CONCLUSIONS
All of the scientific objectives of Leg 176 were dependent on deepening
Hole 735B. The ultimate success of the leg will be measured by the
results published by the science party and other interested investigators
in the years to come. The primary objective of Leg 176 was recovering a
representative section of gabbroic Layer 3 to determine its stratigraphic
variation with depth. This objective was achieved beyond our
expectations, manifested in deepening Hole 735B to more than 1.5 km with
an overall recovery of more than 86% in an environment (ultra-slow
spreading ridges) where the lower crust is believed to be only about 2 km
thick. The supplementary scientific objectives of Leg 176, testing
whether or not the Moho is coincident with the crust-mantle boundary and
deepening Hole 735B well below the crust-mantle boundary were not
achieved due to operational time limitations and drill string failure.
Toward these objectives, however, Leg 176 successfully demonstrated
that the JOIDES Resolution, with her present technology, has the capacity
for deep drilling and high recovery at this location and that the success of
Leg 118 was not an anomalous circumstance. We await future drilling
programs at this location to fully realize all the science objectives
proposed for Leg 176, which include some of the highest order priorities
of the Long Range Plan of the Ocean Drilling Program.
To 176 References
To 176 Table of Contents
ODP Publications
ODP Home