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Terrestrial Palaeoecology and Global Change

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Chapter 5. Tectonic factors of global changes<br />

125<br />

alies (Schouten & Klitgord, 1982), with polarity changes over their vertical sections<br />

(Lowrie & Alvarez, 1981), better agrees with impregnation than spreading.<br />

In other words, the so-called spreading anomalies (the M-series beneath the Cretaceous<br />

sediments in the Atlantic) are basically of the same nature as the J-anomaly of the<br />

same zone reflecting an exhumed basaltic ridge. Likewise, the “quiet zone” of continental<br />

margin is an exhumed mantle impregnation into the marginal fault zone (Witmarsh et<br />

al., 2001).<br />

As for the age progressions over mid-plate volcanic ridges, such as the Hawaiian<br />

Isl<strong>and</strong>s, their plate-tectonic interpretation as hot-spot (plume) traces is scarcely compatible<br />

with radiometric dating. The Hawaiian Isl<strong>and</strong>s <strong>and</strong> the roughly parallel Line Isl<strong>and</strong>s<br />

occur on the same plate, but are of the widely disparate chronologies <strong>and</strong> rates of volcanic<br />

progression. Moreover, the diagonal Line lineament overlaps in age with the orthogonal<br />

Emperor lineament – a paradoxical situation of two simultaneous hot spots leaving<br />

diverging traces on the same plate. No systematic age progression is found over the<br />

Cameroon Line, an alleged plume trace in western Africa (Holliday et al., 1990). In the<br />

case of the Ninetyeast Ridge, Indian Ocean, the age progression is inconsistent with the<br />

hot-spot mechanism (Sclater & Fisher, 1974).<br />

The plume theory fails to explain a midplate volcanism along the Cooke – Austral<br />

Isl<strong>and</strong> Chain, with an inconsistent age progression apparently controlled by lithospheric<br />

stress (McNutt et al., 1997). Such features more realistically reflect propagation of<br />

tectonic stresses <strong>and</strong> concurrent volcanic activities over the parallel, but diachronous,<br />

shear zones. Insofar as igneous activity over meridional lineaments systematically propagates<br />

towards the equator, the Eötvös forcing appears a possibility.<br />

Although still afloat owing to the powerful lobby, the plate tectonics theory shows no<br />

prospect of further development, which means that it will be soon ab<strong>and</strong>oned. Stones<br />

rejected by the builders of the model (essentially geophysical, with little respect to stones)<br />

will then be used as cornerstones for new geodynamic theories. But even then plate<br />

tectonics will remain in the annals of epistemology as a paradigmatic Kuhnian paradigm,<br />

as such deserving a critical analysis.<br />

Meanwhile it seems best to seek explanations of global tectonomagmatic developments<br />

in the most obvious global processes, such as rotation of the earth. The rotational<br />

model is by now the only one accounting for a correlation of geomagnetic, tectonomagmatic,<br />

epeiric <strong>and</strong> climatic processes (Krassilov, 1976d, 1985, 1991, 1995a <strong>and</strong> below).<br />

V.2. Rotaion tectonics<br />

The earth is not the only tectonically active planet, <strong>and</strong> there is little ground for believing<br />

that its tectonic structure is unique in the solar system. Therefore, geodynamic models<br />

can be verified by applying them to other planets or their moons. Comparative planetology<br />

tells us that only non-synchronous planets (those with widely disparate rotation

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