Titlebook: Basement Tectonics 7; Proceedings of the S Robert Mason Conference proceedings 1992 Springer Science+Business Media Dordrecht 1992 Deformat

Gullible

AWRY

tenosynovitis

Fundamental Crustal Lineaments and Transverse Structural Zones in Continental Riftsoften intense fracturing, along trends which are generally transverse or oblique to the main rift-bounding structures. The transverse zones often delimit major re-orientations in the rift trend, or link paired offset margins, and are foci for magmatic activity and heat flow anomalies. Furthermore, t

思想上升

crucial

Basement Extension on the Newfoundland Continental Margin (Canadian East Coast)ridges and a complex continent-ocean transition zone formed during several Mesozoic rifting periods. Recent industry seismic lines and several deep seismic reflection profiles (Lithoprobe East) allow for the recognition of coherent reflections of intra-basement provenance..Precambrian and early Pale

Decrepit

Structural Fabric of the North American Continent, as Defined by Gravity Trendsends is demonstrated by the close correspondence between gravity domains defined on the basis of trend patterns, and structural domains based primarily on geological criteria. This relationship provides a powerful tool for investigating Precambrian basement geology in platform-covered regions of the

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嚴(yán)厲譴責(zé)

Tectonics of Some Spatial Arraysemarkably coincident with inflections in the seismic profile. It is suggested that fault spacing is dependent on the upper brittle part of the crust..Archean plutons occur in wider-spaced arrays (65 km to 90 km), and with either convection or buoyant-layer models, this spacing indicates a magma sour

CRUC

chondromalacia