Research Collection
Volltext
ÄHNLICHE DOKUMENTE
Real rocks, whether shallow or deep in the Earth, combine the properties of ideal viscous, plastic and elastic bodies. Their strain has elastic properties on the time scale of
The present day divergent plate boundaries reside mainly in oceans where they form broad, fractured swells. The prominent physiographic expression is a world-encircling, ca. 100
- (1) erosion which removes the near surface rocks and allows uplift and - (2) gravitational collapse of elevated topography. In effect, many orogenic belts terminated
- Conjugate sets of strike-slip faults form oblique to the main fault (synthetic and antithetic Riedel shears, i.e. with the same and opposite sense of displacement as the
(2) Post-collision underthrusting of several hundred kilometres of continuous Indian crust beneath Tibet implies that uplift of the Tibetan plateau proceeded from south to north
From a practical point of view, subsequent measurements must be carried out in such a way that events on separate traces can be correlated as coming from the same horizon
This page was generated automatically upon download from the ETH Zurich Research Collection.. For more information please consult the Terms
Conventional seismic section based on surface profiling data from the vicinity of the borehole site.. Crosshole