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Title: Spatial distributions of New England magmatic complexes, earthquakes and topographic anomalies

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6460095

Chapman (1968) proposed that the locations of magmatic complexes of the White Mountain magma series were controlled by a structural grid with NNW and E-W trends. The directions of structural control were thought to be strikingly apparent and thus no quantitative means for testing the hypothesis were proposed. The grid directions are not associated with known structures, however, and the significance of Chapman's theory cannot be investigated geologically. In this paper the hypothesis of structural control is tested by statistically analyzing the locations of the White Mountain complexes. The analysis shows that the locations of magmatic complexes do not reveal a component of structural control. The selection of a NNW grid direction was probably strongly influenced by the NNW-elongated outcrop pattern of the White Mountains. The Main coastal plutons cited by Chapman as examples of features defining a structural grid do not form a pattern significantly different from random. The results of analyses of other geophysical and topographic data will be presented to characterize further the role which structural control plays in the geology of New England. The data sets include locations of earthquake epicenters in Vermont and northeastern New York, topographic peaks in the White Mountains, and aeromagnetic anomalies in New Hampshire and Vermont.

Research Organization:
Univ. of Pennsylvania, Philadelphia (USA)
OSTI ID:
6460095
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English