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Salt Systems of the Earth

Salt Systems of the Earth


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About the Book

The most comprehensive and in-depth study of the formation, practical applications, history, and natural recycling of salt, including the global and geological implications of its formative process, natural movement, and development in the Earth's subsurface.

Like water, salt is one of the most commonplace items in our everyday lives. From the omnipresent shaker that you see on every table in every restaurant, to the ocean water we swim in, salt is something that we rarely think about. But there is much more to the story of salt than most people think. Not only is salt a natural resource that must be captured and refined for public consumption, but salt domes, large deposits of salt that form under the ground, are important for finding and drilling for petroleum and natural gas. Salt is so important that, in ancient times, it was sometimes used as a currency in various cultures around the world, and it has been used as a food preservative, long before refrigeration was invented. Salt is something we rarely think about, but it is one of the most important natural resources that exists.

This is the first integrated study of salt's global development in the Earth's subsurface, its tectonic history and kinematic evolution, live salt-naphtide interconnections, and their geological recycling. The Earth's salt is shown as a peculiar umbilical thread in the analysis of numerous geological processes of salt formation, transformation, migration, discharge and regeneration, and their association with hydrocarbons. Presented here is the science of salt, including the active salt bodies' live in Earth's subsurface, their fate and influence over the other geological processes, including grandiose systems of kinetically interrelated allochthonous nappe-like and sub-vertical bodies formed by the migrating salt. Also included are a description of sub-conformable sheet-like salt bodies formed not by the evaporation but by emigration of buried brine-salt masses and their discharge at new, younger stratigraphic levels, a description of a phenomenon of the halo-volcanism due to depth breakthroughs and explosive discharges of the hydrocarbon-brine-salt masses, an examination of the over-diapir surface and brine lakes with fluctuating levels, and many other things. The book provides new interpretations of numerous issues reflecting the salt life manifestations and gives a key to a broad circle of the geological enigmas, from global events like the Messinian crisis in the Mediterranean to Biblical legends and enigmas of the Dead Sea-lake.

Whether you are a scientist or student working in the natural or Earth sciences, a geologist, an anthropologist, a petroleum engineer, a petrophysicist, or any other engineer or student working in petroleum engineering, this groundbreaking work is a must-have. Perfect for any scientist or engineer's library, this volume can be a must-read page-turner or a valuable reference work.


About the Author:

Galina Belenitskaya, PhD, is Chief Research Scientist at the Russian Geological Research Institute (VSEGEI), in St. Petersburg, Russia and has worked there since 1972. She has a doctorate in geological and mineralogical sciences from the Leningrad School of Mines. She is a leading expert in salt geology and litho-geodynamics of natural gas. She is an active member of the International Academy of Mineral Resources, the Russian Mineralogical Society, the Russian Foundation for Basic Research, and the Russian Science Federation. She has authored over 200 scientific publication, including 20 monographs.


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Product Details
  • ISBN-13: 9781119479055
  • Publisher: John Wiley & Sons
  • Publisher Imprint: John Wiley & Sons
  • Height: 229 mm
  • No of Pages: 714
  • Spine Width: 38 mm
  • Weight: 1160 gr
  • ISBN-10: 1119479053
  • Publisher Date: 06 Dec 2018
  • Binding: Hardback
  • Language: English
  • Returnable: N
  • Sub Title: Distribution, Tectonic and Kinematic History, Salt-Naphthids Interrelations, Discharge Foci, Recycling
  • Width: 152 mm


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