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Massif Central相关的网络例句

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In Great Wall's enemy tower, the beacon-fire shop room, in the stele carving engraved inscription and the mountain massif touches the crag prefatory remarks, is the Great Wall culture main body; Inside and outside the Great Wall spreads in the folk story fable, is the Great Wall culture bright oral literature.

长城上的敌台,烽燧铺房,碑刻铭文及山体上的摩岩题记,是长城文化的主体;长城内外流传在民间的故事传说,是长城文化灿烂的口头文学。

The Wandashan massif, in which occurred HIMU-type OIBs with highly radiogenic Pb isotope compositions from the Raohe area, is a foreign terrane accreted to the CAOB.

其中在完达山地体的饶河地区出露了一套异常高Pb同位素比值的HIMU型洋岛玄武岩,代表了中生代的新增生外来地体。

In Yanbian area, high-alumina granites such as Dongqing and Weizigou rock were considered as typical Stype granite and represented the collision of Jiamusi Massif and North China Craton because of the mineral assemblage of garnet and muscovite.

在延边地区,以东清和苇子沟岩体为代表的高铝花岗岩,因其含有石榴石和白云母矿物组合,曾被认为是典型的S型花岗岩,且代表了佳木斯和华北地台的碰撞拼合。

It boasts of wonderful scenic canvas of Himalayas stretching form Mt. Kanchanjunga in the far east to the Annapurna massif in the far west and the revering sunrise that serenades the entire valley.

酒店有 33 间客房,所有客房均面对美丽的喜马拉雅山脉,从这里您能将整个纳迦克特山丘和喜马拉雅山脉的风景尽收眼底,包括早上那令人心醉的日出。

According to Rong County person in charge of construction bureau, mainly divide into 5 areas in large-scale Big Buddhism park: Buddhism culture area, mountains and rivers culture area, comprehensive activity region, the plant appreciation area and recreation and spending holidays area, it joins three mountain two water in Rong County, will pass the energetical afforestation of the massif correctly, improve Big Buddhism's surrounding environment.

据荣县建设局负责人讲,规模宏大的大佛公园主要分5个区域:佛教文化区、山水文化区、综合活动区、植物观赏区和休闲度假区,它连接荣县的三山两水,将通过对山体的大力绿化,改善大佛周边环境。

The fault that appears to have broken in the earthquake is at or very near the boundary between the Precambrian rocks of the Pengguan Massif and the Mesozoic foredeep sediments of the Sichuan Basin .

在地震中被断裂层位于或者接近于彭观山丘前寒武纪岩石与四川盆地中生代前缘沉淀层的边界地带。该断裂带大多情况下向右横向

The massif of Turbacz (1310m o.s.l.),the highest mountain of Gorce,is of a starfish shape.

呈海星形状的Turbacz山丘(海拔1310米)是Gorce山脉中最高的一座。

Recent studies of abyssal peridotites show that they are not melt residues of batching or fractional melting of pyrolite directly after melt extraction of MORB. Petrological studies of peridotites from Luobusa ophiolite massif also indicate that the mantle peridotites are not simple residues of primary pyrolite either.

罗布落蛇绿岩橄的镜下观察和岩石化学资料也证明,它不是原始地幔岩经局部熔化后的残余物,而且由来自更深层的地幔过渡带的硅酸盐超高压矿物底辟上升经熔取出玄武质熔体后,再次局部熔化后的残余物。

Based on the regional tectonic evolution, combined with the high precision isotopic ages from this paper and other geologists, we have some new acquaintances as follows: 1 There has no Caledonian granite belt distributed in north margin of North China Craton. So, the traditional evolving model of North China Carton, which formed on this idea and the acquaintance about the collision of North China plate and Siberian plate, must be incorrect; 2 The age date show that the earliest magmatic activity began since late-Palaeozoic Permian, which is inconsistent with the previous idea that there were Caledonian and Hercynian active continental margin in the north of North China Craton and in the south Xingkai Massif. 3 the crust and lithosphere were thickened by the subduction and collision of Siberia plate and North China plate during Late Paleozoic. The magma is formed when the crust is heated and melts caused by thickened lithosphere delamination and caused the Asthenosphere upwelling. But only a little basaltic magma erupted, most magma underplate under the bottom of the crust. Thermal energy derived from basaltic magma underplating made the middle and lower crust melt partially and the late Permian-early Triassic granites is formed in large scale.

根据区域构造演化分析,并结合本文及他人高精度同位素年龄,我们对延边花岗岩形成的大地构造环境有了新的认识:1在华北地台北缘并不存在所谓的加里东花岗岩带,因此,建立在此之上的传统的华北地台北缘演化模式及有关西伯利亚板块与华北板块的碰撞拼合的认识也必然是不正确的;2华北地台北缘和兴凯地块南缘不存在加里东期和海西期花岗岩带,表明两地块边缘最早的花岗质岩浆活动始于晚古生代的二叠纪,即不存在传统观点所认为的加里东期或海西期活动陆缘;3晚古生代由于西伯利亚板块与华北板块的俯冲碰撞,致使地壳和岩石圈增厚,导致加厚岩石圈发生拆沉作用,使得软流圈上涌,加热地壳使之熔融形成岩浆,但玄武质岩浆少量喷出地表,大部分底侵于地壳底部,形成下地壳高密度的玄武质底侵层,玄武质岩浆底侵的热能引起中下地壳广泛部分熔融,形成大面积分布的晚二叠世—早三叠世花岗岩。

Based on the distributions of nitrogen-compounds in the reservoirs, there might be two individual petroleum carrier systems along the HLSR: the Upper and the Lower systems, which happened to be bordered by a thin layer of marls widely spreaded in the Dongsha Massif.

含氮化合物在油藏空间上独特的分布特征表明,两个相互独立的输导系统存在于惠流构造脊上:称之为上、下输导系统。

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