The Nature of Magmatism in the Appalachian Orogen, Ediția 191

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A. Krishna Sinha, Joseph Bruce Whalen, John P. Hogan
Geological Society of America, 1 ian. 1997 - 429 pagini
The thermal evolution of mountain belts is recorded inthe distribution, origin and ages of magnatism. In this volume, petrologic, isotopic and geochemical evidence is presented to highlight the contribution of igneous rocks to the evolution of the Appalachian Orogen in both Canada and the United States. These papers emphasize the use of modern geochemical and petrologic data to discriminate the sources yielding magmas, and thus the nature of the crust and mantle.
 

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Shieh Y N and Schwartz H P
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Additional
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TABLE 1 MAJOR AND TRACEELEMENT GEOCHEMISTRY
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Preface
Acknowledgments
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Nd and Sr isotopic evidence Contributions to
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Additional
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TABLE 1 WHOLEROCK ANALYSES OF MAQUEREAU GROUP LAVAS
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Zr Ga
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Th
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White R S 1992 Crustal structure and
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Grain
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Ti100
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A
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La Ce Pr Nd Sm Eu Gd Tb Dy Ho
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Williams H 1979 The Appalachian Orogen in
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to alteration Depletion in high fieldstrength
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Liberty
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Mineralogy and Petrology v 78 p
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1000
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Ab50 Anso
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Th Nb La Ce Pr Nd Sm Zr
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www
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ROCKNMORB
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AN
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Italic page numbers indicate major references
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Copyright 1997 The Geological Society of America
Contents
3645 N
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TABLE 1 MAJOR AND TRACEELEMENT GEOCHEMISTRY
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6
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Ga
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Th
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Society of America Bulletin v 106 p
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Elkahatchee Quartz Diorite
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La Ce Pr Nd Sm Eu Gd Tb Dy Ho
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Journal of Geology v 102
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to alteration Depletion in high fieldstrength
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Liberty
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Mineralogy and Petrology v 78 p
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1000
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Ab50Аn50
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10
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APPENDIX 2 LOCATIONS AND DESCRIPTIONS OF NOTRE DAME PLUTONIC ROCKS
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W
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AN
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