Fluid-rock interaction in the Reynolds Range, central Australia: superimposed, episodic, and channelled fluid flow systems

2001 ◽  
Vol 184 (1) ◽  
pp. 357-379 ◽  
Author(s):  
Ian Cartwright ◽  
Ian S. Buick ◽  
Julie K. Vry
Keyword(s):  
Fluid Flow ◽  
Rock Interaction ◽  
Flow Systems ◽  
Central Australia

FLUID FLOW SYSTEMS ASSOCIATED WITH THE MEADE THRUST, WYOMING SALIENT, SEVIER FOLD-THRUST BELT

2016 ◽  
Author(s):  
David Brink-Roby ◽  
◽  
Mark A. Evans ◽  
Gautam Mitra ◽  
Adolph Yonkee
Keyword(s):  
Fluid Flow ◽  
Thrust Belt ◽  
Flow Systems

Insights into fluid flow and water-rock interaction during deformation of carbonate sequences in the Mexican fold-thrust belt

2011 ◽  
Vol 33 (8) ◽  
pp. 1237-1253 ◽  
Author(s):  
Elisa Fitz-Diaz ◽  
Peter Hudleston ◽  
Luc Siebenaller ◽  
David Kirschner ◽  
Antoni Camprubí ◽  
...  
Keyword(s):  
Fluid Flow ◽  
Thrust Belt ◽  
Rock Interaction ◽  
Water Rock Interaction

Iron Oxide (U–Th)/He Thermochronology: New Perspectives on Faults, Fluids, and Heat

Elements ◽  
2020 ◽  
Vol 16 (5) ◽  
pp. 319-324
Author(s):  
Emily H. G. Cooperdock ◽  
Alexis K. Ault
Keyword(s):  
Fluid Flow ◽  
Iron Oxide ◽  
Heat Exchange ◽  
Iron Oxides ◽  
Fault Zone ◽  
Frictional Heating ◽  
Fault Zones ◽  
Chemical Behavior ◽  
Rock Interaction ◽  
Dynamic Motion

Fault zones record the dynamic motion of Earth’s crust and are sites of heat exchange, fluid–rock interaction, and mineralization. Episodic or long-lived fluid flow, frictional heating, and/or deformation can induce open-system chemical behavior and make dating fault zone processes challenging. Iron oxides are common in a variety of geologic settings, including faults and fractures, and can grow at surface-to magmatic temperatures. Recently, iron oxide (U–Th)/He thermochronology, coupled with microtextural and trace element analyses, has enabled new avenues of research into the timing and nature of fluid–rock interactions and deformation. These constraints are important for understanding fault zone evolution in space and time.

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