Revisiting the Possible Influence of Subsurface Water on the Caspian Sea Level

被引：2

作者：

Zverev, V. P. ^{[1
]}

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

机构：

[1] Russian Acad Sci, Sergeev Inst Environm Geosci, Moscow 101000, Russia

来源：

WATER RESOURCES | 2014年 / 41卷 / 07期

基金：

俄罗斯基础研究基金会;

关键词：

sedimentary basin; sedimentation water; mass fluxes; geofluids;

D O I：

10.1134/S0097807814070148

中图分类号：

TV21 [水资源调查与水利规划];

学科分类号：

081501 ;

摘要：

The likely mass fluxes of deep fluids in the Caspian sedimentary basin have been considered. All such flows have been found to be at least several orders of magnitude less than the water mass required for Caspian Sea level rising by 1 cm/year. It has been proved that any substantial changes in Caspian Sea level can be caused only by an active response of the Caspian sedimentary mantle to tectonic stress in the consolidated basement.

引用

页码：833 / 838

页数：6

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