Experimental modeling of structure-forming deformations in rift zones of mid-ocean ridges |
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| Authors: | A L Grokholskii E P Dubinin |
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| Institution: | (1) Physical Geography Museum, Moscow State University, Vorob’evy gory, Moscow, 119992, Russia |
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| Abstract: | The modern methods of physical modeling of structure-forming deformations in extension zones of oceanic lithosphere are discussed;
the methods differ in their experimental equipment, model material, and experimental techniques. The simulation performed
with an elastic-ductile model has demonstrated that extension of a brittle lithospheric layer results in disruption of its
continuity and in formation of a rift valley according to the mechanism of running fracture propagation. The modeling results
provide insights into qualitative pattern of faulting and fracturing within a rift zone, specific features of rift segmentation,
and development of various structural elements (axis bends, echelons of fractures, nontransform offsets, small and large overlaps,
etc.) under various geodynamic conditions of spreading. The modeling has shown that origination and evolution of structures
of various types depend on the lithosphere’s thickness beneath the rift axis; the width of the lithosphere’s heating zone;
the spreading orientation; and, to a lesser degree, on the spreading rate. A relatively rectilinear rift broken into particular
segments bounded by small-amplitude offsets with or without minor overlaps arises in the case of both a small width of the
heating zone, closely related to the axial magma chamber, and a small thickness of the lithosphere (fast-spreading conditions).
In the case of a wide heating zone caused by ascent of an asthenospheric wedge or a mantle plume, offsets of rift are more
pronounced and deformations embrace a wider region. If, as a result, the thickness of the lithosphere increases, the rift
will be less linear and the structural heterogeneity will become more contrasting. In addition to the thickness of the lithosphere,
the angle between the rift zone and the extension axis also controls the rift configuration: the greater the angle, the more
conspicuous the en echelon arrangement of fractures. For any spreading type, the propagating front of linear microfractures
that disrupt the upper brittle layer of the lithosphere predates the origin of mesoscopic fractures and predetermines a general
trend of the rift zone. This indicates that the fractures of various sizes propagate simultaneously. |
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