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Zverev V.P., Kostikova I. A.
Sedimentary waters of the Caspian Depression (masses and fluxes) - M.: Scientific peace, 2008. - 138 p.
Silt. 20, Tab. 23, Bibl. 80.
On an example of the Caspian depression the quantitative estimation of sedimentary waters masses and mass fluxes of recent midland sedimentary basin for the first time is given. It is shown, that for 400 million years of evolution in his limits it was accumulated more than 4*1021 g the free and physically connected waters, which most part <3.3*1021g) it was returned back in development of basin. At the present stage the sedimentary cover of the Caspian depression contains 0.74*1021 g, that almost on the order exceeds masses of water in Caspian Sea. For the first time, on an example of a megadepression of the Caspian sedimentary basin, it is executed a comparative estimation natural sedimentary waters mass fluxes and products mudvolcanics (mineral matter, subsurface waters and gases), with anthropogenous mass fluxes extracted petroleum and gas which has shown, that the quantity characteristic discharge of sedimentary waters (138*1012 g/year) and extraction of hydrocarbons (~60*1012 g/year) in the Caspian basin are within the limits of one order and are close enough, and mass fluxes mudvolcanics products on the order it is less.
For wide rond of geologists: hydrogeologists, lithologists, geochemists, geoecologists etc.
| Introduction | 9 | |
| Chapter 1 | Geological and hydrogeological peculiarity of sedimentary basin | 11 |
| Geological structure | 11 | |
| Hydrogeological conditions | 12 | |
| Forms of water in deposits, her properties and mobility | 13 | |
| Features of deep fluids hydrogeodynamic | 19 | |
| Composition of sedimentary waters | 26 | |
| Chapter 2 | Environment and a history of development of the Caspian depression | 33 |
| Caspian waters mass | 33 | |
| Change of a level of Caspian Sea | 36 | |
| Geological structure of the Caspian depression | 40 | |
| Evolution of the Caspian depression | 49 | |
| Oil and Gas potential of the Caspian depression | 53 | |
| Mud volcanism | 55 | |
| Hydrogeological conditions | 58 | |
| Underground discharge to Caspian Sea | 69 | |
| Chapter 3 | Mass of subsurface waters of the Caspian depression sedimentary cover | 72 |
| Chemically connected water | 73 | |
| Free and physically connected waters | 76 | |
| Ratio of masses of water and rocks | 81 | |
| Chapter 4 | Balance of subsurface waters of the Caspian depression | 83 |
| The free and physically connected waters of Northern and Average Caspian Sea | 83 | |
| The free and physically connected waters of Southern Caspian Sea | 85 | |
| Complete balance of the free and physically connected waters | 91 | |
| Separation of chemically connected waters | 96 | |
| Chapter 5 | Masses and mass fluxes of macro components | 100 |
| Composition of sedimentary waters | 101 | |
| Mass fluxes of macro components | 105 | |
| Chapter 6 | Discharge of sedimentary waters | 113 |
| Features of discharge | 113 | |
| Influence on fluctuation of Caspian Sea level | 120 | |
| The basic mass fluxes of geofluids | 128 | |
| Conclusion | 131 | |
| Bibliography | 133 |
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