Is Haiti becoming a place cursed by earthquakes?
Through modern chemical analyses, researchers at the University of Florida
have discovered that very ancient rocks are present under the island of
Hispaniola. The kind of debris left by the supercontinent Gondwana, they will be
transported for nearly 1,500 km, through the tectonic movements of the
Caribbean plate.
Geologists have so far believed that
Hispaniola, the island home to the Dominican Republic and Haiti, was
geologically relatively young. About 150 million years ago. But analyses by
researchers at the University of Florida have reversed that perspective. The
chemical composition of rocks helps us to know their origin. Detailed studies
of rare element concentrations such as strontium or neodymium and isotopic
ratios of elements such as lead provided researchers with a kind of rock
identification label. They can thus discover the source of the lava or magma
from which they come, and reconstruct the tectonic displacements caused by the
terrain they have formed.
A double surprise
Professor Michael Perfit's team
examined the lava that quickly turned out to have been spat out during an
eruption 1 million years ago. First surprise, because the last known volcano on
the island dates back 40 million years. But the main discovery is yet to come.
After analyzing the plasma source mass spectrometer (ICPMS), geochemists found
oddities in the composition of the samples. Throughout the rest of the island
and more widely throughout the Caribbean arc, there are subduction zone lavas:
basaltic oceanic crust, ancient and dense, subducting under another
lithosphere, oceanic or continental, resulting in deformation and volcanic
formation. Here, however, the curves show very different concentrations of
trace elements. They are strikingly similar to what one might encounter in the
case of volcanoes occurring in the center of a continent. And the rocks of the
superposition, the source of this lava, seem to be at least 1 billion years
old.
An incredible journey
To solve the puzzle, he must take a
solution more than 1,500 km away. At the level of Central and South America,
there are rocks of this type. This is Terranes Grenvillian, fragments of
ancient continents testify to distant ages in the history of the planet or
emerging lands without the same terms.
Ainsi, il semble qu'Hispaniola soit, au moins en partie, située sur les restes d'une croûte continentale très ancienne qui faisait partie intégrante du supercontinent Gondwana qui existait il y a des centaines de millions d'années. Au moment de son éclatement en plusieurs blocs, dont l'Amérique du Sud et l'Afrique, suivi de l'expansion orientale de la plaque des Caraïbes, une partie de cette ancienne lithosphère continentale avait été emportée. Transporté dans sa coque supérieure comme un rondin dérivant entre deux plans d'eau, il aurait survécu sinon dissipé lors de son périple de plus de 1 500 km jusqu'à son emplacement actuel. Les géologues pensent que ce type de débris formerait une sorte de noyau autour d'îles, voire de continents, qui pourraient se former et grossir.
No comments:
Post a Comment