Crustal structure in the Polar sector of the Urals folded system (from DSS data)

被引：0

作者：

Druzhinin, V. S. ^{[1
]}

Rakitov, V. A. ^{[2
]}

Osipov, V. Yu. ^{[1
]}

Nachapkin, N. I. ^{[1
]}

Nedyad'ko, V. V. ^{[2
]}

机构：

[1] Russian Acad Sci, Ural Branch, Yu P Bulashevich Inst Geophys, Ekaterinburg 620016, Russia

[2] VNIIGeofiz GFUP, Geon Ctr, Moscow 107140, Russia

来源：

RUSSIAN GEOLOGY AND GEOPHYSICS | 2014年 / 55卷 / 03期

关键词：

Earth's crust; deep-level structure; deep seismic soundings; Urals folded system;

D O I：

10.1016/j.rgg.2014.01.020

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

A 450 km long composite crustal section of the Urals folded system at 67 degrees N and 60-69 degrees E has been compiled from seismic data on the Polar Urals transect and the results of targeted studies. The main elements of the subsurface structure at more southerly latitudes are preserved for this cross section. The general deep-seated structure is divided into the western and eastern branches. The western one has a northwestern trend and corresponds to the West Urals megazone. The eastern one, with a northeastern trend, includes the Central Urals and East Urals megazones.

引用

页码：390 / 396

页数：7

共 50 条

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