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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