Dear Colleagues
We would like to draw your attention to the following
symposium “The Coupling of Fluid Reservoirs in the Earth”
(T11) to be held at the forthcoming conference on Earth
System Processes in Edinburgh, Scotland, on June 24-28,
2001. The conference is being presented jointly by the
Geological Society of America and the Geological Society of
London, and is also being sponsored by the British and US
Geological Surveys, the University of Edinburgh and the
Edinburgh Geological Society.
Earth System Processes will focus on two major themes critical
to advancing understanding of how our planet works.
Earth System Linkages will explore the relationships between
the solid Earth, the hydrosphere, atmosphere, cryosphere, and
biosphere.
Earth System Evolution will examine the way in which
processes controlling the nature of the planet have changed since
the birth of the solar system 4.5 billion years ago.
Both themes will involve comparison with other planetary
systems in the solar system and beyond. Both will take into
account critical extraterrestrial influences.
Further details of the conference, registration and abstract
submission procedures, and deadlines may be found at:
http://www.geosociety.org/meetings/edinburgh
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Symposium Title: The coupling of fluid reservoirs in the
Earth (T11)
Convenors:
Craig Manning (UCLA) ([log in to unmask])
Colin Graham (Edinburgh) ([log in to unmask])
Keynote speakers:
Steve Ingebritsen (USGS, Menlo Park)
Jamie Connolly (ETH – Zurich)
Summary:
The storage, movement and reaction of fluids in the Earth, and
the exchange of fluids with the hydrosphere and atmosphere,
play a central role in a wide range of Earth processes such as
ore genesis, the formation and migration of hydrocarbons, the
buffering of ocean chemistry, the evolution of the atmosphere,
global climate change, water resources and supply, and crustal
deformation and seismicity.
Fluids are stored within different reservoirs within the Earth, but
the communication between these reservoirs remains poorly
understood. Terrestrial fluid reservoirs are separated by major
crustal transitions, such as the Mohorivicic discontinuity, the
brittle-ductile transition and basement-basin interfaces. The
petrologic, rheologic, and/or lithologic contrasts across these
boundaries should control the transfer of fluids, yet the gradients
in permeabilities, structure/lithology, mechanical/rheological
properties, and fluid pressure and flux remain controversial. The
fluid content and behaviour within these regimes is also widely
debated – is the lower crust wet or dry? can fluid move up and
down temperature? what are the fluxes? does fluid release in the
deep crust influence global climate change? how do the
geophysical properties of the crust (seismic, electrical, acoustic)
vary with fluid content and movement? The movement of fluid
within and between regimes is controlled by permeability
variation in the crust in space and time, but this variation is only
beginning to be understood and is difficult to constrain in situ.
Can geophysical techniques be reliably used to identify fluids in
situ in the mid-deep crust?
The measurement, characterisation and modelling of fluid
storage, movement and behaviour within and between these
various regimes is thus one of the most active and topical areas
of geological research, involving an array of chemical, physical
and theoretical approaches. This symposium is aimed at
providing a lively inter-disciplinary forum for the presentation
and exchange of ideas and results across traditional discipline
boundaries and to bring together geophysicists, geochemists,
and modellers.
Colin Graham
Department of Geology and Geophysics
University of Edinburgh
Edinburgh
EH9 3JW
UK
Phone: 0131-650-4849
Fax: 0131-668-3184
Email: [log in to unmask]
Craig Manning
Department of Earth and Space Sciences
University of California
Los Angeles
California 90095-1567
USA
Phone: 310-206-3290
Fax: 310-825-2779
Email: [log in to unmask] HYPERLINK
mailto:[log in to unmask] }
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