Heat and Fluid Flow at a Crustal Scale | Observations and Models of Coupled Transport in Young Oceanic Lithosphere

Michael Hutnak

ISBN 10: 3659417602 / ISBN 13: 9783659417603

Published by LAP LAMBERT Academic Publishing, 2013

About this Item

Heat and Fluid Flow at a Crustal Scale | Observations and Models of Coupled Transport in Young Oceanic Lithosphere | Michael Hutnak | Taschenbuch | 460 S. | Englisch | 2013 | LAP LAMBERT Academic Publishing | EAN 9783659417603 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Norderstedt, info[at]bod[dot]de | Anbieter: preigu.

Seller Inventory # 105592626

Bibliographic Details

• Title: Heat and Fluid Flow at a Crustal Scale | Observations and Models of Coupled Transport in Young Oceanic Lithosphere
• Publisher: LAP LAMBERT Academic Publishing
• Publication Date: 2013
• Language: English
• ISBN 10: 3659417602
• ISBN 13: 9783659417603
• Binding: Taschenbuch
• Condition: Neu
• Dimensions: 220W x 150H x 29D millimeters 220 millimeters width by 150 millimeters height by 29 millimeters depth
• Weight: 703 grams
• Seller catalogs:
  • Bücher

About this title

Synopsis

Hydrothermal circulation of seawater through the oceanic crust profoundly influences lithospheric and oceanic evolution. The upper oceanic crust comprises an aquifer of global proportions, and sedimentation acts to hydrologically isolate the crustal aquifer from the overlying ocean. Thermally-significant exchange of fluids between the crustal aquifer and overlying ocean can only occur where seamounts or other basaltic outcrops penetrate the sediment blanket. Although much progress has been made in the last several decades in elucidating the nature of hydrothermal circulation in oceanic basement, many of the physical properties and processes remain poorly understood or inadequately quantified. This volume addresses several fundamental gaps in our understanding of ridge-flank hydrological processes, namely the roles of seamounts and basement outcrops is facilitating the exchange of fluid between the crustal aquifer and overlying ocean, the extents and rates of hydrothermal circulation in uppermost basement, the bulk crustal permeability distributions required to support the fluid fluxes, the thermal effects of sedimentation on measurements of seafloor heat flux.

About the Author

Ph. D., Earth Sciences (2007)University of California Santa Cruz,Santa Cruz, CA. USA; B.S. Oceanography (1996)Oceanography Department, University of Washington,Seattle, WA. USA