- Plate Tectonics -
A Paradigm Change
in Progress.
Abstracts
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Abstract:- Spreading ridges occur as two distinct types. An earlier one (Red - Indian - Southern Seas/Oceans) traces an essentially small circle shape in the mantle, is associated with so-called 'mountain building' and 'subduction', and is related to near-flat dislocations. A later one (the Atlantic - SW Indian Ocean) traces an essentially modified longitudinal, near-vertical great circle dislocation with no mountain building and no subduction. The distinction between near-flat and near-vertical dislocations is reflected in the tectonics - Pacific emplacement is initiated as a zone of ductile thinning peripheral to bottom up, forcefully domed mantle intrusion with outwards gravitational collapse of the diapir ('subduction') dissipating as lower mantle extrusion (ridge-spreading) develops. Atlantic emplacement is simply passive, upwelling gap-filling related to top-down, linear crustal failure. |
Abstract:- Current plate maps depicting the consensus model of Plate Tectonics show only active sectors of transform faults, spreading ridges and subduction zones and therefore only a snapshot of recent geological time. A more complete representation of plate architecture is depicted by maps which highlight the full extent of transform faults. Coupled with GPS movement vectors, such maps show that plates grow in a helical spiral of global extent. This linkage to each other of the mantle floors of the world's oceans emphasises the whole-Earth connectivity of mantle growth and provides a basis for reappraising global tectonics in the context of the Earth's spin. |
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Abstract:- The connectivity of the world's oceans indicated by transform faults is spatially partitioned by the Benioff Zone, a highly active zone of Earthquakes up to 600-800km deep encircling the Pacific and coincident on land with the major present-day mountain belts. The Benioff zone separates those ocean floors with 'active' continental margins (many earthquakes) from those with 'passive' continental margins (virtually no earthquakes). Thus the Pacific ocean assumes a spatial and temporal significance different from other oceans of the world. Seen from the perspective of a Pangaean Earth with passive margins closed, and applying the axiomatic universal geological principle that "a map is a section", the Benioff zone is interpreted simply as exhumed asthenosphere, i.e. the roof of the Pacific diapir - the partially melted, more plastic region at the base of the lithosphere overlying the more brittle lower mantle. The encircling mountain belt and its Alpine - Himalayan extension are then simply regarded as the outer crustal 'lid' of the diapir, deformation of which expresses collapsing and overthrusting gravitational adjustment to diapiric mantle rise. Through the interconnectivity of transform faults global deformation is shown to have a dilational symmetry related to the Earth's spin and to unite structures globally across scales in a way which Plate Tectonics, predicated on movement of independent plates, does not. |
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Abstract:- The concept of subduction, the active 'carrying-down' of oceanic lithosphere at the Benioff zone driving convection cells is central to Plate Tectonics, yet it is only one of two interpretations of what may be happening at these active continental margins. The other is "overriding', where the decoupled lithosphere on the continental side of the zone is being carried over the lithosphere on the oceanic side. In using the word 'subduction' Plate Tectonics does not discriminate between the two yet the difference is crucial: 'overriding' (related to spin) is not 'subduction' (related to convection). The consensus choice of subduction follows from a belief that this is a zone of mantle destruction, paired with the complementary creation of ocean floor at spreading ridges. The alternative notion of 'overriding' derives from a demonstrable architectural symmetry of geological structure of the ocean floors and continental margins with the planet's spin. On grounds that Plate Tectonics does not take into account this first-order spin-symmetry of the structure of the planet, and is self-contradictory in many of its inferences, notions of convection are held to be incomplete and in need of revision. In short, convection predicated on subduction as the corollary of ridge spreading is considered to be invalid. |
Abstract:- Three regions of the Earth's crust are notable for their uplift and for being linked through common elements of crustal torsion and mantle growth, 1. the circumglobal mountain belt of typically Mesozoic stratigraphy centred on Tibet in the Himalayas, significantly known as 'The Roof of the World' ; 2. the 'Tomographic Wheel' of Indonesia (the 'Indonesian' or 'Celebes' wheel), recognisable in seismic tomography to 700km depth (benioff limit) and graphically represented by a gravitationally corrected isosurface; and 3. extrusion of the mantle represented by the Pacific Ocean. These three regions represent detachment of successive levels of the lithosphere between the upper crust, the upper mantle and the lower mantle, with the Benioff representing exhumation of the asthenosphere as isostatic ajustment stabilises the planet. Elevation on this scale is coupled with a global drop in sea-level which has exhumed Mesozoic stratigraphy to the highest parts of the world and continues to the present day in the elevation of marine terraces world-wide. A drop in sea-level coupled with elevation on such a scale is not possible in a context of simple models of metre-scale eustatic/ isostatic adjustment and must be seen as corollary effects of outwards movement of the planet's surface from the centre, expressed generally in the architecture of crustal structure, but particularly in the mountain belt that encircles the Earth and in the growth of the ocean floors. The structures expressing global uplift are the same as those describing the architecture of the planet's spin. It is concluded therefore that the planet has grown to approximately double its size since the Mesozoic and that surface elevation and sea-level fall are corollary effects of planetary growth, possibly consequent on unknown aspects of physics connecting mass creation to the celestial sphere. Plate Tectonics based on models of convection disregards first-order aspects of global planetary structure, is contradictory from many perspectives, and is rejected as inadequate as a model for global tectonics. |
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Abstract:- The Earth currently has a rotational oblateness of 0.008 which translates as a difference in diameter of 48km at the equator compared to the poles, and a circumglobal elevation expressed as the dissected plateau known as the 'mountain belt' which extends from the Atlantic through Eurasia and encircles the Pacific. Elevation peaks in the Tibetan region at not less than 8km. Spin symmetry of global structure indicates that this elevation-peak evidences the precursor breakthrough axial to the belt of the curved profile of the lower mantle surface. Lithospheric adjustment occurs as an equilibration across an interface of differential curvature as the Earth adjusts from a more oblate to more spherical shape expressed in the fossilised remnant of crustal oblateness represented by the circumglobal plateau surface and by the active extrusion of the Atlantic, Indian, and Southern Oceans, as the circum-Pacific margins fringing the Benioff zone, and as the Pacific spreading ridge itself. The synoptic picture is one of continuity of whole-Earth adjustment to latitudinally migrating, spherical mantle extrusion modified by spin-related torsion, and is interpreted as a shift in the gravitational barycentre of the Earth-Moon system. This picture provides a geological framework for global dynamics within a context of Earth rotation and expansion, rather than one of internal convection in an Earth of constant size and constant rotation rate which ignores spin symmetry. |
last updated - March 2006