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LITHOPROBE East - Regional Summary

The opening and closing of ocean basins is a fundamental process in the continuing evolution of the Earth. The island of Newfoundland, the focus of this transect, owes its geological configuration to the opening and closing of the ancient Iapetus Ocean during the Paleozoic (~600-275 Ma). With the subsequent opening of the Atlantic Ocean during the Mesozoic (~165-90 Ma), a process spatially offset from the suture zone formed by Iapetus closure, the Appalachian orogen was established along eastern North America.


Map of Newfoundland Appalachians showing tectonostratigraphic zonations, simplified geology and location of onland LITHOPROBE seismic corridors.


The LITHOPROBE East Transect investigates these processes through studies in and around Newfoundland. Interpretation of the extensive marine and onshore geophysical data reveals at least two lower crustal blocks, perhaps associated with the Laurentian (Grenville of North America) and Gondwanan (of African affinity) plates, overlain by allochthonous tectonostratigraphic domains established previously on the basis of surface geological studies. Integration of the multidisciplinary data has led to the development of a model for crustal evolution that involves continent-continent collision between Lurentia and Gondwana as Iapetus closed, with detachment and underthrusting of the subcrustal lithosphere of the Laurentian plate. Oceanic crust of Iapetus was obducted onto the crustal blocks. On the rifted Atlantic margin, marine seismic studies have established two basin styles that differ markedly in structure and stratigraphy from one region to another, results being used by the petroleum industry. At the present ocean-continent transition, interpretations suggest underplating of thinned continental crust by basaltic melt during the rifting process. LITHOPROBE studies have significantly altered previous models for evolution of the Newfoundland Appalachians and are providing a more comprehensive understanding of the processes and structures involved in that evolution.


Simple schematic describing collision between the Laurentian and Gondwanan plates based on LITHOPROBE results


Publications

LITHOPROBE East Transect Reports

 
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