Neotectonic inversions in the Baikal Rift System

被引：10

作者：

Ufimtsev, G. F. ^{[1
]}

Shchetnikov, A. A. ^{[1
]}

Filinov, I. A. ^{[1
]}

机构：

[1] RAS, Siberian Branch, Inst Earths Crust, Irkutsk 664033, Russia

来源：

RUSSIAN GEOLOGY AND GEOPHYSICS | 2009年 / 50卷 / 07期

基金：

俄罗斯基础研究基金会;

关键词：

rifting; tectonic inversion; neotectonics; Baikal rift system;

D O I：

10.1016/j.rgg.2008.12.006

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Cenozoic continental rifting in southern East Siberia and northern Mongolia has been associated with subsidence and broadening of rift basins at the account of their mountain borders. This neotectonic trend is, however, superposed with continuous or periodic tectonic inversions in which the basin floor may uplift while marginal fault steps and saddles between basins may subside. Cenozoic geomorphic inversions are expressed in changes of river flow out of Lake Baikal. (C) 2009, IGM, Siberian Branch of the RAS. Published by Elsevier B. V. All rights reserved.

引用

页码：618 / 627

页数：10

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