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All Inclusive Package Holidays
During the Mesozoic era (about 250 to 65 million years ago)
a large ocean (Tethys Ocean), floored by oceanic lithosphere
existed in-between the supercontinents of Gondwana All Inclusive
Package Holidays and Laurasia (which lay to the south and
north respectively; Robertson & Dixon, 2006). This large
oceanic plate was consumed at All Inclusive Package Holidays
subduction zones (see subduction zone).
All Inclusive Package Holidays At the subduction trenches
the sedimentary rock layers that were deposited within the
prehistoric Tethys Ocean buckled, were folded, faulted and
tectonically mixed with huge All Inclusive Package Holidays
blocks of crystalline basement rocks of the oceanic lithosphere.
These blocks form a very complex mixture or melange of rocks
All Inclusive Package Holidays that include mainly serpentinite,
basalt, dolerite and chert (e.g. Bergougnan, 1975).
All Inclusive Package Holidays The Eurasian margin, now preserved
in the Pontides (the Pontic Mountains along the Black Sea
coast), is thought to have been geologically similar to the
Western Pacific region today All Inclusive Package Holidays
(e.g. Rice et al., 2006). Volcanic arcs (see volcanic arc)
and backarc basins (see back-arc basin) formed and were emplaced
All Inclusive Package Holidays onto Eurasia as ophiolites
(see ophiolite) as they collided with microcontinents (literally
relatively small plates of continental lithosphere; e.g. Ustaomer
and Robertson, 1997). All Inclusive Package Holidays
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