Titlebook: Basement Tectonics 12; Central North Americ John P. Hogan,M. Charles Gilbert Book 1998 Springer Science+Business Media Dordrecht 1998 Cambr

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harbinger

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The Variscan Geodynamic Cycle in the Sardinian-Corsican Massif, According to the Most Recent Data the continental crust and the subsequent opening of the oceanic area. In agreement with Pin and Marini (1993), middle Ordovician magmatism in the Sardinian-Corsican Massif can be related, as in the Central Europe Variscan chain, to ensialic extension causing crustal thinning and initiating rifting.

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guardianship

The North-Trending Swarm of Mesozoic Dikes in the Southern Appalachians: Its Map Pattern and Signifishears indicating that the N-trending dike swarm was emplaced with an E-W-oriented σ. and a vertical σ.. The N-trending dike swarm crosses two major Triassic rift basins: the Dan River Basin of southwestern Virginia and adjacent North Carolina, and the Deep River Basin of North Carolina.

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Geologic Provinces of Oklahomainces in the subsurface on the basis of geological criteria. The authors have attempted to use the originally published names for the recognized provinces. However, we have also used the most . correct names, i.e., Nemaha Uplift, Nemaha Fault Zone, and Central Oklahoma Fault, in lieu of Nemaha “Ridge.”

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Harbor