U-Pb age of the Diana Complex and Adirondack granulite petrogenesis |
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Authors: | Asish R Basu Wayne R Premo |
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Institution: | (1) Department of Earth and Environmental Sciences, University of Rochester, 14627 Rochester, New York, USA;(2) U.S. Geological Survey, Federal Center, MS 963, 80225 Denver, CO, USA |
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Abstract: | U-Pb isotopic analyses of eight single and multi-grain zircon fractions separated from a syenite of the Diana Complex of the
Adirondack Mountains do not define a single linear array, but a scatter along a chord that intersects the Concordia curve
at 1145 ± 29 and 285 ± 204 Ma. For the most concordant analyses, the207Pb/206Pb ages range between 1115 and 1150 Ma. Detailed petrographic studies revealed that most grains contained at least two phases
of zircon growth, either primary magmatic cores enclosed by variable thickness of metamorphic overgrowths or magmatic portions
enclosing presumably older xenocrystic zircon cores. The magmatic portions are characterized by typical dipyramidal prismatic
zoning and numerous black inclusions that make them quite distinct from adjacent overgrowths or cores when observed in polarizing
light microscopy and in backscattered electron micrographs. Careful handpicking and analysis of the “best” magmatic grains,
devoid of visible overgrowth of core material, produced two nearly concordant points that along with two of the multi-grain
analyses yielded an upper-intercept age of 1118 ± 2.8 Ma and a lowerintercept age of 251 ± 13 Ma. The older age is interpreted
as the crystallization age of the syenite and the younger one is consistent with late stage uplift of the Appalachian region.
The 1118 Ma age for the Diana Complex, some 35 Ma younger than previously believed, is now approximately synchronous with
the main Adirondack anorthosite intrusion, implying a cogenetic relationship among the various meta-igneous rocks of the Adirondacks.
The retention of a high-temperature contact metamorphic aureole around Diana convincingly places the timing of Adirondack
regional metamorphism as early as 1118 Ma. This result also implies that the sources of anomalous hightemperature during granulite
metamorphism are the syn-metamorphic intrusions, such as the Diana Complex. |
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Keywords: | Granulites geochronology petrogenesis Adirondacks zircon age |
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