, overcome negative, overcome impetuousness."(Deng Jianjin's Readme). I think basing on this starting point for thinking, he keeps the proper distance with the new generation art whose attitude to life is straightforward, graphic, artificial and evasive.

但很明显,他对生活的态度不是纯感官性的、自闭的、消极的或泼皮式的,甚至也不是中性化的,至少,按照作者自己的说法,这种关注的动机是为了"重新提出人与现实社会的感应问题和新的反思对象",为了展示一种"战胜孤独、战胜消极、战胜浮躁"的理想化的东西,我想,正是在这个思维起点上,他与那些平铺直叙、图解化、矫饰的逃避式地对待生活的新生代艺术保持了应有的距离。

Overseas Chinese literature in the ten years of the new century, presented at a deeper level the integrity of the overseas Chinese writers in the "new old" hand-over communication between the generations, the Chinese writers generation and new immigrants from overseas due to the deep-seated patterns of Chinese literature adjustments, Chinese development in the cultural displace and spread , and all reflect the efforts of overseas Chinese literature beyond the east and west binary to point the "third element".

新世纪10年海外华文文学在深层次上呈现的中华民族文学的整体性,海外华文作家"新老"交接中的世代沟通,华人新生代和新移民作家创作引起的海外华文文学格局的深层次调整,汉语在文化流徙传播中的丰富发展,都反映出海外华文文学超越东、西二元而指向"第三元"的努力。

As BM of new age,do you have any suggestion about construction of the community?

作为新生代的斑竹,请你谈谈你对社区的建设有何意见和建议。

The bogle is one cainozoic era exchange way, is the modern network time representative, is one life style and the new work way.

博客是一种新生代交流方式,是现代网络时代的代表,是一种生活方式和新的工作方式。

Through the analysis of geometrical features of Mesozoic-Cenzoic sedimentary basins in the Lower Yangtze area, we think them to be asymmetric tectonic sinked basins. They are bounded by a set of boundary fault system and failed conjugate fault, and they are segmented along axes.

通过对下扬子区中、新生代非对称性沉积盆地的几何学特征分析,认为这种非对称性构造沉降盆地在剖面上表现为由一组主边界断层和一组天折的共轭断层所围限,而且在走向上具有分段特征。

Ore source of celestite mineralization system is complex in this area. Weathering and erosion of the floor of the basin and the mountain around the basin, evaporite sediment in the earlier, deep water, Mesozoic and Cenozoic volcanism can provide the strontium. In particular, serving as initial ore source, oil-field brine supplies the majority of strontium.

该区矿源场分析表明,锶的来源有基底和周边山系风化剥蚀来源、老含盐地层补给、深部水和中、新生代火山活动补给;其中,盆地基底和周边老山风化以及深部水补给为主要来源,特别是油田水作为矿源层为锶矿床的形成提供了大量锶源。

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