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tectonic相关的网络例句

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These similar results suggest the detrital thermochronoglogy is a successful method for obtaining information of tectonic ac-tivities.

这表明碎屑颗粒热年代学可以成功揭示构造活动的信息。

The application of detrital geochemistry to determining tectonic setting and provenance attribute is an important means for basin analysis and also a helpful supplementary or verification method in using coarse detrital rocks to judge the background of provenance.

利用碎屑岩地球化学特征判断沉积盆地的构造背景和物源属性是盆地分析的重要手段,也是对利用粗碎屑沉积岩的组分统计判断盆地源区背景的有益补充和验证。

As a result of deuteric tectonic destroy and weathering effect,the Jehol bita's palaeogeograpic and basin sedimentary characteristics are hard to make detailed field works and nethermore research.

然而热河生物群产出的古地理环境和盆地沉积特征的研究由于受到后期构造破坏和风化作用的影响,难以开展详细的野外工作,研究程度较低。

These extensional basins were formed at the background which was the tectonic dynamic of horst-uplifing and graden -downfalling at continental crust of the Qinling under slow convergence comprehensively deep lithosphere.

中泥盆世,在伸展作用增强的背景下,在柞山一级盆地内,由次级同生断裂作用形成了断陷型三级构造热水沉积成矿盆地。

The magmatic activity of collision granites provides the information about the tectonic dynamics from the continental margin epicontinental of the south of Erguna block in the Neo-proterozoic to Early Cambrian.

碰撞型花岗岩的岩浆活动提供了该区新元古代-早寒武世额尔古纳地块南部大陆边缘陆缘增生的构造动力学信息。

Negative Ce anomaly is one of diagnostic criteria of geotectonic setting of silicalite. Silicalite in Golug, Xinrenlang and Lhazê in the Gangdisê tectonic belt is characterized by unclear negative Ce anomaly characteristic of epicontinental or neritic sediment, while silicalite in Gyüzê La-Jiaqing area is characterized by weak negative Ce anomaly characteristic of sediment in transitional belt between oceanic basin and continental margin.

硅质岩Ce异常特征是构造背景判别的最有效的手段之一,冈底斯构造带谷露、新认朗与拉孜地区的硅质岩Ce负异常不明显,属大陆边缘或浅海环境,而九子拉家青地区的硅质岩具弱的Ce负异常,属大洋盆地与大陆边缘之间的过渡环境中的沉积。

The epicontinental arc volcanics related to the Permo-Triassic activities suggest the subduction of the Jinshajiang oceanic crust,and the ocean-continent tectonic regime transformation and the northward accretion of continental crust.

与二叠纪和三叠纪活动陆缘有关的陆缘弧火山岩带反映金沙江洋壳发生消减、洋-陆构造体制转换和大陆地壳向北增生的过程。

Beiqinling is between Shangdan Fault and Baoji-Luonan-Luanchuan Fault, it have own particularities in structure, geochemistry, physical geography and stratigraphy, on the stand of tectonic, it's the real division between north China and south China, and the key region to study the evolution of Qinling erogenic belt during later Paleozoic-early Mesozoic.

北秦岭构造带夹持在宝鸡—洛南—栾川断裂带和商丹断裂带之间,其组成及结构构造既不象其北侧的华北板块南缘构造带那样与华北板块相似,也不象其南侧的南秦岭构造带那样与扬子板块相似,在地层、构造、地球化学和地球物理各方面均具有独特性,从大地构造意义上说,它才是中国大陆南北之间的真正分界带,也是解析秦岭晚古生代一早中生代演化的关键区段。

Chagan sag is a secondary tectonic unit in Chagandelesu Depression, northeastern Yingen-Ejinaqi basin, and the basement of the basin is a Paleozoic fold belt of continental margin or island arc at the connection region of North China plate* Tarim plate and Kazakstan plate, with the character of erogenic belt.

查干凹陷属于银根—额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元,其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带,具有古生代造山带的性质。

This paper summarizes various structural models, structural belts, Cenozoic deformation frameworks and tectonic evolution concerning intraplate deformation in the West Kunlun - Pamir Cenozoic erogenic belt and Southwest Tarim foreland basin and suggests that the Cenozoic intraplate deformation be characterized by segmentation and stage evolution.

笔者总结了西昆仑—帕米尔造山带及塔西南前陆盆地板内变形的各类构造模式、构造分带、新生代变形格局及构造演化,提出其新生代板内变形具有弧形构造分段性和阶段性演化的特点,发现了依格孜牙、柯克亚、桑株—杜瓦、卡兹克—阿尔特薄皮弧形推覆构造、齐姆根主弧形构造段及玉力群—克里阳构造段的三角带构造及叶尔羌—棋盘对冲过渡型弧形构造。

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