orogenic belt

The Qiushuwan copper deposit Qinling Group lies in the south of the North Qinling orogenic belt.

秋树湾角砾岩型铜(钼)矿位于北秦岭造山带南侧,含矿地层为秦岭群.

Constraints of age and isotopic compositions on the metamorphic rock units exposed in the southern part of the Dabie-Sulu ultrahigh pressure orogenic belt are essential for the study of regional stratigraphic comparison and further for understanding tectonic process and evolution of this orogen.

厘定大别&苏鲁超高压造山带南缘变质岩带的形成时代和地球化学特征有助于区域地层对比研究和对这一造山带演化过程的深入理解。

Magnetic fabric characteristics of main deformation phases in each tectonic unit of the western Kunlun orogenic belt are studied preliminarily in this paper.

文章对西昆仑造山带各构造单元主要变形期的岩石磁性组构特征进行了初步的研究。

Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.

北淮阳盆岭构造带是大别造山带的重要组成部分.

Garze-Litang fracture zone separates Yidun orogenic belt from Yajiang folded belt.

甘孜 - 理塘断裂带是义敦造山带与雅江褶皱带的分界断裂.

Accordingly, the South China was an Early Paleozoic orogenic belt instead of the Cathaysian Block ( Paleocontinent ).

因此, 华南是早古生代形成的造山带,而不是华夏地块 ( 古陆 ).

Overall average Vp velocity of main hole of 2000m rook is 6. 2km/ s which is correspondent to conclusion with high velocity zone ( 6. 2-6. 3km/ s) of the upper crust in Dabie-Sulu orogenic belt inferred from geophysical methods.

主孔2000m总平均Vp速度为6.2km/s，它与地球物理探测方法获得的大别-苏鲁造山带上地壳具有6.2-6.3km/s高速层结论是一致的。

The Danba area is located in the central part of the Songpan-Ganzi orogenic belt.

丹巴地区位于松潘—甘孜造山带中部.

The Mujiazhuang copper deposit with high radioactive lead isotope area of the South Qinling Orogenic Belt.

铅同位素结果研究表明,穆家庄铜矿矿石铅和近矿围岩岩石铅具有富含放射性成因铅的特点.

Huangcaopo group is the oldest strata in the Eastern Junggar orogenic belt.

荒草坡群是东准噶尔地区最古老的地层,其时代归属问题一直悬而未决.

Meanwhile, discovery and its tectono-paleogeography background of the strata has a great significance for the study of orogenic belt of East Kunlun Mt.

该套地层的发现及其古构造沉积背景的确定对东昆仑造山带的研究具有重要意义。

The upper crust of the Altun orogenic belt has a high average Q value ( about 500). It is likely caused by shallow depth of crystalline basement, outcrop of basement rocks, and slow attenuation of seismic wave.

阿尔金造山带上地壳的平均Q值较高（约500），这可能由于结晶基底埋藏较浅，基岩出露，因此地震波在此处传播能量衰减较慢所致。