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tectonic相关的网络例句

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The results show that: On the condition of this paper (1) The initial collision between two continents would cause the tectonic average stress near the collisional point to increase by 5-9 times as compared with regional stress field.

集中程度受碰撞方式、接触面积等因素影响。在本项目采用的模拟条件下,大陆碰撞初期产生的构造平均压力在碰撞点附近,相对于边界压力增大了5~9倍。

The IRSL and GLSL age estimates reported for 11 samples of colluvial and slope wash deposits from trench wall at Xiyangfang, Yanqin county, Beijing, could be useful for understanding tectonic activity in the last 20ka, particular in last 2000 years, in turn, for assessing earthquake risk around the Yanqing area.

北京延庆西羊房探坑剖面崩积物和坡面沉积物11个样品的IRSL和GLSL测年数据将有助于对延庆地区近二万年来,尤其近二千年来构造活动的理解和地震危险性评估。

These dikes are temporally and spatially associated with the gold deposit,and they have the same Pb isotopic compositions,which suggest the comagmatic activities in the same tectonic background.

区内脉岩与金矿在时空上密切伴生,Pb同位素组成接近,应属于同一构造同源岩浆活动的产物。结合前人C-H-O-流体包裹体研究成果,表明胶东金矿化中有幔源流体参与的成分。

The tectonic lithofacies in periphery belt of compressional basin is systematically studied for the first time.

论文首次对挤压盆地山前带的构造岩相带进行了系统的研究。

This is the result of tensional or compressional forces originating from tectonic movement.

当岩石受到因地壳板块移动而产生的张力或横压力时,断层便会出现。

The content of major elements, such as Fe, Mg, Ca and Al, and trace elements, such as Ti, Sr, Ni, Cr and Co, is linearly correlated to that of SiO2, which suggests that the different volcanic rocks in the basin should be the product of fractional crystallization of congenetic magmas. The parental magma may be generated by the partial melting of an enriched mantle wedge formed by the metasomatism of slab-derived fluids in an active continental margin tectonic setting.

FeO、MgO、CaO、Al2O3、TiO2等主元素和Sr、Ni、Cr、Co等微量元素的含量与SiO2含量呈明显的线性相关关系,表明该区火山岩可能是同源岩浆分异的产物,岩石形成於活动大陆边缘的构造环境,并由遭受消减板块流体交代的富集地幔楔部分熔融而形成。

Neoproterozoic Baoxing Complex in middle to lower metamorphic grade, located in western margin of Yangtze Craton, consists mainly of metamorphic gabbroic, dioritic gneisses, tonalitic and granodioritic gneisses, and massive monzogranites The studies of petrochemistry and SmNd isotopes of Baoxing Complex reveal that the gabbroic and dioritic magmas came from a congenetic magma derived from the partial melting of spinel lherzolites in depletive mantle, and that the magma was intensively contaminated by crustal materials during its emplacement The tonalitic and granodioritic magma were derived from the partial melting of metamorphic basalts in the lower crust And the monzogranitic magma was formed from partial melting of metagreywacks Integrating the lithological association, their trace elements, SmNd isotopic characteristics and petrogenesis, the Baoxing Complex must likely have been emplaced in an island arc tectonic background at the Neoproterozoic active continental margin of Yangtze Craton

位于扬子克拉通西缘的新元古代宝兴杂岩主要由中低级变质的辉长质片麻岩、闪长质片麻岩、英云闪长质到花岗闪长质片麻岩和块状二长花岗岩组成。岩石地球化学和SmNd同位素特征表明,辉长质片麻岩和闪长质片麻岩为同源岩浆演化序列,原始岩浆起源于亏损地幔尖晶石橄榄岩的部分熔融,在上升和侵位过程中受到了地壳岩石强烈混染。英云闪长质和花岗闪长质岩浆形成于下地壳玄武质岩石部分熔融,而二长花岗质岩浆形成于杂砂岩的部分熔融。综合分析宝兴杂岩的岩石组合、微量元素和同位素特征,该杂岩体最有可能形成于新元古代活动大陆边缘火山弧构造背景,并可能经历了碰撞过程。

The coarse clastic rock of the braided channel of the fan-delta plain is formed when sedimentary water body is in the salinity stage of active tectonic period, the cotemporaneous cementation is intense and the cementation of the carbonate and sulphate has intense packing action in eogenetic stage of shallow buried.

构造相对活跃期为沉积水体咸化期,主要发育扇三角洲平原亚相的辫状河道粗碎屑岩,同生期胶结作用强,而浅埋藏早成岩阶段碳酸盐和硫酸盐胶结物充填强烈,致使物性进一步变差,并且不利于晚成岩A阶段的溶蚀作用进行。

The reason for the formation of segmentation is due to the different deformational strength, tectonic condition and rock strength, as well as the different slip layers.

分段性指在构造系和构造单元内部,由于变形强度、构造位置、地层强度和滑脱层组合不同而表现出不同构造变形样式。

During the study, in order to decrease the complexity, the article simplifies the geomorphic process, defines the ideal state, and, according to the geomorphic principle, reasons out some of the 4-Dimensional Geomorphic Mathematical Sub-Models that include the 4-Dimensional Tectonic Geomorphic Mathematical Model, the 4-Dimensional Depositional Geomorphic Mathematical Model, and the 4-Dimensional Denudate Geomorphic Mathematical Model.

在研究过程中,为了减低复杂程度,简化了地貌过程,规定了理想条件,并根据地貌学原理推导了部分理想条件下的四维地貌数学模型,分别是四维构造地貌数学模型、四维沉积地貌数学模型和四维剥蚀地貌数学模型。

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