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The past two decades
have seen major leaps in our understanding of the structure and dynamics of
the continental lithosphere. These advances are due in large measure to the
application of new technologies in such fields as deep seismic imaging, magnetotelluric
sounding, deformation monitoring, geochemical tracing, and geodynamic modeling.
In particular, systematic national programs cored by deep
seismic profiling,such as COCORP (US),
BIRPS (UK),
DEKORP (Germany), ECORS
(France) and LITHOPROBE (Canada),
among others, have been especially effective in making major discoveries about
the continents: lithospheric-scale detachments, deep fluid accumulations,
mobile Mohos, laminated lower crust, and fossil subduction zones in the upper
mantle being just a few.
The continental lithosphere remains a global priority for both
societal and scientific concerns. Key issues remain unresolved and much of
the world, including many critical geological features, remain unprobed. This
is especially true outside the industrialized nations, where intrinsic resources
for such efforts are particularly difficult to obtain.
It is therefore not surprising that the scientific exploration
of the lithosphere has reached a new, more international phase. Multinational
consortia such as EUROPROBE, and multinational
projects such as URSEIS and
INDEPTH,
are an attempt to martial international expertise and resources to investigate
structures and processes of the continental lithosphere that represent global
scientific priorities. However, experience with such efforts has also led
to recognition that the science could benefit from a more coordinated approach
at the international level.
With this in mind, the International Lithosphere Program
has approved a new international committee with responsibility for stimulating,
coordinating and reporting new continental lithospheric studies from a global
viewpoint. The objective of the proposed committee is not to supplant, nor
to hinder, nor to constrain any individual, national or international effort
to study the continental lithosphere. To the contrary, it is to help stimulate
and facilitate such efforts. This committee is an outgrowth of grass-roots discussions held
at the international deep seismics symposia held at Asilomar, CA, in 1996,
and Barcelona, Spain, in 1998.
For more
information contact:
Larry
Brown, Cornell University, U.S.
Onno Oncken,
GeoForschungsZentrum Potsdam, Germany
Barry
Drummond, Australian Geological Survey Organization
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Last
Updated 1/7/03