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flysch相关的网络例句

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与 flysch 相关的网络例句 [注:此内容来源于网络,仅供参考]

The structural mélanges is of the shape of a trumpet with its west section more wide and its east section more narrow, being made up of flysch slice, archibathyal silicalite, argillite slice, serpentinite slice, island arc slice, carbonate rock slice, continent-breaken pieces and so on.

该带西宽东窄,呈喇叭状,由复理石岩片、深海硅质岩、泥质岩岩片、蛇纹质岩片、火山岛弧岩片、碳酸盐岩岩片、大陆碎片岩片等组成。其中以复理石岩片为基质包含其它外来构造岩片。

The deposition of flysch onto the young floors of chiasmic basins is widely accepted as certain.

复理石的沉积作用发育在裂陷盆地年青底板上的看法被广泛接受。

The basin sediments include volcaniclast and deep-water deposit from arc and terrigenous flysch deposit.

盆地沉积物包括来自岛弧的火山碎屑、深海沉积物和陆源复理石沉积。

There is the obvious character of passive marginal basin in Yangtze south-east margin, and there is the continental-margin rifting basin in Huaxia north-west margin, which is characterized by the thick flysch sediment as well as the narrow and steep distribution zone.

华南加里东褶皱带是扬子陆块与华夏陆块及其间的华南洋经过加里东造山运动的碰撞产物,但关于这次碰撞的性质及其成因,在我国存在多种不同的看法。

The deep-water in situ deposits and deep-water allogene deposits develop flysch rhythmic sequences.

深水原地沉积与异地沉积在剖面上组成了复杂的复理石韵律。

The Zhusileng-Hangwula belt is between the Yagan fault and the Engger Us fault. Early Palaeozoic non-volcanic flysch shows that it is a pa...

上述各构造单元在沉积建造、岩浆岩组合、变质作用以及地球化学特征等方面都有明显的差异,单元之间以断裂作为界线。

During the Neoproterozoic to the Early Paleozoic, the South China was a marginal basin captured by the Yangtze active continental margin, filled with very thick flysch, sandstone, and shale sediments.

华南新元古代到早古生代是扬子活动大陆边缘构造"捕获"的一个边缘海盆地,其间充填了巨厚的复理石、砂、页岩沉积。

Combining the discusses of flysch prototype basin which is called Baryan Har basin, we know that the Baryan Har basin is a large-scale back-arc basin resulted from intensively depression of back-arc area. It formed after tectonic setting transforms to pressure from extension and is at the same time as development of Yidun island arc.

同时,结合对沉积复理石的原型盆地——巴颜喀拉海盆性质的讨论,以为巴颜喀拉海盆是在松潘-阿坝地区构造背景由拉张转化为积存之后,在义敦岛弧发育的同时,弧后区强烈坳陷形成的大型弧后盆地。

The unit bottom was the unconformity developed by Wuling Movement, and the unit top was overlapped by glacial deposition of Nanhua System. What\'s more, an unconformity can be found in Northern Guizhou and North-western Hunan. At the same time, this boundary was an important transformation between different deposition types: Banxi Group was rift basin deposition with flysch suite, and bearing a vast amount of pyroclasts, and this suggests that there was strong activity of crust. But the overlapping glacial deposition stood for steady deposition with penecaprock characteristic, and under unique climate environment.

下为武陵运动形成的角度不整合面所限;其上被南华冰期沉积所超覆,在黔北—湘西北可见角度不大的不整合,而且这一界面是两个不同沉积类型或建造之间的一个转换:板溪群为具有复理石韵律的裂谷系充填,其中发育大量火山碎屑沉积,显示较强的地壳活动性;而上覆的南华冰期沉积所代表的是一个具有准盖层性质的、独特气候环境下的稳定沉积。

Its sedimentary formation consists of predominant flysch tur bidite and shale.

地槽阶段开始于早寒武世,一直延续到中志留世。

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