Glenn Spinelli and Demian Saffer

Slides:



Advertisements
Similar presentations
Plate Tectonics Evolution of Continents, Ocean Basins, Mountains Continental Margins.
Advertisements

Divergent boundary Transform fault Convergent boundary Three types of plate boundaries Fig. 1.
Frictional and transport properties of the Chelungpu fault from shallow borehole data and their correlation with seismic behavior during the 1999 Chi-Chi.
1 Average reservoir residence times ReservoirAverage residence time Antarctica20,000 years Oceans3,200 years Glaciers20 to 100 years Seasonal snow cover2.
L=A  -r Dynamic recrystallization. Some Applications Dewatering due to partial melting and the lithosphere-asthenosphere structure (Karato.
Summary of examples of correlation between lithology and seimicity Jessica Hawthorne Ge277 February 26, 2014.
The Structure of the Earth and Plate Tectonics
Design of Recuperative Heat Exchanger Presented by -- Jinying Zhu.
The governing equation for groundwater flow can be written using total head (h) or pressure (p). Why do we typically use head (h) as the dependent variable?
13. Subduction Zones William Wilcock
OET Nautilus Workshop University of Rhode Island, ISC 6–9 May 2013 OET Nautilus Workshop University of Rhode Island, ISC 6–9 May 2013 AT25-04: Hydrogeologic,
Magnetic anomaly number age (Ma) from geomagnetic reversal chronology extrapolated in South Atlantic assuming constant rate of spreading paleontological.
Volcanoes and Plate Tectonics
Geometry & Rates of 3D Mantle Flow in Subduction Zones
Electrohydrodynamics Laboratory Y. Feng and J. Yagoobi Heat Transfer Enhancement and Two-Phase.
The Structure of the Earth and Plate Tectonics. Structure of the Earth The Earth is made up of 3 main layers: –Core –Mantle –Crust Inner core Outer core.
Constructive Plate Margins - Revision
Major Ocean Currents An Ocean Current is a large volume of water flowing in a certain direction. Surface currents are driven by wind and carry warm or.
Volcano Vocabulary. Volcano A mountain formed when molten rock is pushed to Earth’s surface and builds up.
Section 1: Volcanoes and Plate Tectonics
Heat Transfer.
Specify domain’s starting fluid temperature on the Initial pane Porewater temperature is 40 °C.
Institute of Volcanology and Seismology FEB RAS
1 Life in Water Chapter 3. 2 The Hydrologic Cycle Over 71% of the earth’s surface is covered by water:  Oceans contain 97%.  Polar ice caps and glaciers.
Glenn Spinelli Effects of fluid circulation in ocean crust on subduction zone temperatures and metamorphism.
Extant models: Thorough characterization of microbial habitats within submarine volcanoes demands that physical flow models be combined with models of.
Chapter 2: Canada’s Physical Landscape. Formation of the Earth 2.1 Planet Earth Formation of the Earth 2.1.
Porewater temperature is 40°C Specify domain’s starting fluid temperature on the Initial pane.
Along Strike Variations in Heat Flow 1.Shallow Thermal Structure of the Middle America Trench, Costa Rica Robert Harris, COAS Oregon State University Ingo.
Slow Slip: An Ubiquitous yet Poorly Understood Mode of Strain Release Susan Y. Schwartz Department of Earth and Planetary Sciences UC Santa Cruz.
Oxygen Potential in High Burnup LWR Fuel using Themochimica in MOOSE/BISON Theodore M. Besmann.
© Mark E. Damon - All Rights Reserved Another Presentation © All rights Reserved
Features of Plate Boundaries
Standards 3: Thermal Energy How Heat Moves  How heat energy transfers through solid.  By direct contact from HOT objects to COLD objects.
9.4 Testing Plate Tectonics
Plate Tectonics and Volcanoes
* Materials that allow heat, electricity, or sound waves to pass through them.
Continental Drift.
THE MECHANISMS OF PLATE MOTION
What is the thermal structure of a subduction zone?
Conduction Convection Radiation
Thermal Energy & Heat.
From the trench to the seismogenic zone: Establishing links between low-T metamorphism, fluid pressure, and fault stability Demian Saffer, Penn State.
Evan Solomon School of Oceanography University of Washington
Energy.
Comparison of the thermal characteristics and temperature profile of the ground in Cyprus with other Mediterranean countries This work is supported by.
The Moving Crust Topic 4.
Heat Transfer List three types of heat transfer and describe each.
Heat Exchange -Heat ALWAYS travels in the direction of: HOT  COLD
Metamorphic Rocks.
effects of volcanic activity
PLATES AND TECTONIC MOVEMENT
Plate Heat Exchanger (PHE)
Section 3: Plate Boundaries
Why is there melting and volcanism at subduction zones?
Thermal Energy By: Lauren Robinson. HEAT Heat is the flow of thermal energy or energy in transit. It transfers from a warm object to a cold object. Transfer.
Oceans, Coastlines, Shores
Fluids derived from the compaction and
Structures of Accretionary Prism Offscraping, Underplating and Sediment Subduction.
Plate Tectonics Test.
Plate Tectonics.
6.2 Notes The Theory of Plate Tectonics
Forms of Energy Unit 3 Part 2 Vocabulary.
Types of plate margin There are 2 types of crust:
Alteration of Rocks by Temperature and Pressure
Explain the theory of plate tectonics.
Energy and Chemical Changes
Energy in thermal systems
Complete chart for 18 minutes
Strain Release Along the Northern Costa Rica Seismogenic Zone
Presentation transcript:

Glenn Spinelli and Demian Saffer Trench-parallel fluid flow in the Nicoya margin subduction zone resulting from temperature differences Glenn Spinelli and Demian Saffer

Subduction zone hydrogeology Saffer and Bekins, 1998 fluid pressure affects fault strength transport of chemical species nutrients to vent communities heat transport

Subduction zone fluid flow in 3-D Screaton and Ge, 1998 Bangs et al., 1996

Thermal controls on hydraulic conductivity Kato et al., 2004 Morrow et al., 2001 Khot > Kcold Kcold > Khot

Nicoya margin heat flow and temperature Spinelli et al., 2006 Fisher et al., 2003

Along-strike differences in hydraulic conductivity

Nicoya margin trench-parallel fluid flow

Nicoya and other circum-Pacific examples

Conclusions Along-strike differences in temperature influence subduction zone hydrogeology trench-parallel differences in fluid pressure & flow shallow, cold decollement  flow from cold to hot side deep, hot decollement  flow from hot to cold side

Along-strike differences in hydraulic conductivity

Effect of dewatering distribution